Indian Journal of Traditional Knowledge Vol.12 (3), July 2013, pp 454-464 Use of indigenous soil and water conservation practices among farmers in Sikkim Himalaya P K Mishra & S C Rai* Department of Geography, Delhi School of Economics, University of Delhi, Delhi-110007 E-mail: [email protected] Received 10.10.11, revised 13.04.12 This paper analyses indigenous soil and water conservation practices in a watershed of Sikkim Himalaya based on information collected through a questionnaire survey. Information used in the analysis were obtained through a survey of 150 farmers in 3 ecological zones (low, mid and high), group discussions, key informant interviews, and field observation conducted during 2009-10. Farmers have adopted several conservation practices passed on to them by their forefathers. Farmers in all ecological zones have practiced several structural and biological land management practices to conserve soil and water. Adoption of terrace cultivation, construction of retention walls, bunds, construction and maintenance of waterways, mixed cropping, crop rotation, mulching, agroforestry, and use of farm yard manure are found significantly higher in all ecological zones of the watershed. This indicates that the farmers have very high belief in indigenous techniques of conservation. Findings are discussed in the context of conservation programmes within the watershed. The findings of this study have important policy implications for sustainable land management in the region. Keywords: Land management, Structural measures, Biological measures, Watershed, Agroforestry, Sustainable development, Soil erosion IPC Int. Cl.8: A01, A01B, A01B 77/00, A01G 31/00, E02B 3/18, E02B 3/00, A01D, A23B, A01N 3/00, E02D 3/10, A01G 9/24, A01G 25/00, A01G 27/00 Land and water are the basic natural resources, which support life in all forms. Both resources are limited to meet the increasing demand for food, fuelwood and timber in the world. Mountain watersheds have attracted global concern due to the threat of serious environmental and socio-economic implications arising from natural resource degradation1. Erosion of agricultural landscape is a significant socioenvironmental issue within the Himalayan region due to on-site and off-site damages associated with soil loss from land-use/cover change2,3. Displaced soil contributes to water pollution and reduces future productivity of land resources that have a significant environmental and socio-economic consequence for society4. The impacts of land degradation consist of two types: on site and off site. A loss of productivity and shortfalls in both food and cash crops are the immediate impacts of land degradation. It is estimated that 175 million ha of land in India suffers from various problems of soil erosion and land —————— *Corresponding author degradation5. This is all the more important because the country looses about 5334 M tones (16.4 t/ha) of soil annually. Of this, about 29% is carried away by the rivers into the sea and 10% is deposited in the reservoirs, resulting in a loss of 1 to 2% of their storage capacity6. Short-sighted policy-makers and planners find investments in conservation and development of mountains less attractive compared to the adjacent plains, as their comparative advantages are overlooked. As a result, mountain watersheds are either undergoing or are vulnerable to degradation, despite local people’s efforts to prevent such effects7. Traditional or indigenous technologies are entirely based on local needs and surroundings, prepared from locally available resources and from the wisdom and knowledge handed down from generation to generation. These are locally managed and maintained. A few studies have shaded light on hills farmers’ land management practices7,8,9, but their areas of concern have been selected aspects of management including landslide prevention and repair measures. Therefore, the objective of this paper is to: (i) present the findings of a study designed to examine MISHRA & RAI: SOIL AND WATER CONSERVATION PRACTICES IN SIKKIM HIMALAYA how indigenous practices influence adoption of conservation systems at the farm level, (ii) find out how hill farmers have changed their land management practices to control land degradation under the situation of steadily increasing population pressure on very small landholdings, and (iii) document to serve as a basis for programme planners to give such low cost technologies their due importance. Study findings are discussed in the context of conservation programmes within the watershed. Methodology This study is based on information obtained through a questionnaire survey, field observation, and group discussions. The household survey was conducted during study period (2009-10). A sample size of 150 households was obtained from watershed covering each ecological zone, viz. low, mid, and high. Simple random sampling method was employed to select households for the questionnaire survey. At the outset, the interviewer introduced himself to the villagers. Villagers were told about the nature of work and assured that responses were to be used for research purposes, that their cooperation to this effort was sought, and confidentiality would be maintained. Detailed information on the management practices of each parcel of land owned by the sampled households were collected using structured questionnaire. Farmers were asked to complete a structured questionnaire that required about 30 - 40 minutes to complete. The response rate for each zone was about 80%. Average age of the respondents is 70 yrs. Given the large sample size, the broad distribution of the sample throughout the study watershed, the high response rate, and the sampling technique used to select the sample, the samples are assumed to be representative of the farm populations within the each ecological zone. Information on soil and water conservation practices including construction of terraces, waterways, retention walls, gully control measures, alley cropping, mulching and application of organic manures was collected through household survey. Besides, information on farmers’ experience in land management, soil fertility and soil erosion was collected through personal interview and group discussion. The degree of adoption and diversity of practices, however, vary from one farm household to another, depending on their socio-economic condition and biophysical characteristics of lands. To determine 455 the overall degree of adoption of soil and water conservation measures, 16 common soil and water conservation practices of farmers were selected. Hill farmers have practiced different types of structural and biological measures of soil and water conservation to control erosion and landslide and applied different types of fertilizers to maintain soil fertility as summarized in Table 1. Descriptive statistics were used to examine general trends within the data set, while one-way analysis of variance was used to test the research expectations with the Statistical Package for Social Sciences 9 (SPSS) software. One way ANOVA analysis was applied to analyses the significance difference of indigenous SWC practices among different ecological zones of the watershed. All the analysis was done at 0.05 or 5% level of significance. Study area The study area Papung-Ben Khola watershed located in the South district of Sikkim state was selected for this study. This watershed extends between 27° 13΄ 34˝ to 27° 16΄ 12˝ N and 88° 22΄ 18˝ to 88°27΄ 15˝ E. It is spread in 27.77 km2 area and characterized by an elevational range of 326 to 2600 m asl. It comprises of most of the human habitation zone, vegetation types and cropping patterns that are common in the state. The watershed is one of the most populated (10841 persons) areas in state providing a wide range of cultural-ethnic diversity and land-use pattern. Agricultural practices extend from valley bottom to hilltop, with a variety of cropping systems and management practices. Fragmented into several parcels, farmlands are being managed in different ways, to maximize benefits with the limited amount of resources available to farmers. The climate is monsoon type with average rainfall was 3204 mm, and most of the rainfall takes place during monsoon from June to September. Average temperature ranges from 3-26°C. Results and discussion Structural measures of soil and water conservation Terraces Terraces are narrow strips of land carved out across the hill slopes for cultivation of cereals, including rice, maize, wheat and millet. Regardless of land type, most terraces in the watershed were constructed long back. Some of them were, however, constructed a few decades ago in response to increasing food demand INDIAN J TRADITIONAL KNOWLEDGE, VOL. 12, NO. 3, JULY 2013 456 Table 1-Brief description of terminologies used in the context of hill farming system and soil and water conservation Terminologies and measures Terminologies used in the context of hill farming system Description Hill slope Terrace riser Farm edge Goth Slicing terrace riser Panikhet Tarikhet Khet Packo/Bari Gharbari Measures of soil and water conservation Terrace Terrace bund Contour bund Waterway Retention wall Alley cropping Shrub formations in gullies Vegetative measures of landslide control Mulching Farmyard manure Green manure Compost Sloping land between valley floor and ridge Steep slope between terrace of different altitude Farm boarder Makeshift livestock shed constructed in the farm terrace Thinly slicing of the slope between terrace by spade to remove weeds and grasses Irrigated rice field located in the valley floors and foothills Rainfed rice field located in the hill slope Common local term for both panikhet and tarikhet Rainfed maize and millet field Homestead used for fruit, maize, wheat, millet and vegetable production Narrow strip of land carved out across the hill slopes for the cultivation of cereals An embankment at the outer edge of khet terrace made to control water flow An embankment built along the contour line to control soil erosion and siltation Small canal at the inner toe of terraces made to convey runoff at a non-erosive point A reinforced wall constructed to protect terrace riser from being collapsed Alternate rows of field crops and perennials grown in a contour pattern in sloping land Bush formations, including bamboo, in gullies established to control gully expansion in the hill slopes Establishment of different shrubs and tree species with extensive root systems for rehabilitation and control of landslides The practicing of covering the plowed land by crop residues and leaf litters for moisture and soil conservation Dung mixed with leaf litter and crop residues used for fertilizing land Plant species containing soil nutrients Decomposed mixture of organic materials, including manure, utilized for fertilizing land for steadily growing household size. All respondents in each ecological zone of the watershed responded that they are practicing terraced farming since long back (Table 2). There is no significant difference between ecological zones in terms of percentage of farmers who have terrace construction (Table 3). Leveled bench terraces (Fig.1a) are the dominant structural measures adopted by hill farmers to stabilize irrigation water required for rice cultivation in Panikhet and Tarikhet. These terraces have been maintained without any change in each ecological zone. Bari terraces in the area have outward-facing slopes that facilitate quick drainage of water required for millet, maize and legume crops. Terrace risers use to be relatively wide in the past when the population pressure on land resources was relatively low10. Farmers have sliced terrace risers to increase the area under crop production. Even the tiny fraction of land under risers has been intensively utilized for legume crops, which was not the practice until few decades ago7. Similar results were also recorded in the Papung-Ben Khola watershed. During field survey it was observed that about 23% of the cultivated land is under leveled terrace and used for paddy and other crops during monsoon season. Most of the leveled terraces have a height of 2 - 5 m; width 2 - 5 m, and the length varies from 15 - 35 m. The width of the terrace is determined by the slope (gradient) of the land. In the hill slope, an average of 20 - 25 terraces exist, but in the lower altitude a sequence includes not more than 10 terraces because of the larger width of the paddy fields. Remaining 77% are sloping terraces. All respondent of the area have agreed that terracing is necessary, without which the plant nutrients cannot be conserved and cultivation of crops are impossible. MISHRA & RAI: SOIL AND WATER CONSERVATION PRACTICES IN SIKKIM HIMALAYA Bunds Terrace bunds are small embankment constructed at the outer edge of the terraces to control water flow. Terrace bunds used to be relatively wide in the past when the population pressure on land resources was relatively low. Farmers have sliced terrace bunds to increase the area under crop production. Even the tiny fraction of land under bund has been intensively utilized for legume crops, which was not the practice until a few decades ago7. Farmers have also constructed contour bunds across the farm edges. Mostly made from stone, these bunds control soil erosion and siltation. Besides, contour bunds prevent stray livestock from sneaking into farmlands. Contour bunding is the most popular 457 soil conservation measures in Sikkim Himalaya. Contour consists of constructing narrow based trapezoidal bunds on contour into the runoff water behind them so that all the stored water is absorbed gradually into the soil profile for the crop use. Farmers are well aware of erosion problem in the area. Moreover, they agreed that this measure is effective to protect the soil loss. About 90% of the respondents have constructed bunds on their fields with the other measures including vegetative barriers in the leveled terrace (Table 2). The farmers of the watershed are pioneer in bunding and have taken up bunding work on large scale in the leveled terrace (paddy) to check the runoff. These bunds on steep slopes are created by way of excavating parabolic Table 2-Indigenous soil and water conservation practices in Papung-Ben khola watershed of Sikkim Himalaya Ecological Zones Practices Low (n=50) (%) Mid (n=50) (%) High (n=50) (%) Mean 100 96 100 50 100 78.6 (1) Mechanical measures Terraces Bunds/contour bunding Construction and maintenance of waterways Gully control Diversion channels Stone barriers 100 90 88 69 41 89 (2) Biological measures 75 55 20 90 82.6 63 37 90 Alley cropping Mulching Minimum tillage Crop rotation Mixed cropping Vegetative barriers Agroforestry 27 30 91 90 80 75 100 100 41 49 100 100 65 70 (3) Soil fertility management 33 88 70 100 45 100 75 30 89.66 75 100 45 100 70 Farm yard manure Green manure Crop residue and weed burning 87 32 100 55 23 100 73 28 100 85 65 50 91 78 29 100 Table 3-Analysis of variance findings for indigenous soil and water conservation practices in each ecological zone of Papung-Ben Khola watershed of Sikkim Himalaya Ecological Zones Mean Std. Dev. F-Test (Calculated) F-Test (Tabulated) Significance Level Result (p<0.05) Low 73.60 25.33 No significant 6.86 19.41 0.05 or 5% Mid 70.57 25.24 variation High 65.26 27.63 One way ANOVA at p<0.05 has revealed that there is no significant difference among indigenous SWC practices in all three ecological zones (Fdf (12, 2) = 19.41, Fc =6.86). 458 INDIAN J TRADITIONAL KNOWLEDGE, VOL. 12, NO. 3, JULY 2013 channels (0.30 m top and 0.15 m deep) on contours and keeping the dugout soil in form of a bund at the lower edge of the channel. The widths of the bunds are usually 0.15 m and these bunds are extensively used to store water in the leveled terrace (paddy fields), for effective measures in arresting soil erosion. These bunds are also used for planting various types of pulses as double cropping system. Construction and maintenance of waterways Waterways have been an integral part of the terraced farming system in the mountains of Nepal and other Himalayan region11. The main purpose of waterways in land management system is to convey run-off at a non-erosive point12 (Fig. 1b). Uncontrolled surface run-off moving down slopes across hill slopes destroys terrace risers and removes soils from the farmlands, eventually decreasing crop yields and increasing the cost of terrace maintenance7. To cope with the problem, farmers of the watershed have constructed waterways (Table 2) and there is no significant variations between ecological zones in terms of percentage of farmers who have constructed them (Table 3). According to their location, waterways in the area can be categorized into different types. Inter-terrace waterways are constructed across the inner toe of bari terraces. A narrow waterway is constructed across terraces for the diversion of surface runoff, which is channeled through waterways and drained into either gullies or grasses. This type of practice is found in the middle zone of the watershed. Inter-terrace waterways are constructed to prevent land from getting oversaturated, because this adversely affects the yield of some crops. Such waterways are also utilized to uniformly distribute water in farm plots during the dry seasons. Farm edge waterways are constructed about 10 to 15 m above the farm border. Waterways, especially in high-erosion-prone areas have been paved with stones to prevent gully formation. Gully control Gullies are relatively permanent steep-sided watercourses with momentary flows during rainstorms12. According to respondents, gully formation was high when forests on hill slopes were cleared for expansion of farm. Once gullies were formed, they started expanding both vertically and laterally, eventually engulfing adjacent farmlands. Farmers started making contributions to the gully control through planting bamboos trees, and making stone walls to stabilize the land through joint efforts. About 67% of the respondents had participated in gully control measures (Table 2). Farmers planted bamboo species to control gully erosion. Establishing bamboo species, including Bambussa balloca, Dendrocalamus hamiltonii, Bambussa spp. and Arundinaria raccum in deep gullies and along stream banks is an age old practice adopted to minimize soil erosion, river bank erosion and gully expansion. These species propagate rapidly and have fibrous root system with excellent soil-binding capacity. Leaves of these species are used as fodder, stem as thatching and handicraft materials, and branches as fencing materials7. Bamboos species planted in gullies at the valley bottom occasionally block surface runoff and flood farmlands. To protect soil from this, farmers have filled gaps between bamboo clumps with stone walls. Diversion channels (Irrigation system) Fig. 1—(a) Terraces: an age old soil and water conservation measures; (b) Construction and maintenance of waterways The construction of diversion channels is a traditional practice in the watershed and practiced by all farmers. The objective is to drain the water to leveled terrace (paddy field) from nearby situated MISHRA & RAI: SOIL AND WATER CONSERVATION PRACTICES IN SIKKIM HIMALAYA natural drainage ways, during high intensity rainfall events. The diversion channels are constructed on places from where water can easily enter the field. These diversion ditches are made collectively by all farmers who have irrigated land. About 37% of the farmers were responded that they spent their labour and capital in preparation and maintenance of diversion channels. Traditional diversion channels have a channel slope of 5 - 40%. Most diversion channels are maintained by the farmers before the onset of monsoon, some farmers try to improve the channels’ stability with sods, especially in sections with steeper slopes. The size of a diversion channels depends on the soil type and the expected maximum amount of runoff water. In practice most channels are width (0.45 m) and not very deep (0.45 m), the width and depth of these channels varies following topography. About 23% farmers practice grassed waterway diversion channels replacing normal channels to conserve soil along the channels where soil particles are loose and erosion rate is high. It was observed that these terraced paddy fields get water from these diversion channels connection rivers, rivulets, jhoras, dharas and simsar, which are charged by rainwater. 459 cost. They also played an important complementary role in supporting farm household economies by providing fuelwood, fodder, and food13,14. Alley cropping Until a few decades ago, trees and shrubs used to be grown mostly in private pasture land together with fodder trees. With the dwindling forest fodder supply caused by deforestation and restrictions on free access to forests, farmers started planting fodder trees and shrub on the edges of terrace risers, including palatable fodder species like Artocarpus lakoocha, Ficus hookerii, Ficus hirta, Ficus nemorales, and Ficus sp. Large tree species were gradually replaced by nitrogen fixing and high fodder-yielding shrub species, including Bahuhinia variegata, Leucaneia leucocephala and Morus indica, as crop yield under the shade of tall trees gradually declined. Farmers found farm edges, foot trails, gullies, and terrace risers at higher elevations suitable for tall species. In the absence of an effective extension service, alley cropping was being practiced by 30% of the households of the watershed (Table 2). Mulching Construction of stone barriers in watershed is an age old practice. Large stones from the field are removed and deposited downstream. Most of these traditional stone barriers are 0.60 - 1.5 m high, and terraces have been formed upstream. However, most farmers clean their fields from stones or by making boundary bunds as a soil conservation measure. As it is an age old practice, still farmers replicate similar but smaller stone on their own field with the main objective to clean the field by removing the bigger stones. Survey result showed that about 90% of the respondents practice stone barriers in their field and it is the widely adopted soil and water conservation (SWC) practice in the area, mainly because of their visual impact as a sediment trap, and the accumulation of water in the soil around these practices. Stone barriers are most successful on fields with slopes until 15%. Spreading of organic residues instead of mixing (stubble mulching) them can help in the reduction of soil and water loss to a considerable extent15. Farmers considered mulching an effective means of moisture conservation in farmlands, which are vulnerable to a lot of moisture loss during the winter and early spring seasons. To prevent this, farmers with a relatively large household size and small land holding cover the plowed land with crop residues, leaves and twigs. Mulching is also practiced to prevent seedbeds from getting exposed to the sun and rain and to protect seedlings from hailstones. About 90% of the farmers in the watershed were practicing mulching (Table 2). The leaves of Siris (Albizza odoratissima) trees are used for this purpose. These leaves after decomposition help to enhance the fertility of soil. Generally, 4 tons/ha of mulching considerably reduces the soil loss and runoff from the field. Notably, no significant variation was found among the three ecological zones in terms of percentage of farmers practicing mulching (Table 3). Biological measures Minimum tillage Farmers in the watershed are also practicing several types of biological measures of land management (Table 2). These practices evolved from the past have contributed to control land degradation at relatively low In minimum tillage, farmers plough their land only once during land preparation, which is followed by seed showing. Rest of the agricultural activities is similar to that of conventional practice. Minimum Stone barriers 460 INDIAN J TRADITIONAL KNOWLEDGE, VOL. 12, NO. 3, JULY 2013 tillage cannot be adopted in isolation. It is a basic management tool16. Conservation tillage is defined as any tillage system that leaves at least 30% of the soil surface covered with crop residues after planting17. The information about maize production in minimum tillage is based on the farmers’ field experiment18. This maintains continuous ground cover during the year reducing erosion. It is observed by the farmers that amount of soil loss is less in minimum tillage plots in comparison with the ploughed plots. Some farmers still consider leaving crop residue on the field shows poor husbandry skills but minimum tillage techniques are becoming more widely known and accepted. Crop rotation Crop rotations are important land management practices in the area. Crop rotation involves incorporation of legumes with cereals in a sequence to take advantage of different feeding zones, both for nutrients and water, and to offset disadvantage of mono-cropping in controlling insect, pest and diseases, etc. Crop rotations are practiced by all the farmers of the watershed (Table 2). Crop rotation on a recently harvested potato field makes residual nutrients available for the other crops. Moreover, crop rotations help combating plagues and avoid soil mining. In the study area, most common crop rotation is potato-maize-paddy. Farmers in the watershed have developed systematic management and conservation alternatives of mixtures of crops with multipurpose agroforestry tree species that create appropriate environment to some high value crops and intercropping of many other local varieties. Mixed cropping Mixed cropping is a traditional and very old practice in the watershed. Advantage of this type of cropping are good crop cover, feeding of crops from different soil layers and under rainfed conditions an assurance to farmer against total failure. The use of agroforestry is frequently observed in traditional mixed cropping systems in the watershed. About 45% of farmers use mixed cropping to diversify production and assure yielding of at least one of the crops (Table 2). The main crop (maize) is grown as usual, and the vegetables (principally beans or cabbage) is scattered in smaller quantities over the whole field. In some cases intercropping is applied, with several small rows of the secondary crop (ginger) in between the furrows of the main crop. The main purpose of mixing different crops is the protection of the main crop (maize and beans) against pests and diseases (Fig. 2a). The intensity of cropping varies from farm to farm and from household to household due to differences in socio-economic conditions, particularly inputs and products, dependence on land and tenurial system, etc. Vegetative barriers Vegetative barriers are well known practice in the watershed and adopted by all the farmers (Table 2). However, vegetative-barriers as a runoff control measure to stabilize steep cultivated hillsides, have been intensively studied. It was found that planting on contour is the best soil and water conservation measure. Contour cultivation and contour plantings are the basic agronomical practices, which are adopted by the farmers of the watershed on the slopy land. These are non-monetary practices and have been proved to be ideal for soil and water conservation. Vegetative barriers are very important for protection of the soil and it helps enhancing the soil in two ways. Firstly, the plants act as barrier to the run-off, which helps in retaining the nutritive value of the soil. Secondly, the roots of the plant remains add organic matter to the soil, thus improving the soil structure. It was also found during the field observation that associated vegetative-barriers on the contour, consisting of grasses and trees on dry field (bari) and pulses on wet field (khet) are most successful and best adopted by all farmers. Among species most commonly planted on bunds and field boundaries are fodder trees such as Artocarpus lakoocha (badahar), Ficus roxburghii (nevaro), Ficus nemoralis, (khaneu), F. clavata (Khaneu lutey), Fnemoralis Wall (Dudhilo), Ficus roxburghii (Nebara), Schima wallichii (Chilaunay), Engelhardtia spicata (Mahua) and Melia azaderach (Bakaino). Apart from this, other are fruit trees such as papaya and orange, crops such as beans, pulses, and natural grasses such as Thysanolaena maxima (Amlisho), Pennisetum agrostis (Napier). In the watershed area Amlisho (broom grass) (Fig. 2b) was found very suitable and economically beneficial when planted at the horizontal distance of 4.5 - 6.0 m, so that the entire landscape is stabilized and moisture is retained, thereby improving moisture regime. It is used widely in the watershed because of its multipurpose use. Broom grass leaf is used as fodder to feed the livestock, hard stem for fuel, supporting MISHRA & RAI: SOIL AND WATER CONSERVATION PRACTICES IN SIKKIM HIMALAYA the vegetables in mixed cropping, and most important its flower part, is used for making brooms which fetches good price in the market. A good plant of Amlisho produces approximately 5 kg of flower per year and the market prices is Rs.30/- kg. This way a plant is generating Rs 150/- to the farmers. It was found in the group discussion with the farmers that to cover one hectare of bunds and other suitable places where Amlisho can play a vital role in soil and water conservation. Clone and cutting method is used for planting the bushes. Agroforestry The multi-functionality of the agroforestry systems has been realized in the watershed over the last many decades. Large cardamom based agroforestry system is observed to accelerate the nutrient cycling, increases the soil fertility and productivity, reduces soil erosion, conserves biodiversity, and also conserves water and soil. Large-Cardamom based Agroforestry system Fig. 2—(a) Mixed cropping: maize with ginger; (b) Broom grass: as a vegetative barrier in agriculture field 461 Traditional cultivation of the large cardamom (Amomum subulatum) in Sikkim is one example of harnessing the local mountain niche (Fig. 3). Large cardamom, a native plant of Sikkim, is a perennial low-volume, high value, non-perishable cash crop grown beneath the forest cover on marginal and barren lands and can be grown between 600-2000 m asl. It helps watershed in two ways: (i) by converting abundant marginal and barren lands in more productive lands and harnessing local niche, and (ii) by maintaining and improving the ecosystem and the environment of the region through promoting soil conservation and soil fertility19. The standing biomass in the cardamom system is about 2.5 times higher than in the maize-potato system, thereby providing more biomass resources for farm family utilization. The agronomic yield is very low in the cardamom system, as much as 21 times less than in the maizepotato system, indicating that cardamom are a lowvolume, high value cash crop. Soil fertility levels influence plant productivity considerably. Therefore, soil health is critical, especially in the mountains where erosion problems are quite conspicuous. The soil nutrient levels, especially organic carbon and total nitrogen, in the cardamom agroforestry system are comparatively higher than in the maize-potato dominated system19. The large cardamom is cultivated either under mixed tree species or under Alnus nepalensis cover. The agronomic yield of the large cardamom is about 2.2 times higher beneath the Alnus tree than beneath mixed tree species. According to the data, 65.34 kg/N/ha/yr was fixed in the cardamom agroforestry system19. Nitrogen and phosphorus Fig 3—Large-cardamom: an age old cash crop based agroforestry system 462 INDIAN J TRADITIONAL KNOWLEDGE, VOL. 12, NO. 3, JULY 2013 concentrations of different tissues of N2-fixing Alnus are higher than those of mixed tree species20. and gradually landholdings7. Mandarin Orange based Agroforestry system Green manures Mandarin orange is a major tree crop while intercropping of maize, pulses, ginger, buckwheat, fingermillet, pulses, oilseeds, taro and yam are also practiced. Mandarin orange and ginger are potential cash crops after large cardamom. Albizzia is widely grown with other agroforestry trees in mandarinbased farming. Mandarin orange is a high value, comparatively less labour intensive cash crop. Diversity of crops and other associate tree species are maintained in the system for other subsistence requirements and benefits. The on-farm agroforestry species such as Erythrina indica, Ficus spp. Alnus nepalensis, Albizia spp., Artocarpus lacoocha, Thysanolema maxima, Dendrocalamus spp. etc. are agro-ecologically adapted and socially accepted keystone species for their role in conserving and enhancing biodiversity in the mountain watersheds. Alnus and Albizzia have been a boon to the region for their role in nitrogen fixation, ecological adaptability, natural regeneration and restoration of degraded landslide areas, and accelerated nutrient cycling in the cultivated systems. Crop residue and Weed burning Soil fertility management Besides adoption of structural and biological measures, farmers of the watershed apply different types of organic, green manures and crop residue and weed burning practices to improve land productivity. Farm Yard Manure Farm Yard Manure (FYM), comprising mainly manure and livestock bedding, is the major source of fertilizer in the area. Livestock beds, consisting of waste fodder, tree leaves, and crop weeds, and manure are cleared twice a day to keep the goth clean. These materials are normally dumped in front of goth in a 3-4 foot-deep pit and remain exposed to the sun, rain and wind for several weeks until their transfer to the field. The amount of FYM applied to all types of land is significantly high in the low and mid ecological zone. Overall, farmlands in the watershed receive FYM at the rate of 12400 kg/ha/yr. In all ecological zones; priority is given to gharbari followed by bari for application of FYM. Though it is a major source of fertilizer, the supply of FYM is steadily declining in the watershed as farmers have reduced their livestock herd size to cope with shortage of labour shrinking grazing-lands and Applying green manure species, namely Adhatoda vasica, Euphorbia roylena, Artemissia vulgaris spp, etc. to vegetable and paddy seedbeds has been a traditional practice of small percentage of farm households in the area (Table 2). Mostly found in the wild, these plant species contain more than double amounts of NPK compared to FYM21, 22. Some of these species are also considered useful for controlling weeds and pests. Despites their awareness of the usefulness of green manure, farmers has not been able to apply it intensively because of the scarcity caused by lack of conservation and promotional efforts. In response to the dwindling availability of green manure, farmers are using leaves of Sachima wallichi and Castanopsis spp. Especially for paddy cultivation. These species, according to farmers, have low nutrient content and helps prevent soil from becoming acidic. In some instances weeds grown in the fields are also being utilized as green manure, specifically for millet. Burning crop residue and weeds is a traditional method of fertilizing particularly in bari land. During the dry summer season, farmers collect maize and millet stubble, leftover paddy straw, dried weeds, and woody plants grown in bari terrace. The collected biomass is burned when sign of rainfall appears, so as to allow the ash to get mixed well with the soil after the rain as well as to control the fire from spreading into other farm plots. Farmers spread the ash all over the farm plot to enhance soil fertility and to control some pests. Similar practices are being reported in other parts of the Hindu-Kush Himalayan region7. Evaluation of indigenous practices Indigenous soil and water conservation practices are widely used by the farmers of the watershed. However, the validation study during the field visit and research findings revealed that most of them are technically effective and at the same time easily replicated by farmers. Table 4 illustrates an overview of all SWC practices that were used by the farmers. The present practices were judged by the following criterion: (i) effectiveness, (ii) replicability, and (iii) ranking. Table 4 also reveals that most of the SWC practices receive an overall positive conclusion. MISHRA & RAI: SOIL AND WATER CONSERVATION PRACTICES IN SIKKIM HIMALAYA 463 Table 4—Evaluation of available SWC practices in the watershed Judgement Criteria* Practices Effectiveness Replicability Main Strengths Conclusion Terraces Bunds/contour bunding Construction and maintenance of waterways Gully control + + + + +/0 + + + + + Diversion channels Stone barriers Alley cropping Mulching Minimum tillage 0 0 0 + 0 +/0 0 Crop rotation Mixed cropping + + + + Vegetative barriers + + Agroforestry Spring-shed development (Natural springs) + + + + Farm yard manure(FYM) Green manure * With: + = Positive; 0 = Neutral; - =Negative + + + + Prevent soil erosion Prevent soil erosion and nutrient loss Irrigation, diversion of surface runoff Availability of plant species and stones Adequate channel slope High availability of stones Utilization of each parcel of land High availability of mulching material Protects soil erosion and moisture retention Soil fertility Good crop cover and diversified production Runoff control and provides fodder and fuel-wood N2 fixing and runoff control Ground water recharge, major source of drinking water Availability of dung and organic material High availability of plant species 0 0 However, even these practices have to overcome certain limitations before successful results and widespread adoption can be achieved. All the “neutral” judged practices have limitations that are more serious. Certain farmers only will adopt these practices, and more participatory research and (technical) assistance is required for their widespread adoption. In any case, as argued none of the above practices alone can improve agricultural production and SWC. Only adopting mechanical measures are not very effective without the biological measures and soil fertility management. FYM use, in combination with vegetative barriers, agroforestry, terracing, diversion channels and adequate mixed cropping systems, are the first suggested step towards establishing more productive and sustainable agricultural lands in the watershed. Meanwhile, the other discussed practices should be further investigated and validated. Besides the above mentioned practices, future research must also focus on new SWC alternatives. Given that, blending traditional and modern technologies is important23. Being a hilly area, ecological conditions in the study area vary even with a short distance. There are several types of soils that vary in physical and chemical properties, depending on parent materials, altitude and + 0 0 0 + 0 + + + + + + + slope gradient. Farmers are not aware of chemical properties of soils but they are well aware of the productive value and problems associated with all types of soils, and have adopted appropriate conservation measures to control the degradation of problem soil. Farmers have established vegetative barriers, and constructed waterways, retention walls to control soil erosion. Experiences from agro-ecology and traditional agricultural management and knowledge systems can definitely enrich the current available stock of SWC practices. However, operationalizing local knowledge is still in its infancy24. Conclusion Erosion of soil is a significant socio-environmental issue within the Sikkim Himalayan region. While soil erosion can create serious on-site problems, a large proportion of the negative environmental consequences of soil erosion are associated with offsite damages. Land being the major source of the food supply, majority of the farmers in the study watershed has pursued efforts to enhance land productivity, conserve soil and water, and increase soil fertility to cope with shrinking landholdings caused by the population growth and family fragmentation. In this regard, they have improved terraces, intensified 464 INDIAN J TRADITIONAL KNOWLEDGE, VOL. 12, NO. 3, JULY 2013 agroforestry practices and participated in gully control, and waterway construction activities. They also practices alley cropping and mulching to improve land productivity. The study watershed is very strong in traditional soil and water conservation practices. Most of the indigenous practices are readily available and can be promoted without major restrictions, viz. terrace, contour bunding, agroforestry, vegetative barriers, diversion channels, stone barriers, mixed cropping, crop rotation and FYM/green manure. All these practices are based on indigenous knowledge. The findings of this study justify that farmers devise alternative technologies for increasing land productivity, as they are exposed to the risk of food scarcity due to shrinking per capita land holdings. The significance findings of this study have important policy implications for sustainable land management in the area. Any future land management initiative should aim at enabling watershed settlers to adopt practices conducive to increase income as well as to enhance land conservation. Acknowledgement Authors are thankful to the Head, Department of Geography, Delhi School of Economics, University of Delhi for providing facilities. Authors are also thankful to the farmers of Temi-Tarku, Damthang, Deo, and Raigaon villages of Papung-Ben Khola watershed for their support and information during field survey. 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