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Reviving the Ganges Water Machine: potential

机译:复兴恒河水机:潜力

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The Ganges River basin faces severe water challenges related to a mismatch between supply and demand. Although the basin has abundant surface water and ground-water resources, the seasonal monsoon causes a mismatch between supply and demand as well as flooding. Water availability and flood potential is high during the 3-4 months (June-September) of the monsoon season. Yet, the highest demands occur during the 8-9 months (October-May) of the non-monsoon period. Addressing this mismatch, which is likely to increase with increasing demand, requires substantial additional storage for both flood reduction and improvements in water supply. Due to hydrogeological, environmental, and social constraints, expansion of surface storage in the Ganges River basin is problematic. A range of interventions that focus more on the use of subsurface storage (SSS), and on the acceleration of surface-subsurface water exchange, has long been known as the Ganges Water Machine (GWM). The approach of the GWM for providing such SSS is through additional pumping and depleting of the groundwater resources prior to the onset of the monsoon season and recharging the SSS through monsoon surface runoff. An important condition for creating such SSS is the degree of unmet water demand. The paper shows that the potential unmet water demand ranging from 59 to 124 Bm(3) year(-1) exists under two different irrigation water use scenarios: (i) to increase irrigation in the Rabi (November-March) and hot weather (April-May) seasons in India, and the Aman (July-November) and Boro (December-May) seasons in Bangladesh, to the entire irrigable area, and (ii) to provide irrigation to Rabi and the hot weather season in India and the Aman and Boro seasons in Bangladesh to the entire cropped area. However, the potential for realizing the unmet irrigation demand is high only in 7 sub-basins in the northern and eastern parts, is moderate to low in 11 sub-basins in the middle, and has little or no potential in 4 sub-basins in the western part of the Ganges basin. Overall, a revived GWM plan has the potential to meet 45-84 Bm(3) year(-1) of unmet water demand.
机译:恒河流域面临与供需不平衡有关的严峻用水挑战。尽管流域拥有丰富的地表水和地下水资源,但季节性的季风导致供求不平衡以及洪水泛滥。在季风季节的3-4个月(6月至9月),水的可用性和洪灾潜力很高。然而,最高需求发生在非季风期的8-9个月(10月至5月)。要解决这种不匹配现象,这种不匹配现象可能会随着需求的增加而增加,因此需要大量的额外存储以减少洪水和改善供水。由于水文地质,环境和社会的限制,恒河流域地表存储的扩展存在问题。长期以来,人们将一系列专注于地下存储(SSS)使用和加速地表下地下水交换的干预措施称为恒河水机(GWM)。 GWM提供这种SSS的方法是在季风季节开始之前通过额外抽水和消耗地下水资源,并通过季风地表径流给SSS补充水。建立这样的SSS的重要条件是未满足需求的程度。本文显示,在两种不同的灌溉用水情况下,潜在的未满足需求量为59至124 Bm(3)年(-1):(i)增加拉比(11月至3月)的灌溉量和炎热天气(印度的4月至5月)季节,孟加拉国的Aman(7月至11月)和Boro(12月至5月)季节,到整个可灌溉区域,以及(ii)为拉比提供灌溉,印度和印度的炎热季节孟加拉国的Aman和Boro季节遍及整个种植区。但是,只有北部和东部的7个子流域实现未满足的灌溉需求的潜力很高,中部的11个子流域中到中等的需求较低,而中国的4个子流域的潜力很小甚至没有。恒河盆地西部。总体而言,已恢复的GWM计划有可能满足45-84 Bm(3)年(-1)的未满足用水需求。

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