Vulnerability of Environmental Resources in Indus Basin after the Development of Irrigation System

M. Irfan, A. Qadir, Habib Ali, N. Jamil, S. Ahmad
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引用次数: 15

Abstract

The climatic and topographic characteristics of Indus Basin provided an excel-lent condition for the development of irrigation system. Archaeological remains of Harappa and Mohenjo-Daro indicated that several canals were constructed in this region. The Indus River System (IRS) was developed into a complex network of canals, and 74% of its water was utilized for irrigation after Indus Water Treaty. After 1947, Indus irrigation network was extended, and cropland area was increased from 8.5 to 18.2 MH in Pakistan and 2.02 to 8.5 MH in India. Construction of dams, barrages, and canals to divert the maximum river water for irrigation resulted in drying up the natural pathways of the rivers, except during monsoon season. The aquifer in the irrigated areas became high and created problems of waterlogging and salinity, but due to extensive groundwater extraction, water table near urban centers is lowered now. Water quality was degraded due to addition of fertilizers, pesticides, chemicals, municipal sewage, and industrial effluents. Due to climate change, the glaciers in the upper catchment areas are continuously retreating and the frequency of floods and droughts is increasing. The objective of this chapter is to provide a comprehensive review of irrigation system developments in Indus Basin and its implications on environmental resources.
灌溉系统发展后印度河流域环境资源脆弱性研究
印度河流域的气候和地形特征为灌溉系统的发展提供了良好的条件。哈拉帕和摩亨佐-达罗的考古遗迹表明,在这个地区修建了几条运河。印度河水系(IRS)发展成为一个复杂的运河网络,在印度河水条约之后,其74%的水被用于灌溉。1947年以后,印度河灌溉网络扩大,耕地面积从巴基斯坦的8.5增加到18.2 MH,印度的2.02增加到8.5 MH。建造水坝、拦河坝和运河来转移最大的河水用于灌溉,导致河流的自然通道干涸,除了在季风季节。灌溉区的含水层变得很高,造成了内涝和盐碱化的问题,但由于大量开采地下水,城市中心附近的地下水位现在降低了。由于添加肥料、农药、化学品、城市污水和工业废水,水质下降。由于气候变化,上游集水区冰川不断退缩,洪涝灾害频发。本章的目的是全面审查印度河流域灌溉系统的发展及其对环境资源的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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