首页> 外文会议>2007 IYRF;International Yellow River Forum on Sustainable Water Resources Management and Delta Ecosystem Maintenance >Site Specific Micro-Watershed Based Sustainable Hill Farming in Upper Catchments of Indian Himalya
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Site Specific Micro-Watershed Based Sustainable Hill Farming in Upper Catchments of Indian Himalya

机译:印度喜马拉雅山上游流域的基于特定地点的小流域可持续丘陵耕作

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The North West Himalaya is characterized by high altitude (1,000m to >3,500m above msl), steep slope (15% to >100% slope), high intensity rainfall (> 100mm/h), prevalence of shallow and gravelly soil (7.5~15cm depth and >40% gravel), severe degradation, loss of forest cover and inaccessibility (8.6km length of roads compared to 37km/100km2 in India). The region spreads over 33 million ha across Jammu and Kashmir, Himachal Pradesh and Uttarakhand states in India. Twenty two million people inhabit this region, who are supported by 2.14 million ha of cultivable land, with an average land holding of less than 0.1hm2. North-West Himalaya (NW Himalaya) mid-hills (600~1,800m above msl), cultivation is mostly practiced on terrace hill slopes. Majority of the farmer's family produce only 4~5 months of sustenance food from its cultivated terraces (Ved Prakash and Narendra Kumar 2006). Thus, increase in the productivity of the micro watersheds has become the major thrust area for food security in the hills. Shortages of land and low productivity are the cause for cultivation of steep and unstable hill slopes. Srivastava et al., (1983) reported that about 33% of cultivated land belong to class Ⅴ, Ⅵ and Ⅶ against the norm of not cultivating any land having capability beyond Ⅵ yet farmers tends to cultivate steep slopes to increase production which leads to more erosion and loss of productivity. Agriculture in the region faces major problem of the water resources and its management as 90% of the area is rainfed. The problem further gets aggravated due to slopy terrains and shallow soil depth, which allow major portion of the rain water to be lost as runoff (Singh et al, 2001).
机译:喜马拉雅西北部的特征是高海拔(海拔高度从1,000m到> 3,500m),陡坡(坡度从15%到> 100%),高强度降雨(> 100mm / h),浅层和砾石质土壤普遍存在(7.5)深度约15厘米,砾石含量大于40%),严重退化,森林覆盖率降低,交通不便(印度的公路长度为8.6公里,而印度为37公里/ 100平方公里)。该地区遍及印度的查mu,克什米尔,喜马al尔邦和北阿坎德邦,面积超过3300万公顷。该地区有2千2百万人居住,得到214万公顷耕地的支持,平均土地占有量不到0.1 hm2。西北喜马拉雅山(NW喜马拉雅山)中山(MSL之上600〜1,800m),耕种大多在阶地山坡上进行。农民家庭中的大多数只能从其耕种的梯田生产4〜5个月的维持性食物(Ved Prakash和Narendra Kumar 2006)。因此,增加小流域的生产力已成为丘陵地区粮食安全的主要重点领域。土地短缺和生产力低下是耕种陡峭而不稳定的山坡的原因。 Srivastava等人(1983年)报告说,约有33%的耕地属于Ⅴ类,Ⅵ类和class类,这与不耕种Ⅵ类以外的任何土地的规范有关,但农民倾向于耕种陡坡以增加产量,从而导致更多的耕作。侵蚀和生产力损失。该地区的农业面临着水资源的重大问题,因为该地区90%的土地都以雨水灌溉,因此其管理工作十分困难。由于地势崎and和土壤深度较浅,问题进一步加剧,这使得大部分雨水作为径流而流失(Singh等,2001)。

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