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首页> 外文期刊>Journal of Water Resource and Protection >Groundwater Depletion with Expansion of Irrigation in Barind Tract: A Case Study of Tanore Upazila
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Groundwater Depletion with Expansion of Irrigation in Barind Tract: A Case Study of Tanore Upazila

机译:Barind地带的地下水耗竭与灌溉扩展:以Tanore Upazila为例

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In this paper successive depletion of groundwater level with expansion of groundwater irrigation in Barind Tract has been discussed from mid 1960s to 2010 in the context of Tanore Upazila, which is located in severely drought prone area of northwest Bangladesh. After starting of groundwater irrigation in Bangladesh, it spread rapidly all over the country, and about 80% of agricultural land is now supplied irrigation from groundwater. Availability of irrigation in Barind Tract has revolutionized its agriculture, but groundwater level is successively falling all over the country due to excessive withdrawal, and this process is accelerating due to water withdrawal from major rivers by upstream countries. In northwestern part of Bangladesh groundwater depletion problem is severe because this part is free from seasonal flooding. Only source of recharging of groundwater aquifer in this area is rainfall, but rainfall is also lowest here among the country. In this context, this paper presents the change of groundwater level with the spreading of groundwater irrigation in Barind Tract. Hydrograph analysis, groundwater level mapping, groundwater depletion rate calculation are done from groundwater level observation well data of Bangladesh Water Development Board (BWDB) and Barind Multipurpose Development Authority (BMDA). Climatic condition is analyzed by calculation of rainfall deviation from the data of Bangladesh Meteorological Department (BMD). Focus Group Discussion (FGD) and interviews with farmers and experts of different branches are conducted to understand the nature of problems in the study area. Agricultural pattern, cropping intensity (262% in study area and national intensity is 180%), methods of cultivation, crop variety and yields all show a positive change after starting of groundwater irrigation in mid 1980s, but water level is continuously lowering at the rate of 1.37 ft/y in wet season and 0.72 ft/y in dry season. Water is the main input for agriculture but successive depletion of groundwater level can be a serious problem for water stressed Barind Tract. Crop diversification, artificial recharging, increasing dependency on surface water, increasing irrigation efficiency, rainwater harvesting etc., can be option for the area.
机译:本文在1960年代中期至2010年中,在孟加拉国西北部干旱多发的干旱地区塔诺尔·乌帕齐拉(Tanore Upazila)的背景下,讨论了Barind Tract地区地下水位的连续消耗和地下水灌溉的扩大。在孟加拉国开始进行地下水灌溉之后,它迅速遍及全国,现在大约80%的农业用地都由地下水灌溉。 Barind Tract的灌溉方式使农业发生了革命性变化,但由于过度抽水,全国地下水位连续下降,由于上游国家从主要河流抽水,这一过程正在加速进行。在孟加拉国西北部,地下水枯竭问题十分严重,因为该地区没有季节性洪水。该地区唯一补给地下水蓄水层的来源是降雨,但该国的降雨量也是最低的。在此背景下,本文提出了巴林德地区地下水位随地下水灌溉范围的变化。水文图分析,地下水位图,地下水枯竭率计算是根据孟加拉国水利发展局(BWDB)和巴林德多用途开发署(BMDA)的地下水位观测井数据进行的。通过根据孟加拉国气象局(BMD)的数据计算降雨偏差来分析气候条件。进行了焦点小组讨论(FGD)并与农民和不同部门的专家进行了访谈,以了解研究区域内问题的性质。 1980年代中期开始地下水灌溉后,农业格局,耕种强度(研究区为262%,全国耕地为180%),耕作方法,作物品种和单产均呈现出正向变化,但水位却以该速率持续下降。雨季为1.37英尺/年,旱季为0.72英尺/年。水资源是农业的主要投入,但是对于干旱胁迫的Barind Tract,地下水位的连续消耗可能是一个严重的问题。该地区可以选择作物多样化,人工补给,增加对地表水的依赖,提高灌溉效率,收集雨水等。

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