EPTD DISCUSSION PAPER NO. 4 Environment and Production Technology Division International Food Policy Research Institute 1200 Seventeenth Street, N.W. Washington, D.C. 20036-3006 U.S.A. September 1994 EPTD Discussion Papers contain preliminary material and research results, and are circulated prior to a full peer review in order to stimulate discussion and critical comment. It is expected that most Discussion Papers will eventually be published in some other form, and that their content may also be revised. WATER MARKETS IN PAKISTAN: PARTICIPATION AND PRODUCTIVITY Ruth Meinzen-Dick and Martha Sullins ACKNOWLEDGMENTS Research completed under USAID to Pakistan Grant Number 391-0492-G-00- 1791-00 for the Ministry of Food and Agriculture, Government of Pakistan. Special thanks are due to Naeem Sarwar and Khalid Saifullah for collecting additional data for this study, and to Manzoor Gill, Jafar Raza, Behjat Hojjati, and Sumiter Broca for assistance in analysis. Sohail Malik and Zakir Rana provided valuable comments and insight, in addition to much assistance in arranging for the data collection. Pierre Strosser collaborated extensively in identifying the important issues to be addressed with regard to water markets in Pakistan, and shared detailed field data used for comparison in this paper. Dr. Bashir Ahmed of Agricultural University, Faisalabad, also provided useful comments and access to National Input Output Survey data used for comparative purposes. Steve Vosti, Peter Hazell, Mark Svendsen, and Mark Rosegrant commented on a draft of the paper. Responsibility for any errors rests with the authors. ABSTRACT Water markets provide one of the most promising institutional mechanisms for increasing access to irrigation from groundwater, particularly for tenants and small farmers. While water markets are found in all provinces of Pakistan, they are most prevalent in canal irrigated areas of Punjab and in NWFP. This study reviews the emerging literature on water markets and uses farm-level survey data to examine the performance of groundwater markets, with particular emphasis on Faisalabad District in Punjab and Dir District in NWFP. Findings indicate that, while large landowners are more likely to own tubewells and pumps, smaller landowners and tenants are more likely to rely on purchases from other farmers' tubewells for access to groundwater. The distance over which water can be transported provides a limitation to water market sales, but lined watercourses increase the distance over which tubewell water can be sold. Contractual arrangements for water in the IFPRI study areas of Faisalabad and Dir districts include hourly charges, buyer providing the fuel plus a fee for wear and tear, and sharecropping for water. While all types of irrigation--canal, purchased groundwater, and own tubewell water--are shown to increase yields of wheat, groundwater has a higher impact than canal water, and water from own tubewells, which provides farmers with the greatest degree of control, has a greater effect on yields than purchased groundwater. Unreliability of access to purchased tubewell water was a problem for over half of water buyers in the study areas. This analysis indicates that purchasers are more likely to have unreliable access to groundwater if they buy water from small-capacity, electric-powered tubewells, if they are young and own little or no land. Policy measures to improve access to and reliability of groundwater through water markets include increasing the density of tubewells, especially by assisting small farmers to purchase tubewells; lining water delivery channels; and providing more reliable electrical power supply to rural areas. Further research is needed on how water markets work in less favorable environments, such as those with salinity, waterlogging, or falling water tables, and to identify policy interventions that are appropriate under each set of circumstances. CONTENTS 1. Introduction.................................................................................................................... 1 2. Who Participates in Water Markets? ........................................................................... 11 3. Relationships Between Water Buyers and Sellers ....................................................... 27 4. Nature of Water Market Contracts............................................................................... 30 5. Agricultural Productivity Under Water Markets ......................................................... 35 6. Reliability of Irrigation Service ................................................................................... 45 7. Research and Policy Measures for Water Market Development ................................. 52 References......................................................................................................................... 59 WATER MARKETS IN PAKISTAN: PARICIPATION AND PRODUCTIVITY Ruth Meinzen-Dick1 and Martha Sullins***2 1. INTRODUCTION Irrigation plays a key role in Pakistan's strategy for increasing agricultural productivity. Surface irrigation has allowed the extension of cultivation into areas and seasons which lack sufficient rainfall for agriculture, and raised yields above what is possible under rainfed cultivation. Groundwater irrigation is increasingly important in improving production, either alone or in conjunction with surface irrigation. Access to water in public irrigation systems (surface canals and public tubewells) is tied to ownership of land in the command area. This land ownership entitles the farmer to a fixed turn of irrigation flow during a rotation cycle, to be used only on that land. The rigidity of this system limits the productivity of surface irrigation and public tubewells, a limitation which is especially apparent in comparison with privately-managed groundwater irrigation, where farmers have more control of water timings (see Renfro and Sparling 1986). Access to privately-managed groundwater irrigation is dependent on investment in wells and pumping devices. To the extent that large and wealthy farmers are most likely to own tubewells and small or poor farmers are unable to make the necessary 1 Research Fellow, Environment and Production Technology Division, International Food Policy Research Institute. 2 Former Senior Research Assistant, Environment and Production Technology Division, International Food Policy Research Institute. 2 investment, the latter may be excluded from the benefits of highly productive groundwater resources. On the other hand, widespread private ownership leads to over- investment in wells and pumpsets, particularly where holdings are small or fragmented. Institutional arrangements are needed to spread access to groundwater to other farmers, and to increase agricultural productivity and equity of irrigation water resources. Water markets, in which farmers buy and sell irrigation water, provide one of the most promising institutional mechanisms for increasing access to irrigation with private groundwater, for providing vertical drainage, and for increasing the efficiency of water use in irrigation systems (see Rosegrant and Binswanger 1992). While such markets are not formalized or officially recognized, the sale of water from private tubewells is a growing form of water allocation. The sale and purchase of public canal water supplies, though legally prohibited under the Canal and Drainage Act, is another type of private water market transaction which takes place in Pakistan. These are, however, much less common than tubewell water sales.1 This paper examines the nature and operation of groundwater markets in Pakistan. It deals with the extent of water market development, who participates, the nature of transactions, the impact on productivity of irrigated agriculture, and the reliability of purchased irrigation services, with particular reference to Faisalabad District 1 In the IFPRI sample, only 2 farmers reported purchasing canal water, compared to 74 purchasers and 10 sellers of tubewell water. A WAPDA (1990) study of water trading and sale practices in 100 water- courses found 2-3 times as many farmers involved in sale of water from private tubewells as from public (canal and tubewell) sources. The difference in amount of water sold was even more dramatic: Buyers Sellers Number Total hours Number Total hours Public sources 30 161 21 180 Private tubewells 107 4,635 44 22,979 3 in Punjab and Dir District in NWFP. The final section suggests policy instruments for extending water markets and improving their performance. BACKGROUND Irrigation provides crucial water for agricultural production on over 80 percent of the gross cropped area in Pakistan. Most of this irrigation comes through public canal systems, which, according to official reports, deliver surface water to approximately 70 percent of the irrigated area. However, throughout the 1970s and 1980s groundwater irrigation has been the most rapidly-growing source of irrigation: it now serves approximately 25 percent of the irrigated area, and provides over 36 percent of the irrigation water available at the farm gate (Pakistan: Ministry of Food, Agriculture and Cooperatives 1991; Rana and Shafiq-ur-Rehman n.d.). Groundwater has become a crucial input, both as a sole source of irrigation and as a supplement to surface irrigation in canal irrigation commands. From the mid-1950s to 1980 public tubewells provided the primary source of groundwater irrigation development in Pakistan, under the Salinity Control and Reclamation Program (SCARP). According to the World Bank (1984:i): "The Government of Pakistan opted for public control of an extensive groundwater pumpage program based on the rationale that this arrangement would enable the Government to meet multiple groundwater objectives in an efficient and equitable manner." These objectives included: 1. providing vertical drainage to control waterlogging and salinity problems, especially in saline groundwater areas. 2. increasing cropping intensities and agricultural production. 4 3. capitalizing on the economies of scale in pumping technology. By providing water to a larger area than that controlled by single farmers, public tubewells could use larger pumps which are, in theory at least, more efficient. 4. reducing inequity in access to groundwater, by serving farmers with all sizes of holdings, regardless of financial resources for investment. In practice, institutional problems as well as technical difficulties resulted in disappointing performance of public tubewells. Rising operation and maintenance expenses for public tubewells (which consumed 60 percent more than the entire national budget for canal operation and maintenance in 1983/84; see Aklilu and Hussain 1992:29), in conjunction with the poor performance of public tubewells in terms of timeliness and reliability of irrigation supplies, led the government to devolve responsibility for groundwater irrigation development from the public to the private sector. The first two policies adopted in Pakistan's Revised Action Plan for Irrigated Agriculture (WAPDA 1982: 16) were: Recommendation 1: Future Development of Usable Groundwater should be entrusted to Private Sector, . . . Recommendation 2: Present SCARP Tubewells in the Usable Groundwater Areas should be phased out and Replaced by Private Tubewells. Pakistan's experience suggests that private tubewell development can fulfill the objective of providing adequate vertical drainage, at least in areas of fresh groundwater (Chaudhry and Young 1990). By 1982, approximately 80 percent of total groundwater was extracted through 186,000 private tubewells, compared to 20 percent provided by 5 12,500 public tubewells (World Bank 1984).2 Increases in cropping intensities and agricultural productivity are greater under private tubewell ownership, primarily because private tubewells are more reliable (Johnson 1989:15; World Bank 1984:29). The potential gains in technical efficiency derived from public tubewells using large-capacity pumps are offset, in practice, by frequent breakdowns and inadequate maintenance. Most private tubewells provide greater water use efficiency by more closely matching water deliveries to crop needs, instead of adhering to the rigid schedules of public tubewell deliveries. However, as the government closes public tubewells, the extent to which private groundwater development will benefit a large number of farmers and meet stated equity objectives remains an important question. There is increasing interest throughout much of South Asia in water markets as a means of increasing access to and use of groundwater for irrigation.3 Much of the literature on this subject is based on field studies conducted in India and Bangladesh. This paper reviews the issues identified in this literature, in order to set the stage for an empirical study of the performance of water markets in Pakistan. 2 The large majority of tubewell development has taken place in Punjab. In 1989/90, 88 percent of the private and 65 percent of the public tubewells of Pakistan were located in that province (Pakistan, Ministry of Food, Agriculture and Cooperatives 1991:194). 3 Water markets were a major topic in the World Bank Colloquium on How to Reach the Poor Through Groundwater, in Washington DC, April 12-14, 1989. 6 Although water sales from private wells are a longstanding practice, these informal arrangements have only recently been recognized and empirically examined (Chambers, Saxena and Shah 1989:100-101).4 In most cases in South Asia, water sellers are farmers who sell surplus water after meeting the needs of their own fields. In Gujarat State in India, where water markets are highly developed, individuals and even private water companies are investing in wells primarily to sell water to others. Tubewell water sales have become a profitable enterprise for small farmers in Uttar Pradesh in India (Shankar 1992a) and even for the landless under the PROSHIKA program in Bangladesh (Wood and Palmer-Jones 1990). In Pakistan, water markets are reported in all provinces, but are most active in Punjab, where the greatest groundwater development has taken place. By 1975, over 30 percent of tubewell owners in Pakistan reported selling water, but the fraction of water sold was very small (World Bank 1984:35). A study by Pakistan's Water and Power Development Authority in canal command areas of Punjab, Sindh, and NWFP found water sales in 43 of 100 watercourses (WAPDA 1990; see also Bajwa and Ahmad 1991). Sims' (1988) micro-level study in canal-irrigated villages in the Punjab found that approximately one-third of farmers purchased groundwater from neighbors, while 29 percent owned tubewells. The potential advantages gained from groundwater market development lie in improving utilization of tubewell capacity, increasing access to irrigation water supplies 4 There are numerous anecdotal reports and a growing number of studies of private water sales in Uttar Pradesh, Haryana, Punjab, Bihar, West Bengal, Orissa, and Andhra Pradesh in India (Shankar 1992a, b; Pant 1991a, b; Kolavalli and Atheeq 1990; Kolavalli, Naik and Kalro 1992; Kolavalli, Kalro and Asopa 1989; Saleth 1991; Shah and Raju 1988). Perhaps the most highly-developed private water markets in India are found in Gujarat state, where farmers invest in wells and underground networks of pipes for water deliveries (Shah 1985; Kolavalli and Chicoine 1989). 7 (especially among farmers with small or fragmented holdings), and lowering water tables in areas of waterlogging (see Chambers, Saxena and Shah 1989; Chaudhry and Young 1990). By providing water to other farmers, tubewell owners can use a higher proportion of their well capacity than they would otherwise use on their own holdings. The availability of hired tubewell services reduces the need for other farmers to install their own wells. Because water markets increase the use of installed pumping capacity, they can improve the economic efficiency of private tubewell irrigation. Private well ownership tends to be concentrated among larger or wealthier farmers because of their ability to mobilize the necessary resources, including personal finances, credit, and government connections for electricity supplies (Chambers, Saxena and Shah 1989; Johnson 1989; Chaudhry 1990). According to the World Bank (1984:35), 70 percent of tubewells are owned by farmers with over 12.5 acres, and half of all tubewells by farmers with over 25 acres, which seems "to point toward an adverse effect of private tubewells on income distribution within agriculture." Water markets make it possible for those without wells to use groundwater for irrigation.5 The opportunity to sell groundwater can make it profitable for farmers to invest in wells even if their own holdings are too small to use the full pumping capacity (see Shankar 1992b). Dhawan concludes: the thrust of empirical research on groundwater markets, both in India and Bangladesh, has been to underscore the superiority of the institution of groundwater markets over the public tubewell system in catering to the irrigation needs of small and marginal farmers (1991:2). 5 In examining inequality of irrigation distribution, Gill and Sampath (1992) note the effect of water trading and sales, especially in Rabi season, in promoting equity. 8 Shah (1991) argues that the expansion of irrigation through water markets provides increases in cropping intensity and the demand for agricultural labor, which ultimately benefit the landless and those who rely on wage labor for household income. Increased employment opportunity is one of the biggest advantages for landless members of pump groups in Bangladesh (Wood and Palmer-Jones 1990). Other researchers on water markets voice concern regarding who appropriates the gains from irrigation (e.g. Pant 1991b). Groundwater is an open access resource, but ownership of wells and pumps is required to extract the water. The prospect of exploitative "water lords" has been raised, especially where control over water through well ownership reinforces inequality based on land and other assets (e.g. Barah 1992). Shah (1991) suggests that well owners extracting monopoly rents from the sale of water is most likely to be problematic where the markets are not competitive. Since water transactions are restricted by topography and the distance between source and field, market competition is more difficult to achieve. However, Shah (1991) suggests that the availability of groundwater resources and alternative irrigation supplies (especially canal water), a high density of wells, and the presence of lined conveyance structures can reduce the sellers' monopoly power and hence the price of water.6 Empirical research and anecdotal evidence indicate a variety of contract forms and wide range of prices in water markets. Buyers may be required to provide labor, fuel, or a share of the crop, though the tendency is to move toward a cash charge per hour of water supplied as water markets develop (Chaudhry 1990, Shah 1991). 6 Pant (1991b: 277) also observed that the relative social and economic position of buyers and sellers affects water rates. In Orissa State, India, small farmers selling water to large landowners charged less than nearby large farmers selling to small landowners. 9 Research has shown that the energy pricing structure has a major influence on the price of water in private groundwater markets (Shah 1985, 1991). In India, a flat monthly rate based on the horsepower of the engine is associated with a much lower water price than a unit charge based on electricity consumption. With the flat rate power tariff, the marginal cost of pumping is dramatically reduced, and therefore well-owners maximize their profits by pumping and selling as much water as possible (within the limitations of groundwater and power availability). Water from diesel wells is consistently sold at a higher rate than water from electric wells of similar capacity because of the higher energy, capital, and maintenance costs. Kolavalli (1989) notes that transactions are not impersonal, but are part of multi- stranded linkages in which buyers may give preference to relatives or those with whom they have other relationships, either through lower water rates or priority for service. This may be a way of dealing with high transactions costs for water sellers, particularly where water is provided on credit (see also Bardhan 1984). Detailed observations on the relationships between buyer and seller and their effects on price and reliability of irrigation services are difficult to collect, and therefore have not been carefully examined in previous studies. While several studies of water markets have dealt with the price of water (e.g. Kolavalli and Atheeq 1990; Shah 1989), there has been less analysis of the reliability of purchased private irrigation services and its impact on productivity. Chambers, Saxena and Shah (1989) cite farmers' preference for purchased irrigation water above canal supplies as evidence of quality of service, but admit the difficulty of estimating adequacy, reliability, and other indicators. Freeman, Lowdermilk and Early (1978) and Renfro 10 (1982) studied water trading and sales in Pakistan as a means of increasing farmers' control over irrigation supplies. The former used yields as a proxy indicator of quality of irrigation services; the latter used data on water and cash input use, cropping intensity, and gross income per unit area. Both studies found that, while water purchases increased productivity over canal irrigation alone, they did not have as great an effect as tubewell ownership because tubewell ownership provided a higher degree of control. The following sections of this paper use empirical data to address both productivity and equity aspects of water markets in rural Pakistan. Data on reliability of irrigation service and on agricultural production allow us to deal with the impact of water markets in greater detail than previous studies. Household surveys on various aspects of agricultural production and rural poverty conducted by the International Food Policy Research Institute (IFPRI) in Faisalabad, Attock, Dir, and Badin Districts during 1990 to 1992 provide the basis for much of the analysis. While the latter three districts were selected to represent the poorest infrastructure development in Punjab, NWFP and Sindh provinces, Faisalabad was included to represent a leading agricultural district (see Alderman and Garcia, 1991). Data on household assets and agricultural production are available from 1986 to 1992, but the last full survey round, covering the 1990-91 agricultural year, provides the greatest detail on agricultural production and irrigation, and will therefore be used in this paper. Plot-level data on soil characteristics from all sample farmers are also available from 1992. A re-survey of all tubewell owners and households participating in water markets, conducted in 1992, provides detail on these transactions and on reliability of water markets. While the study attempts to link findings 11 from the study areas to patterns of water markets indicated in other, more nationally representative studies, the findings are largely based on Faisalabad and Dir Districts. 2. WHO PARTICIPATES IN WATER MARKETS? Water markets are most prevalent in the Punjab and Northwest Frontier Provinces of Pakistan, where groundwater irrigation is most developed. Punjab contains the highest number of well-owners who sell water, as well as the highest number of private wells. However, in NWFP a higher proportion of well-owners are involved in water markets: according to NESPAK (1991) data, 25 percent of sample well-owners reported selling water in NWFP, compared to 22 percent in Punjab, 3.5 percent in Sindh, and 2.5 percent in Baluchistan.7 In the IFPRI study, water markets were found only in Faisalabad District of Punjab and Dir District of NWFP. Attock District of Punjab is a barani (rainfed) area, and no Attock farmers in our sample owned or used tubewells. The study villages in Badin District of Sindh are largely underlain by saline groundwater aquifers, which pose a serious constraint to groundwater irrigation and water market development. Only one of the sample farmers from Badin owns a tubewell, but does not sell water from it; none reported buying groundwater. 7 Provincial figures reported in the NESPAK (1991) final report are a simple average percentage of well owners selling water across all districts. The percentages reported here are a weighted average of percentage selling, with the number of tubewells in each district as the weights. 12 The study areas in Faisalabad District lie within the command area of the Rakh, Jhang, and Gugera Branches of the Lower Chenab Canal, with a relatively flat terrain. Canals provide the sole source of irrigation to 53 percent of the cultivated area in the Division (including Jhang and Toba Tek Singh Districts), with groundwater irrigating an additional 13 percent of the area, and conjunctive use of surface and groundwater on 31 percent of the area (Punjab Bureau of Statistics 1988). Groundwater use in the district is less than recharge, but there are some problems with groundwater salinity. Annual rainfall is under 500 millimeters, so cultivation is heavily dependent on irrigation. The major crops grown in Faisalabad are wheat, sugarcane, cotton, rice, and maize. Dir district has relatively hilly terrain. With higher annual rainfall (averaging 1364 millimeters), the area is less dependent on irrigation. The main sources of irrigation are small-scale surface systems, with some tubewells. The major crops are wheat, tomato, onion, and maize. The pattern of water market participation found in the IFPRI study, with greatest activity in canal-irrigated areas of Punjab and in NWFP, is largely borne out by data from the National Input Output Survey of Major Crops, which interviewed 1700 farmers distributed across all agroecological zones in Pakistan,8 with the exception of Baluchistan. Table 1 indicates that the highest proportion of farmers relying on purchased groundwater was found in the cotton/wheat zone of Punjab (Sahiwal, Bahawalnagar, Bahawalpur, R.Y. Khan, and Multan/Vehari districts), where over a third of all farmers buy tubewell water. The mixed cropping zone of Punjab, which includes Faisalabad District, had the second highest proportion of tubewell water buyers, with 8 For details on the classification of agroecological zones, see Pinkney (1989). 13 21.8 percent. Although 16 percent of farmers in the barani zone of Punjab, which includes Attock, purchase groundwater and 36 percent own tubewells, tubewell use is concentrated in Jhelum District, and is very low in Attock District itself (Punjab, Bureau of Statistics 1988:53). 14 T ab le 1 -- T yp e of ir ri ga tio n an d ac ce ss to tu be w el l w at er b y ag ro ec ol og ic al z on e P un ja b Zo ne s S in dh Z on es N W FP Z on e R ic e/ C ot to n/ Lo w C ot to n/ R ic e/ Ex ce pt W he at M ix ed W he at In te ns ity B ar an i W he at O th er D I K ha n To ta l U ni rr ig at ed 3 0 4 0 24 0 0 71 10 2 (0 .7 ) (0 .0 ) (1 .0 0) (0 .0 ) (4 8. 0) (0 .0 ) (0 .0 ) (5 1. 4) (6 .2 ) Pu bl ic ir rig at io n 10 8 27 10 6 69 0 11 9 13 6 59 62 4 s ou rc es o nl y (2 6. 5) (1 7. 3) (2 7. 4) (3 0. 4) (0 .0 ) (8 5. 0) (9 7. 1) (4 2. 8) (3 7. 9) Pu rc ha se d tu be w el l 39 1 16 14 8 3 0 5 86 w at er o nl y (9 .6 ) (0 .6 ) (4 .1 ) (6 .2 ) (1 6. 0) (2 .1 ) (0 .0 ) (3 .6 ) (5 .2 ) C an al a nd p ur ch as ed 19 33 12 1 54 0 1 1 2 23 1 t ub ew el l w at er (4 .7 ) (2 1. 2) (3 1. 3) (2 3. 8) (0 .0 ) (0 .7 ) (0 .7 ) (1 .4 ) (1 4. 0) O w n tu be w el l w at er 12 8 12 30 13 18 1 0 1 20 3 o nl y (3 1. 4) (7 .7 ) (7 .8 ) (5 .7 ) (3 6. 0) (0 .7 ) (0 .0 ) (0 .7 ) (1 2. 3) C an al a nd o w n 11 0 83 11 0 77 0 16 3 0 39 9 t ub ew el l w at er (2 7. 0) (5 3. 2) (2 8. 4) (3 3. 9) (0 .0 ) (1 1. 4) (2 .1 ) (0 .0 ) (2 4. 3) To ta l s am pl e si ze 40 7 15 6 38 7 22 7 50 14 0 14 0 13 8 16 45 (2 4. 7) (9 .5 ) (2 3. 5) (1 3. 8) (3 .0 ) (8 .5 ) (8 .5 ) (8 .4 ) (1 00 .0 ) So ur ce : C al cu la te d fr om d at a in N at io na l I np ut O ut pu t S ur ve y of M aj or C ro ps , c ol le ct ed b y A gr ic ul tu ra l U ni ve rs ity , F ai sa la ba d. A gr oe co lo gi ca l z on es de fin ed a s i n Pi nc kn ey , T . C . Th e de m an d fo r p ub lic st or ag e of w he at in P ak is ta n. I FP R I R es ea rc h R ep or t 7 7. ( W as hi ng to n, D .C .: In te rn at io na l F oo d Po lic y R es ea rc h In st itu te , 1 98 9) . N ot e: F ig ur es in p ar en th es es a re p er ce nt ag e of fa rm er s i n zo ne . a D I K ha n D is tri ct o f N W FP is in cl ud ed in P un ja b lo w -in te ns ity z on e. 15 Less than 3 percent of farmers use any groundwater in either of the zones in Sindh. Of 138 farmers interviewed in the NWFP zone, only 5 percent reported pur- chasing water from tubewells. The extent of water market participation among IFPRI sample farmers in Faisalabad and Dir districts is indicated in Table 2. Nearly half of the sample farmers in Faisalabad District purchase tubewell water, more than twice the number who own tube- wells. Of the 22 sample farmers who own tubewells in Faisalabad, only 5 reported selling tubewell water. In Dir, where groundwater irrigation is less prevalent, nine percent of all sample farmers purchase water, approximately the same proportion who own tubewells, but twice the number who sell tubewell water. Water markets are most pervasive in Faisalabad, where groundwater purchasers or sellers were found in all six study villages (Table 3). Within the villages, participation rates ranged from 0 to 16 percent of farmers (0 to 100 percent of tubewell owners) selling water, and 0 to 81 percent of farmers purchasing water. Although all villages in Faisalabad fall within the command area of public canal irrigation systems, the watercourses in Jaranwala receive almost no surface water. Thus many of the farmers in Jaranwala have invested in wells, often jointly with other farmers, giving it a significantly higher proportion of well owners (75 percent of sample farmers) than other villages. Only five of eleven study villages in Dir had any groundwater use among sample farmers, and groundwater markets were reported in three of those five villages (Table 4). The water market is most active in Katigram, where more than one-fourth of the farmers own tubewells, and nearly all well owners sell water. 16 T ab le 2 -- Sa m pl e fa rm er p ar tic ip at io n in tu be w el l w at er m ar ke t i n Fa is al ab ad a nd D ir D is tr ic ts , 1 99 2 D is tri ct Fa is al ab ad D ir To ta l Tu be w el l o w ne r 22 7 29 (2 2. 2) (7 .9 ) (1 5. 4) Tu be w el l w at er se lle r 5 4 9 (5 .1 ) (4 .5 ) (4 .8 ) Tu be w el l w at er bu ye r 49 8 57 (4 9. 5) (9 .0 ) (3 0. 3) To ta l s am pl e si ze 99 89 18 8 So ur ce : IF PR I s ur ve y da ta , 1 99 2. N ot e: Fi gu re s i n pa re nt he se s a re p er ce nt ag e of sa m pl e fa rm er s i n th e di st ric t. 17 T ab le 3 -- W at er m ar ke t p ar tic ip at io n am on g IF PR I s am pl e fa rm er s i n Fa is al ab ad D is tr ic t, by v ill ag e, 1 99 2 V ill ag e Sa dd oa na S in gp ur a Ja ra nw al a G oj ra K ha lis ab ad S um un dr i To ta l C ha k Su ba da rw al a Tu be w el l o w ne r 0 1 1 5 1 4 1 2 2 (0 .0 ) (1 6. 7) (7 5. 0) (9 .1 ) (1 8. 2) ( 5. 3) (2 2. 2) Tu be w el l w at er 0 1 3 0 0 1 5 se lle r (0 .0 ) (1 6. 7) (1 5. 0) ( 0. 0) (0 .0 ) (5 .3 ) (5 .1 ) Tu be w el l w at er 15 4 5 7 1 8 0 45 bu ye r ( 71 .4 ) (6 6. 7) (2 5. 0) ( 63 .6 ) (8 1. 8) ( 0. 0) (4 5. 5) To ta l s am pl e si ze 21 6 20 1 1 22 19 9 9 So ur ce : IF PR I s ur ve y da ta 1 99 2. N ot e: Fi gu re s i n pa re nt he se s a re p er ce nt ag e of sa m pl e fa rm er s i n th e vi lla ge . 18 TUBEWELL OWNERS What are the characteristics of tubewell owners and water purchasers? Table 5 presents a logistic regression (logit) model used to examine tubewell ownership among sample farmers in Faisalabad and Dir districts. The logit technique allows us to examine the effect of a number of variables on the underlying probability of a dichotomous dependent variable, such as the probability of owning a tubewell. In this model, land ownership, age of head of household, whether a household has a member who has worked or is working abroad, and dummy variables for Jaranwala village and Dir district (areas with less access to canal irrigation) are hypothesized to influence the probability of owning a tubewell. The dummy variables are proxy indicators for availability of alternative water supply. Other indicators of water supply, such as position of farm relative to canal systems and discharge in the watercourse, might refine the model, but are difficult to quantify and measure. Household wealth or income are not included in the model because it is likely that tubewell ownership has contributed to wealth or income, rather than the reverse. Similarly, factors such as cropping pattern, which influences demand for tubewell water, are not included because no indicator is available for farmers' desired cropping pattern, and availability of tubewell water has a stronger influence on cropping pattern than actual cropping pattern has on availability of tubewell water. 19 T ab le 4 -- W at er m ar ke t p ar tic ip at io n am on g IF PR I s am pl e fa rm er s i n D ir D is tr ic t, by v ill ag e, 1 99 2 V ill ag e K at ig ra m B at an S ha h A la m K ha np ur K am an ga ra 6 O th er T ot al B ab a V ill ag es Tu be w el l o w ne r 5 0 1 0 1 0 7 ( 27 .8 ) ( 0. 0) (1 4. 3) (0 .0 ) (2 0. 0) (0 .0 ) (7 .9 ) Tu be w el l w at er 4 0 0 0 0 0 4 se lle r (2 2. 2) (0 .0 ) (0 .0 ) ( 0. 0) (0 .0 ) ( 0. 0) (4 .5 ) Tu be w el l w at er 1 3 0 4 0 0 8 b uy er (5 .6 ) ( 25 .0 ) (0 .0 ) (2 1. 1) (0 .0 ) ( 0. 0) (9 .0 ) To ta l s am pl e si ze 1 8 1 2 7 19 5 2 8 89 So ur ce : IF PR I s ur ve y da ta , 1 99 2. N ot e: F ig ur es in p ar en th es es a re p er ce nt ag e of sa m pl e fa rm er s i n th e vi lla ge . 20 Table 5--Results of logistic regression model for tubewell ownership Independent Wald Variables Units Coefficient T Ratio Statistic Size of land ownership acres .122 ** 4.03 16.24 Age of head of household years .051 ** 2.34 5.48 Relative abroad dummy 1.668 ** 2.15 4.63 Jaranwala village dummy 4.458 ** 5.41 29.32 Dir district dummy .036 .05 .00 Constant -6.829 ** -4.35 18.90 Model Chi-Square = 66.9 ** with 5 degrees of freedom Number of observations = 182.0 Classification Table for Tubewell Ownership Predicted Percent NOT OWNER OWNER Correct Observed NOT OWNER 147 7 95.4 OWNER 12 16 57.1 Overall 89.6 Source: IFPRI survey data, 1991/92. ** Significant at 5 percent probability level * Significant at 10 percent probability level 21 Results of this model indicate that land ownership has a strong positive effect on well ownership, implying that households owning more land are more likely to own wells. The age of head of household has a significant positive effect on well ownership, perhaps because farmers invest in tubewells as the household becomes established. Households with a member currently working abroad or returned from abroad are also significantly more likely to own wells. This seems to indicate that remittances are a source of financing for tubewell investment.9 The dummy variable for Jaranwala village has a large and significant coefficient. As noted above, the lack of alternative canal irrigation supplies has pushed these farmers to purchase tubewells, and joint investment has enabled even small farmers in this village to own at least a partial share of a well. The pattern of well ownership in Dir district, however, is not significantly different from that of Faisalabad district. This model correctly predicts the well ownership status of 90 percent of all cases. 9 The reverse direction of causality--that income derived from tubewell ownership has financed international migration--is unlikely. Adams' (1992) study of migration among households in the IFPRI sample found that households with less than an acre of irrigated land were most likely to migrate. 22 Although small holding size is not an insurmountable obstacle to well ownership (as demonstrated by a high proportion of joint well owners with small holdings in Jaranwala village), it is a constraint to widespread tubewell ownership. Tenants, especially those with no land of their own, are at a disadvantage in tubewell ownership because they do not have secure enough rights to land on which to install a tubewell, and are likely to face credit constraints for tubewell investment (see Malik, Broca and Gill 1992). In the survey on water markets, over 60 percent of groundwater purchasers cited the expense of purchasing a tubewell as the reason why they did not have their own wells, but 25 percent cited a lack of land ownership or too small a holding size as the reason for not investing in a well (Table 6). Groundwater quality problems also prevent farmers from installing their own wells. Water markets meet a need for water among those who have too little land, cannot afford tubewells, or find the investment not worthwhile, and those who have problems with the groundwater quality on their own land. TUBEWELL WATER PURCHASERS A logistic regression model, similar to that for tubewell ownership, has been calculated to identify factors which predict who purchased tubewell water during rabi and kharif of 1991-92 (Table 7).10 Since remittances are less likely to have an impact on water purchases than on investment in tubewells, the variable for relatives abroad is omitted from this model, but a variable for season is added to see if there is a significant difference between rabi and kharif irrigation purchases. As in the model for tubewell 10 Because of the small number of tubewell owners in the sample, it is not possible to develop a model to predict which tubewell owners sell water. 23 ownership, cropping patterns are not included because they are determined largely by the availability of water. The location of fields relative to the canal system and to tubewells whose owners are willing to sell, along with ground- water quality are likely to affect water purchases, but these factors are not included because the data are unavailable.11 Table 6--Water buyers' reasons for not owning tubewells District Faisalabad Dir Total Too expensive 40 14 54 (54.1) (93.3) (60.7) Holding too small 11 0 11 (14.9) (0.0) (12.4) Not landowner 12 0 12 (16.2) (0.0) (13.5) Land not near canal 1 0 1 (1.4) (0.0) (1.1) Groundwater quality 6 1 7 (8.2) (6.6) (7.8) Only buy when own TW broken 3 0 3 (4.1) (0.0) (3.4) Purchase as supplement only 1 0 1 (1.4) (0.0) (1.1) Total number of water buyers 74 15 89 Source: IFPRI survey data, 1992. Note: Figures in parentheses are percentage of water buyers. 11 Tubewell ownership was not included in the model because of the high multicollinearity between land ownership and tubewell ownership. Similarly, operational holding size was not included because it is highly correlated with land ownership. An alternative specification of the model, with operational holding instead of land ownership, did not show a significant effect of holding size on water purchases. 24 Table 7--Results of logistic regression model for tubewell water purchase Independent Wald Variables Units Coefficient T Ratio Statistic Size of land ownership acres - .039 ** -2.28 5.22 Age of head of household years - .031 ** -3.30 10.87 Season dummy - .355 -1.24 1.54 Jaranwala village dummy -1.398 ** -3.38 11.46 Dir district dummy -3.262 ** -8.15 66.50 Constant 2.250 ** 3.98 15.82 Model Chi-Square = 118.4 ** with 5 degrees of freedom Number of observations = 352.0 Classification Table for Tubewell Ownership Predicted Percent NOT BUYING BUYING Correct Observed NOT BUYING 221 31 87.7 BUYING 36 64 64.0 Overall 81.0 Source: IFPRI survey data, 1990-1992. ** Significant at 5 percent probability level * Significant at 10 percent probability level 25 This model shows that, whereas the size of land ownership and the age of household head have a strong positive effect on tubewell ownership, these variables have a significant negative effect on water purchases.12 Thus younger households with less land are more likely to purchase groundwater than older households owning substantial amounts of land. Tenants are likely to be dependent on other households' tubewells, as well as other households' land, for their cultivation. Farmers in Dir are significantly less likely to purchase groundwater than those in Faisalabad, in part because of the lower availability of tubewells in Dir.13 Farmers in Jaranwala are also significantly less likely to purchase water. In this village joint ownership, rather than water markets, provides small farmers with access to groundwater. Because alternative sources of irrigation are not available, farmers in that village seek to assure themselves of access to groundwater by investing in wells rather than depending on groundwater purchases. The season does not have a significant effect on water purchases: 30 percent of farmers reported purchasing irrigation in kharif, compared to 25 percent in rabi. Land ownership and age are indicators of overall status of farm households. Investment in tubewells are not made for prestige, but the status of households can enable them to mobilize the resources needed for tubewell investment, including financial resources and government assistance (such as electricity connections). Therefore, it is 12 In a logit model for groundwater purchasing, using cross-sectional survey data from 5 states in India, Saleth (1991) also found a significant negative effect of farm size on likelihood of purchasing in 3 of 5 states. The other two states are characterized by very small and fragmented holdings and higher average rainfall. Thus the need for supplemental groundwater was less, and the larger farmers in those states were as likely to purchase groundwater as small farmers. 13 The effect of number and density of tubewells in a village was tested in an alternate specification of the model. Tubewell density has a significant positive effect on the likelihood of water purchases, both in addition to the dummy variables for Dir and Jaranwala, and without the dummy variables included. The variable for tubewell density is not included in the final model because there are multicollinearity problems when it is included along with the dummy variables for location, and tubewell density does not explain as much as the two dummy variables. 26 not surprising that higher-status households are more likely to own wells, and lower- status households are more likely to rely on tubewell water purchases.14 However, not only low-status households purchase water: 7 of 28 tubewell owners in the IFPRI sample also purchase water. Water purchases may provide a backup when a farmer's own well is not functioning, or may be used to irrigate land that cannot be served by a farmer's well. In several cases, farmers preferred buying water to operating their own wells because purchased water from electric-powered wells was cheaper than using their own tractor- powered tubewells. Results of these model indicate that, whereas private tubewells are likely to be owned by large farmers, water markets improve equity of groundwater use by making water available to small landowners or tenants and younger households--those farmers who are least likely to own tubewells. In Faisalabad, where water markets are most active, they provide the only access to groundwater for approximately half of the farmers who own less than 12.5 acres. 14 A comparable pattern of larger landowners owning wells and smaller landowners purchasing tubewell water, based on National Input Output Survey data from the Punjab mixed cropping zone, is shown in Appendix Table 1. 27 3. RELATIONSHIPS BETWEEN WATER BUYERS AND SELLERS PHYSICAL RELATIONSHIPS Water markets are not perfectly competitive markets in which buyers are free to choose among a number of sellers. In many areas there are not a large number of water sellers, and, under most conditions prevailing in Pakistan, tubewell irrigation water is not a commodity which can be transported far from the source to the area of application. Conveyance losses between the tubewell and the field restrict purchasers to buying from tubewells located in close proximity of their fields. The distance over which it is feasible and economically viable to transmit water depends on the soils, topography, and type of channel used to convey the water. In the IFPRI study, the average distance between the tubewell and purchasers' fields was 600 meters in Faisalabad District, and 180 meters in Dir, which has more undulating topography. Use of lined watercourses or field channels, which have lower transmission losses than unlined channels, increases the distance over which water can be transported. Ten of the thirteen cases in which the distance between source and fields was over 1000 meters used lined watercourses (including one case in which water travelled down 3 kilometers of lined watercourse between the well and field). Lined canals and pipes ensure that water purchasers receive more of the water they pay for from the tubewell, and permit sales to a wider potential number of fields from each tubewell.15 Thus, they go hand in hand with the development of competitive water markets. They allow purchasers to obtain water within a wider radius of their 15 Underground pipes can even, to some extent, overcome topographic limitations to water sales, by enabling water to reach fields at a higher level than the tubewell. 28 fields, thereby increasing the number of potential suppliers. Shah and Raju (1988) report that as competitive water markets developed in Gujarat state, India, tubewell water sellers who wanted to maintain clients install lined conveyances to ensure that water reaches as many buyers as possible with low losses. Despite these advantages of water markets, there has been little private investment in lining or pipes in the IFPRI sample areas. Four farmers reported using lined field channels to convey purchased tubewell water part of the way (though in two of these cases the lined field channels were only the first 20 meters from the tubewell). Three sellers used underground pipes, which have the lowest conveyance losses. Pukka (lined) watercourses are used more frequently than lined field channels or pipes because watercourse lining results from government and collective farmer investment, while lining field channels or installing pipes requires considerable private investment. Farmers use watercourses for tubewell water despite the Canal and Drainage Act provision that all who do so are assessed the water rate for canal irrigation use. A NESPAK (1991) study suggests that this law restricts the sale of tubewell water, and recommends allowing farmers to use watercourses for tubewell water without charge to encourage water markets and the mixing of marginal-quality tubewell water with fresh canal water supplies. The Canal and Drainage Act further restricts transporting tubewell water by prohibiting farmers from carrying water across public watercourses. It may be worth lifting this restriction, provided the pipes or other structures used to carry the tubewell water do not block or erode the watercourse. 29 Renfro's (1982) study notes an association between private tubewells and collective activity among farmers, particularly with regard to watercourse lining.16 Renfro and Sparling (1986:206) suggest the reason for this is that "Farmers with cooperative neighbors are more likely to invest in tubewells, and the presence of private tubewells gives farmers new reasons to cooperate with each other." However, this explanation omits the role of watercourse lining in reducing transmission losses of high- value groundwater. An alternative explanation is that, with tubewell use in general, and water market sales in particular, farmers recognize the value of canal lining and have greater incentive to reduce water losses. With lined watercourses, tubewell water can be conveyed over a greater distance between the well and fields, thus expanding the potential market from tubewells along the watercourse. Renfro and Sparling (1986:206) argue that watercourses with private tubewells are less in need of lining because they have additional sources of water. However, watercourse rehabilitation not only conserves canal water, but by reducing transmission losses of tubewell water, lining can also encourage the development of competitive water markets. Therefore, in areas where watercourse lining is to be done, it may be appropriate to give priority to lining watercourses with private tubewells as a means of fostering water markets.17 SOCIAL RELATIONSHIPS Physical proximity is not the only relevant relationship which influences the development of competitive water markets. Social relationships between buyer and seller 16 Under the On-Farm Water Management projects implemented by the Government of Pakistan with USAID and World Bank assistance, farmers are required to organize into Water Users' Associations in order to receive government assistance for watercourse improvement (see Byrnes 1992). 17 Lining watercourses will also reduce groundwater recharge to some extent, and thus reduce availability of tubewell water. However, there will continue to be recharge from irrigated fields. 30 may also restrict the sale and purchase of groundwater if tubewell owners are only willing to sell to close relatives or those with whom they have other ties. This does not appear to be a problem in the IFPRI study areas. Only 22 percent of water market transactions in Faisalabad District were between close relatives. Approximately one third (37 percent) of transactions were between members of the same biradari, which repre- sents a broader social grouping. Sale of tubewell water between kin is even more rare in Dir, where only 2 percent of transactions were between close relatives or biradari members. There, water market transactions were more likely to follow patron-client ties, with 37 percent of sales reported between landlord and sharecropper (compared to less than 1 percent in Faisalabad District). As noted above, selling water to relatives is a means of controlling transactions costs and ensuring fee repayment. Relatives may also have the closest land holdings, due to inheritance patterns. However, transactions costs may be higher with relatives, either because of quarrels or difficulty in collecting payments. Shah (1992) hypothesizes that as water markets develop, they become de-personalized. This seems to have taken place in the study areas, because personal relationships neither restrict access to groundwater nor are shown to have a significant effect on the reliability of deliveries, as discussed below. 4. NATURE OF WATER MARKET CONTRACTS A flat charge per hour of pumping is the most common form of water market contract in both Faisalabad and Dir districts (Table 8). This type of arrangement occurs under diesel, tractor, and electric-powered pumpsets. Water from diesel pumpsets in Jaranwala is commonly sold under an arrangement whereby the buyer supplies the diesel 31 and motor oil for the pump, and pays an additional fee of Rs 4 to Rs 6 per hour to the well owner to cover the wear and tear on the engine. Sharecropping contracts for water are used under both diesel and electric tubewells in Dir. Table 8--Water market contracts, by type of pump Type of Pump Diesel Tractor Electric Total Faisalabad District Flat charge per hour 9 19 44 72 Buyer brings fuel 18 0 0 18 Share of crop 0 0 0 0 Total 27 19 44 90 Dir District Flat charge per hour 13 0 0 13 Buyer brings fuel 0 0 0 0 Share of crop 2 0 6 8 Total 15 0 6 21 Source: IFPRI survey data, 1992. Note: Table includes number of sellers' and buyers' responses about type of contract. Prices under the hourly charge system range from Rs 14 to Rs 80 per hour, depending on the pump type, capacity, and location (see Table 9). The higher price of water from tractor tubewells reflects the higher cost of operating this type of pump. The average price of water under the hourly charge system is approximately the same for diesel and electric tubewells, although the former are usually more expensive to operate. The average capacity of the electric tubewells is higher, though, so the cost per horsepower is lower for electric than diesel tubewells. The mean hourly cost of water to 32 the purchasers from diesel tubewells is slightly higher under the buyer-brings-fuel system than under the flat hourly charge. Water sellers with diesel pumps are apparently only recovering their own costs under either type of contract.18 The sellers' transactions costs in acquiring the fuel and operating or supervising the operations of the pump are presumably higher under the hourly charge contracts, but there may be an unwillingness to let some purchasers operate the pumps themselves under the buyer-brings-fuel system. Among IFPRI sample villages, the buyer-brings-fuel contract was only found in Jaranwala, where there is also a high incidence of joint ownership of wells. However, this type of contract is also reported in other areas with conjunctive canal and tubewell irrigation, such as in southern Punjab. All water transactions under hourly charge contracts in Dir are found in Khanpur. The price is Rs 40 to 80 per hour, which is higher, on average, than in Faisalabad. Several factors could account for the higher price in Khanpur: the well from which most farmers purchase is large-capacity, powered by a 113-horsepower truck engine, and therefore more expensive to operate.19 Irrigation water is also more scarce in Dir than in Faisalabad, where canal water is more readily available and groundwater tables are generally higher. A final consideration may be that most water purchasers in Khanpur are buying water from their landlord, whereas that is only found in one case in Faisalabad. 18 Unfortunately, much of the information on price of purchased tubewell water comes from water buyers, rather than from the sellers. There are thus not enough data on tubewell operations costs and water delivery rates to determine the profit margin for water sales or the exact price per unit water pumped. 19 The price per horsepower is lower in Dir than Faisalabad, but this may be misleading because the relationship between horsepower and water delivery is not linear, particularly when comparing the pumpset powered by a truck engine with lower-horsepower engines designed for tubewells. 33 Table 9--Average cost of tubewell water, by type of pump and contract Type of Pump Diesel Tractor Electric Faisalabad District Flat charge (Rs per hour) 29.44 43.95 27.82 (8.08) (7.56) (7.77) Buyer brings fuel (Rs per hour) 32.06 n.a. n.a. (5.39) Dir District Flat charge (Rs per hour) 49.23 n.a. n.a. (17.54) Share of crop (percent) 25.00 n.a. 23.15 (0.00) (2.31) Source: IFPRI survey data, 1992. Note: Costs computed from sellers' and buyers' responses. Figures in parentheses are standard deviations. n.a. not applicable. A larger sample of water sellers and purchasers under different ecological and socioeconomic conditions would be necessary to estimate the effect of these factors on the cost of private tubewell water. It does not appear, however, that the prices reported under the hourly rate or buyer-brings-fuel type of contracts represent a large profit to the tubewell owner. Thus, concerns over water sellers appropriating the value of groundwater do not seem justified, particularly in the Faisalabad area. Sharecropping contracts for tubewell water are only applied to tomato, onion, and some maize cultivation in Dir. The standard rate is 25 percent of the crop. Three water sellers reported giving a different rate to their tenants: 20 percent as the share for the water (in addition to the share for the land), or 50 percent for the land and water combined. The use of sharecropping contracts for provision of water in Dir may reflect 34 the greater prevalence of sharecropping for land in that area than in Faisalabad. Sharecropping contracts for water are also reported for rice and berseem crops in other regions (Chaudhry 1990; Dr. Muhammad Jameel Khan, personal communication, March 1992). The extent of crop share contracts for water may be underestimated where the landlord supplies both land and tubewell water. While tubewell irrigation may then be considered as one of the inputs which the landlord provides (such as fertilizer or plowing services), to do so masks the importance of timing and reliability of irrigation service in the overall production process. It is noteworthy that sharecropping for tubewell water is practiced under the cultivation of crops such as tomatoes, onions, or rice, which are sensitive to moisture stress at critical periods. In sharecropping contracts, the water seller has a stake in the outcome of the crop, and a share in the risk if the water supply does not meet crop needs. Therefore, the seller has an incentive to supply tubewell water in an adequate and timely manner. This is not as critical for crops less susceptible to the timing of irrigation, or where alternate sources of irrigation are readily available. Chaudhry (1990) and Shah (1991) have suggested that, as water markets develop, there is a tendency to move toward cash contracts. If, however, sharecropping for water offers a greater incentive for sellers to provide reliable irrigation service, this type of contract may remain for water-sensitive crops. Further empirical research on the provision of tubewell water in different agroecological zones and for different crops is necessary to establish whether risk-sharing is a significant consideration in the choice of contract and timeliness of irrigation service. 35 5. AGRICULTURAL PRODUCTIVITY UNDER WATER MARKETS Previous studies have shown clear productivity gains to farmers purchasing groundwater over those using only public canal or public tubewell supplies, but the gains were much less than those obtained by tubewell owners. The wheat and cotton yield increases of tubewell water purchasers (compared to those with canal water only) were half as great as the yield increases for tubewell owners in Freeman, Lowdermilk and Early's (1978) study. For rice the gap was narrower: water purchasers obtained 78 percent of the yield increases of tubewell owners (see Table 10).20 A study of private tubewells by WAPDA (1980, cited in World Bank 1984) found that overall cropping intensity and the proportion of area under water-consumptive crops was higher for tubewell owners than for water purchasers. There was also a yield gap between water purchasers and tubewell owners for sugarcane, rice, wheat, and vegetables (Table 11). Part of the difference in yields may be due to lower applications of irrigation water and complementary inputs such as fertilizer and insecticides by tubewell purchasers than by owners (even though tubewell purchasers used more inputs and had higher yields than non-users for almost all crops). Renfro (1982) found that the cropping intensities, the proportion of area 20 A WAPDA (1990) study also assesses the productivity impact of purchased water. However, the yield differentials are based on farmers' assessments of what their yields would be with and without privately purchased water, and are thus not as reliable as comparisons of actual yields of farmers with and without purchased water. 36 Table 10--Average yields of major crops, by water source in Freeman, Lowdermilk and Early's (1978) study. Canal Public Purchased Own Crop Only Tubewell Tubewell Tubewell (kg/acre) Wheat 672 747 784 896 Rice 522 709 784 859 Cotton 261 299 373 485 Source: D. M. Freeman, M. K. Lowdermilk, and A. C. Early. "Farm irrigation constraints and farmers' responses: Comprehensive field survey in Pakistan". (Water Management Technical Report No. 48-E, Volume V, Colorado State University, Fort Collins, CO, 1978). Note: All tubewell water is in addition to canal supplies. 37 T ab le 1 1- -S um m ar y of in pu t u sa ge a nd y ie ld s f or tu be w el l u se rs a nd n on -u se rs in W A PD A st ud y Ite m U ni t Ty pe Su ga rc an e R ic e G ar de ns V eg et ab le C ot to n W he at Pu ls es O ils ee ds O th er s To ta l 1. C ro pp in g pa tte rn % a cr es O * 8 21 4 3 8 60 15 8 18 15 7 P* 5 16 2 2 8 36 13 13 19 13 6 N u* 3 7 1 1 7. 5 50 16 11 15 11 3 2. P er a cr e us e of : i. N itr og en 50 k g O 1. 5 1. 5 0. 5 0. 9 0. 5 1. 0 - 0. 2 0. 5 ba g P 1. 0 1. 3 0. 5 0. 5 0. 5 0. 75 - 0. 1 0. 4 N u 1. 0 1. 0 0. 4 0. 5 0. 2 0. 5 - - 0. 2 i i. Ph os ph or us 50 k g O 0. 25 0. 5 0. 2 1. 0 0. 25 0. 75 0. 1 - 0. 2 ba g P 0. 2 0. 5 0. 2 0. 5 0. 1 0. 6 - - - N u 0. 2 0. 4 0. 1 - 0. 1 0. 2 0. 2 - 0. 1 ii i. Se ed ra te M au nd s O 67 0. 13 13 0 30 0 0. 15 0. 9 0. 6 0. 1 50 or R s P 71 0. 12 15 0 30 0 0. 14 0. 8 0. 6 0. 1 50 N u 53 0. 13 15 0 30 0 0. 11 0. 9 0. 7 0. 1 50 iv . I ns ec tic id e R s O 14 11 .0 50 - 25 1. 0 - - - P 18 10 .5 50 - 13 - - - - N u 7 11 .2 50 - 17 - - - - v . C an al w at er A cr e- fe et O 1. 5 1. 5 2. 0 1. 5 0. 9 0. 6 0. 2 0. 1 0. 4 P/ N u 1. 2 1. 2 1. 5 1. 2 0. 7 0. 4 0. 2 0. 1 0. 3 v i. Tu be w el l d el ta A cr e- fe et O 2. 0 2. 0 1. 1 0. 7 0. 3 0. 5 - - 0. 5 P 1. 0 1. 5 1. 0 0. 6 - 0. 3 - - 0. 3 3. Y ie ld p er a cr e M au nd s O 59 5. 0 32 .1 23 .6 24 50 .0 16 80 .0 9. 3 26 .3 9. 3 9. 1 60 0. 0 or R s P 48 5. 0 29 .3 22 .9 25 73 .0 15 95 .0 8. 5 21 .7 10 .4 8. 9 60 0. 0 N u 31 5. 0 21 .4 18 .7 21 38 .0 10 30 .0 9. 2 18 .5 10 .8 9. 7 60 0. 0 So ur ce : W A PD A , " Pr iv at e Tu be w el l a nd F ac to rs A ff ec tin g C ur re nt R at e of In ve st m en t," A nn ex ur e IV -3 . 19 80 . * O = T ub ew el l o w ne r, P = Tu be w el l w at er p ur ch as er a nd N u = N on -u se r o f t ub ew el l w at er . 38 under water-consumptive crops, and the gross income per acre achieved by tubewell water purchasers more closely approximated that of farmers who only received canal water than that of tubewell owners, even though their cash and labor inputs were virtually as high as those of tubewell owners (Table 12). In part, water buyers may have lower cropping intensities and yields than tubewell owners because buyers choose to use less water due to the cost of purchased tubewell water. However, the price of water for tubewell purchasers in the IFPRI sample was not much greater than the cost to tubewell owners (except for owners of electric pumpsets with fixed electricity charges, who face a very low marginal cost and therefore have an incentive to pump as much water as can be used). Whether tubewell water purchasers use less groundwater based on an input allocation decision or supply constraints is unclear. As discussed below, there are numerous occasions on which tubewell water is not available to water buyers at any cost, despite their demand for it. The lower reliability of purchased tubewell water compared to owned tubewell water is likely to be a major contributor to any yield or income gap between tubewell owners and water purchasers. Renfro (1982:83) concludes that, in comparison with water purchasers, "obviously actual sampled tubewell owners can exert more control over water supplies with favorable impacts on productivity." The differences in cropping pattern between tubewell owners, water purchasers, and non-users of tubewell water are not as clear in the IFPRI sample villages as in the WAPDA (1980) and Renfro (1982) studies. Table 13 examines the cropping pattern in Faisalabad and Dir districts by source of irrigation. 39 Table 12--Input use and agricultural productivity in Renfro's (1982) study Canal Water Tubewell Tubewell Only Buyers Owners Total Gross crop income 3018 3475 4659 3297 (Rs/acre) (1081) * (1632) * (2029) (1453) Canal water use/ 26.3 26.2 25.2 26.0 acre (acre minutes) (9.5) (5.6) (6.7) (9.2) Tubewell water use/ 0.0 14.2 31.4 7.9 acre (acre minutes) (0.0) * (13.3) * (21.9) (14.9) Cash input expenditure 309 385 388 344 (Rs/acre) (156) (158) (86) (198) Labor use 73.8 76.2 75.5 74.0 (mandays/acre) (37.8) (35.4) (46.4) (37.3) Cropping intensity 160 168 184 164 (percent) (25) (28) (23) (26) Percent high water 35 36 45 36 using crops (17) (22) (20) (19) Sample size 69 50 10 129 Source: R. Z. H. Renfro. "Economics of local control of irrigation water in Pakistan: A pilot study". (Ph. D. diss., Colorado State University, Fort Collins, CO, 1982). Note: Figures in parentheses are standard deviations. * Difference between categories significant at 0.05 probability level. In Faisalabad, the average total cropping intensity for tubewell owners, water purchasers and non-tubewell users is 176 percent. In Jaranwala, where there is no alternative irrigation source, tubewell water purchasers have a slightly higher cropping intensity than owners (182 compared to 176 percent--though the differences are not significant). In Dir, tubewell owners have the highest average cropping intensity (197 percent), followed by non-tubewell users (171 percent) and water purchasers (167 percent). 40 The proportion of area under individual crops shows no clear pattern across the sample. For example, tubewell owners in Faisalabad plant more fodder, wheat, and sugarcane than other crops, while wheat is the major crop for water purchasers, followed by fodder and sugarcane. Non-tubewell users in Faisalabad plant the greatest proportion of their land in sugarcane, an extremely water-consumptive crop, followed by wheat. In Jaranwala, both tubewell owners and water purchasers plant a greater amount of fodder than do farmers in other Faisalabad villages. In Dir, tubewell owners plant 62 percent of their land in fodder, while water purchasers (who are largely tenants) plant only 5 percent and non-tubewell users plant 21 percent. Dir farmers, particularly tubewell owners and water purchasers, also plant a large area under wheat and maize, as well as substantial area under tomato and onion. Further analysis of the net returns to total farm operations would be necessary to understand the relationship between crop choice and type of irrigation. 41 T ab le 1 3- -C ro pp in g pa tt er n by a cc es s t o tu be w el l w at er , F ai sa la ba d an d D ir D is tr ic ts P er ce nt o f T ot al A cr es U nd er To ta l O th er O th er C ro pp in g W he at R ic e Su ga rc an e Fo dd er M ai ze Pu ls es C ot to n O ils ee ds To m at o O ni on V eg et ab le s C ro ps In te ns ity Fa is al ab ad - To ta l Tu be w el l o w ne r 59 2 30 70 1 0 4 0 0 0 8 0 17 5 (n =2 2) (2 4) (6 ) (3 1) (4 4) (4 ) (0 ) (1 1) (0 ) (0 ) (0 ) (2 1) (0 ) (2 2) Tu be w el l w at er b uy er 71 2 25 49 8 0 15 0 0 0 5 0 17 6 (n =4 6) (1 9) (7 ) (2 4) (3 1) (1 8) (0 ) (2 0) (1 ) (0 ) (0 ) (1 7) (1 ) (2 7) N on -tu be w el l u se r 48 1 68 42 8 1 5 1 0 0 3 0 17 7 (n =2 4) (3 0) (4 ) (4 7) (4 7) (1 1) (5 ) (1 0) (4 ) (0 ) (0 ) (1 4) (0 ) (3 7) Ja ra nw al a Tu be w el l o w ne r 57 4 26 88 0 0 0 0 0 0 0 0 17 6 (n =1 5) (2 8) (7 ) (3 6) (4 0) (0 ) (0 ) (0 ) (0 ) (0 ) (0 ) (0 ) (0 ) (2 1) Tu be w el l w at er b uy er 71 7 26 76 0 0 0 0 0 0 0 2 18 2 (n =5 ) (2 2) (1 5) (4 3) (3 4) (0 ) (0 ) (0 ) (0 ) (0 ) (0 ) (0 ) (3 ) (3 0) Fa is al ab ad o th er V ill ag es Tu be w el l o w ne r 61 0 37 32 3 0 14 0 0 0 26 0 17 3 (n =7 ) (1 3) (0 ) (2 0) (1 8) (7 ) (1 ) (1 5) (0 ) (0 ) (0 ) (3 3) (0 ) (2 5) Tu be w el l w at er b uy er 71 2 24 46 9 0 17 0 0 0 6 0 17 5 (n =4 1) (1 9) (5 ) (2 1) (3 0) (1 9) (0 ) (2 1) (1 ) (0 ) (0 ) (1 8) (0 ) (2 7) N on -tu be w el l u se r 48 1 68 42 8 1 5 1 0 0 3 0 17 7 (n =2 4) (3 0) (4 ) (4 7) (4 7) (1 1) (5 ) (1 0) (4 ) (0 ) (0 ) (1 4) (0 ) (3 7) D ir - A ll V ill ag es Tu be w el l o w ne r 50 0 0 62 49 1 0 0 17 19 0 0 19 7 (n =4 ) (4 1) (0 ) (0 ) (9 3) (5 6) (2 ) (0 ) (0 ) (3 3) (3 2) (0 ) (0 ) (7 ) Tu be w el l w at er b uy er 44 1 0 5 40 5 0 4 30 23 5 11 16 7 (n =8 ) (2 5) (5 ) (0 ) (8 ) (4 0) (1 0) (0 ) (9 ) (3 3) (3 5) (1 0) (1 3) (4 1) N on -tu be w el l u se r 64 3 0 21 48 4 0 2 16 8 0 6 17 1 (n =7 3) (3 5) (1 4) (0 ) (3 8) (3 8) (1 0) (0 ) (7 ) (2 6) (1 8) (1 ) (1 8) (4 2) So ur ce : IF PR I s ur ve y da ta , 1 99 0- 19 92 . N ot e: F ig ur es in p ar en th es es a re st an da rd d ev ia tio ns . 42 In order to examine the impact of different sources of irrigation on yields, a production function was estimated using plot-level data for the 1990-91 agricultural year. Due to limited degrees of freedom for other crops in the sample, this equation was estimated for wheat only, a staple crop grown by nearly all farmers in both Faisalabad and Dir. Table 14 shows the results of this estimation, using linear regression.21 Seeding rate, total fertilizer applications (defined as kilograms of elemental Nitrogen and Phosphorous per acre), total labor inputs, soil characteristics of pH, potassium, phosphorous, and salinity are included in the model along with the number of irrigation applications from own tubewells, purchased groundwater, and canal water. Soil pH has been transformed to degree of alkalinity, a variable computed by subtracting 7 from to the original pH value.22 Salinity is represented by a dummy variable indicating if measured electrical conductivity levels are greater than or equal to 4 millimhos per centimeter, the threshold level for average crop tolerance of salinity. 21 Alternative functional forms, such as Cobb-Douglas and log-linear, were tested, but did not fit the data as well as linear regression. The large number of cases with values of 0 for one or more of the independent variables, notably the irrigation inputs, may account for the poor fit of the Cob-Douglas equation. Quadratic and interaction terms were tested, but found not significant, and are therefore not included in the model. 22 Original pH on sample plots ranges from 7.0 (neutral) to 8.5 (alkaline). 43 Table 14--Effect of irrigation applications on plot-level wheat yields in Faisalabad and Dir Districts Independent Standard T Variable Variables Coefficient Error Statistic Mean Seeding rate (kg/acre) 3.60 ** 1.82 1.98 40.93 Fertilizer (N + P kg/acre) 4.67 ** .73 6.09 47.12 Labor (person-days/acre) 1.89 * 1.12 1.68 27.86 Degree of alkalinity (adjusted pH) 253.54 ** 69.20 3.66 0.62a Soil Potassium (ppm/acre) 1.25 ** .38 3.32 128.14 Soil Phosphorous (ppm/acre) -4.50 4.82 -.93 10.07 Soil salinity dummy -44.61 68.99 -.65 .13b Canal irrigations 31.14 ** 9.00 3.46 2.53 Purchased tubewell irrigations 44.58 ** 16.66 2.68 .62 Own tubewell irrigations 48.31 ** 18.45 2.62 .50 Constant -63.16 112.20 -.56 Adjusted R Square = 0.31 ** Number of observations = 263.0 Source: IFPRI survey data, 1990-1992. a Degree of alkalinity = soil pH - 7.0. b Variable equals 1 if electrical conductivity > 4 mmhos/cm, 0 otherwise. ** Significant at 5 percent probability level * Significant at 10 percent probability level The seeding rate and amount of nitrogen and phosphorous fertilizer have a strong positive effect on wheat yields.23 Total labor inputs, including family, exchange, permanent hired, and casual hired labor are also associated with higher yields. The level of potassium in the soil and degree of soil alkalinity are positively associated with yields. Higher pH values influence yields because slightly alkaline soils (those with a pH above 7.0) are characterized by greater nitrogen, phosphorous, and potassium availability. The 23 A single variable for the sum of nitrogen and phosphorous fertilizer is used because the levels of these two inputs are multicollinear. If N and P are included as separate variables in the model, both have significant coefficients of approximately the same magnitude as the total fertilizer coefficient (4.4) in the final model. 44 coefficients for other soil characteristics--phosphorous content and salinity are not significant. The lack of a significant effect of electrical conductivity on wheat yields is important because in areas of tubewell irrigation, secondary soil salinity induced by large amounts of groundwater use is a potential concern (Murray-Rust and Vander Velde 1992). Present levels of salinity, which average 0.8 millimhos per centimeter in Dir and 3.2 millimhos per centimeter in the Faisalabad study area do not appear problematic, but higher levels may reduce productivity. After controlling for fertilizer input and soil fertility, all three types of irrigation inputs had a significant positive effect on wheat yields. But the magnitude of the coefficients indicates that each irrigation application from own tubewells has the highest impact on yield, followed by purchased groundwater and canal applications. The number of applications is an imperfect indicator of irrigation, because it does not control for the volume of water used per application (though the area of crop irrigated is controlled for), nor for timing of applications. The volume of water per application is usually lower for tubewell than for canal applications, and therefore would not explain the higher productivity of groundwater irrigation. However, farmers have relatively little control over timing under warabandi rotations of canal systems. Tubewell water can be adjusted to the crop needs and growing cycle, and therefore have a greater impact on production. The estimates of productivity of tubewell irrigation, particularly from own tubewells, are influenced by a number of tubewells in Jaranwala, a village within the formal command area of the canal system, but which actually receives little or no canal 45 water (except through groundwater recharge). While it may be argued that this is not representative, it is precisely in such areas that tubewell irrigation is likely to be most important in agricultural production. This production function, which focuses on seeds, fertilizer, labor, soil fertility, and irrigation, does not include all influences on productivity, such as weather, seed variety and quality, human and physical capital, and even water quality. There are also selection processes underlying farmers' decisions to invest in tubewells and to purchase tubewell water, in addition to factors influencing whether farmers have access to canal water, which could be included in the model. Furthermore, these relationships may differ under other agroecological conditions, such as areas with significant salinity problems. However, these results show that irrigation, and especially tubewell irrigation, has a strong impact on yields among sample farmers in Faisalabad and Dir Districts. At the same time, they point to a productivity gap between the effect of own tubewell water, over which farmers have considerable control, and purchased tubewell water, over which farmers have less control. The following section examines factors which affect the reliability of purchased tubewell water, in order to identify ways to improve the performance of water markets. 6. RELIABILITY OF IRRIGATION SERVICE The productivity of irrigated agriculture is not determined solely by the amount of irrigation water supplied. The timeliness and reliability of water supplies is also critical. Timing waterings to meet crop evapotranspirative demand has a direct impact on yield, while the confidence farmers have in their water supply can affect their crop choice, level 46 of fertilizer and labor use, and the application of other inputs. Few studies of water markets have addressed the timeliness and reliability of purchased irrigation services, especially because they are difficult to quantify and measure. However, availability of water throughout the season, especially at critical times, provides one indicator of irrigation service. Because tubewell water is not tied to a fixed warabandi rotation schedule, it is easier to match tubewell irrigations to crop needs, in order to provide more frequent irrigations during periods of peak demand, if necessary. Tubewell water is also available throughout the year, except during periods of mechanical breakdown. In the IFPRI sample, tubewell owners reported that pump or engine failures made groundwater unavailable for an average of 2 weeks per season in Faisalabad, and 1 week per season in Dir. This compares favorably with the reported unavailability of canal water for an average of 4 weeks per season in Faisalabad and 5 weeks per season in Dir. Although the reliability of irrigation service under private tubewells is generally higher than under public sources such as canals and government tubewells, it is likely to be lower for water purchasers than for farmers with their own wells because tubewell owners sell surplus water after meeting the needs of their own crops. Thus, the deficits created by shortages of groundwater or energy supplies are not shared equally between owner and purchaser, but rather reduce groundwater availability to purchasers first. Such groundwater shortages compound groundwater unavailability due to mechanical failure of pumps, the latter affecting both owners and purchasers. Tubewell water sellers and purchasers in the IFPRI sample were asked whether water was always available when requested, as an indicator of reliability. Farmers 47 responded that water is most likely to be unavailable during periods of electricity shortage or load shedding, and during periods of peak water demand. Not surprisingly, the water purchasers were more likely to identify problems with water availability than were the water sellers (Table 15). Over a fourth of Faisalabad water buyers reported that they were unable to purchase water to meet crop needs during times of load shedding, although no sellers reported being unable to sell because of load shedding. Times of peak demand are more problematic: nearly a fourth of all sellers and over half of all buyers reported that purchased tubewell water was not always available when needed during such periods. 48 T ab le 1 5- -R ep or te d av ai la bi lit y of p ur ch as ed tu be w el l w at er Pu rc ha se d Tu be w el l F ai sa la ba d D ir T ot al W at er U na va ila bl e Se lle rs B uy er s Se lle rs B uy er s Se lle rs B uy er s D ur in g: R ep or tin g R ep or tin g R ep or tin g R ep or tin g R ep or tin g R ep or tin g El ec tri ci ty lo ad 0 22 0 0 0 22 sh ed di ng (0 .0 ) (2 6. 5) (0 .0 ) (0 .0 ) (0 .0 ) (2 2. 4) Pe ak d em an d se as on s 1 54 2 1 3 55 (1 4. 3) (6 5. 1) (3 3. 3) (6 .6 ) (2 3. 1) (5 6. 1) To ta l s am pl e si ze 7 83 6 15 13 98 So ur ce : IF PR I s ur ve y da ta , 1 99 2. N ot e: F ig ur es in p ar en th es es a re p er ce nt ag es . 49 What influences the reliability of purchased irrigation water? Three factors can be hypothesized to have an effect: type of tubewell, characteristics of the buyer, and the relationship between seller and buyer. Electric tubewells are more susceptible to power outages, and are therefore likely to be less reliable. Larger-capacity tubewells and those which draw water from deeper levels are hypothesized to be more reliable. Buyers with higher social status, indicated by land ownership and age, are also hypothesized to have more reliable access to purchased tubewell water. If social ties influence reliability of water markets, farmers who buy water from close relatives or their landlords would be expected to receive more reliable irrigation service. A logistic regression model has been used to test these hypotheses, using buyers' reported availability of tubewell water whenever needed as an indicator of reliability. Dummy variables for Jaranwala village in Faisalabad and for Dir district are included to control for agroecological differences between these areas and the rest of the sample (most notably the differential availability of canal irrigation). Results of the logit model are given in Table 16. As predicted, electric tubewells are significantly less reliable than those with diesel or tractor-powered lifts.24 Larger- diameter tubewells were significantly more reliable than smaller ones, but deeper tubewells do not provide more reliable irrigation for purchasers--indeed, the coefficient is negative, though not significant. Deeper tubewells may be located in groundwater-scarce areas, and therefore provide less reliable supplies to purchasers. 24 In an alternate specification of the model, the difference was found between diesel and tractor tubewells was tested and found not significant. 50 Table 16--Results of logistic regression model for reliability of purchased tubewell water Independent Wald Variables Units Coefficient T Ratio Statistic Electric tubewell dummy -2.189 ** -2.934 8.617 Tubewell diameter inches 1.267 ** 2.368 5.587 Tubewell depth feet -.026 -1.245 1.553 Size of land ownership acres .072 ** 1.986 3.949 Age of household head years .045 * 1.844 3.398 Buy from close relative dummy .855 .866 .750 Buy from landlord dummy 10.613 .435 .189 Jaranwala village dummy .668 .726 .527 Dir district dummy 4.209 ** 2.397 5.745 Constant -5.929 * -1.838 3.378 Model Chi-Square = 58.2 ** with 9 degrees of freedom Number of observations = 96.0 Classification Table for Reliability of Purchased Tubewell Water Predicted Percent NOT RELIABLERELIABLECorrect Observed NOT RELIABLE 49 6 89.1 RELIABLE 9 32 78.5 Overall 84.4 Source: IFPRI survey data, 1992. ** Significant at 5 percent probability level * Significant at 10 percent probability level The amount of land owned has a significant and positive effect on reliability, suggesting that water sellers are less likely to deny requests for water from larger land- owners than from small landowners or landless tenant cultivators. This is due to the influence of the land owners, not the size of farm operated. An alternate specification of the model with operational holding, rather than land ownership, showed no significant 51 coefficient for size of holding.25 The age of purchasers' head of household, another indicator of status, has a positive effect on reliability. The model does not show kinship or landlord-tenant relationships between water buyer and seller to have a significant effect on reliability of access to groundwater. Jaranwala village does not differ significantly from other areas in reliability of purchased tubewell water, but buyers in Dir district reported significantly more reliable access to groundwater. This is somewhat surprising because irrigation is less available in Dir than in the canal-irrigated areas of Faisalabad, and therefore demand for groundwater would be expected to be higher. However, rainfall is higher in Dir, and therefore groundwater may be more readily available to those farmers needing supplemental irrigation. While buyers' reported problems with unavailability of purchased groundwater is an imperfect indicator of reliability, this model points to important sources of problems in groundwater markets. Purchasers are more likely to receive insufficient groundwater if they buy from small-capacity, electric-powered tubewells; if they are young and own little or no land; and if they live in Faisalabad District. Improving the reliability of electric power or switching to diesel pumps are the most readily identifiable interventions to improve reliability of groundwater markets (as well as reliability of water for well owners). Both of these options are, however, expensive. Identifying the factors which lead to lower reliability in Faisalabad than in Dir requires further study. 25 Both ownership and operational holding size could not be included because of multicollinearity problems. 52 Although land ownership and age have strong influences on reliability, they do not appear to point to policy interventions that can improve reliability. Improving the reliability of irrigation by increasing the land ownership and age of water-purchasing households is not feasible, or even desirable. However, it may be possible to raise the status of purchasers relative to water sellers by encouraging smaller farmers to purchase tubewells. This study does not have data on both the sellers' and buyers' characteristics for each relationship, but it is possible that farmers with less land will provide more reliable service, both because there is less of a status gap between them and the purchasers, and because tubewell owners with less land will not need as much water to meet irrigation needs on their own fields, and thus have surplus water available for sale. 7. RESEARCH AND POLICY MEASURES FOR WATER MARKET DEVELOPMENT Water markets are largely autonomous, indigenous institutions which function-- and are likely to continue functioning--without a great deal of official intervention. What type of attention, if any, should the government, researchers, and other agencies pay to water markets? This final section highlights policy instruments and remaining research questions pertaining to water market development. First, understanding the role water markets play in mediating access to and control over groundwater resources can assist tubewell development programs in serving a larger number of farmers. This study indicates that water markets improve the equity of groundwater use by increasing the access of small farmers, tenants, and younger households who are least likely to own tubewells. Thus, neither public tubewells nor 53 ownership of tubewells by all farmers are required to ensure widespread use of groundwater in areas where water markets operate. However, the study also demonstrates that water markets do not operate in all areas, raising the question of which factors influence the activity of water markets. Conditions that affect the amount of groundwater available for sale include the number of tubewells in an area, the proportion of tubewell owners willing to sell water, and the nature of the underlying groundwater resource. Because, with current technology, water cannot be transported over large distances, wells must be available within close proximity to buyers' fields for groundwater markets to operate. Chambers, Saxena and Shah (1989) suggest that a higher density of tubewells fosters the development of competitive water markets. Thus, programs which assist private tubewell development, especially in areas of adequate, good-quality groundwater, are also likely to assist water market development. Making information about water markets more widely available both to individuals and groups of farmers may also stimulate further investment in tubewells. For example, knowledge of the potential for groundwater sales in a given area, different credit options for investment and contractual arrangements for water sales could be an important decision-making tool for potential investors. This information could be gathered and disseminated by local groups, non-governmental organizations or projects such as the Private Tubewell Development Project. Due to the small sample of tubewell owners, this study was not able to determine factors affecting which tubewell owners will sell water. Possible factors influencing the decision to sell include the size and location of tubewell owners' land holdings and their 54 cropping patterns, as well as tubewell technology and energy costs. Further research on this topic, as well as on the nature of the specific transactions occurring between buyers and sellers, would be useful in stimulating water markets. As noted above, large farmers are most likely to own tubewells, while small farmers are more likely to depend on water purchases, and consequently face less reliable access to groundwater. Howev