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下恒河流域地下水灌溉适宜性评价——基于水文地球化学参数和土地利用动态变化。

Suitability of the Lower Ganga basin groundwater for irrigation, using hydrogeochemical parameters and land-use dynamics.

机构信息

Centre for Ocean, River, Atmosphere and Land Sciences, Indian Institute of Technology Kharagpur, Kharagpur, West Bengal, 721302, India.

Department of Civil Engineering, Aliah University, New Town, West Bengal, 700160, India.

出版信息

Environ Sci Pollut Res Int. 2023 Nov;30(55):116831-116847. doi: 10.1007/s11356-022-24708-9. Epub 2023 Jan 3.

Abstract

The northern Ganga basin is one of the most densely populated basins in the world. Most agricultural and industrial contaminants drained in the river length are likely to be accumulated in the lower part of the Ganga basin. In this study, we have used ten parameters obtained from 495 sampling locations, besides using long-term climate data (GLDAS_NOAH025_M) to understand the irrigation suitability using the TOPSIS model. Multi-criteria decision making (MCDM) model using TOPSIS has been used to make the best choices from the available finite number of alternatives based on their ranking. The entropy weights for the irrigation suitability parameters such as electrical conductivity (Ec), sodium adsorption ratio (SAR), magnesium hardness (MH), sodium percent (Na%), total hardness (TH), Kelly's ratio (KR), permeability index (PI), chloride concentration (Cl), groundwater level fluctuation (GWLF), and the Lang factor (Df) are found to be 0.08, 0.14, 0.02, 0.02, 0.04, 0.08, 0.01, 0.32, 0.29, and 0.01, respectively. We find that SAR, Cl, and GWLF control the water quality for irrigation in the Lower Ganga basin since these parameters have relatively higher entropy weights (more than 0.10). The results obtained from the computed performance index or the closeness coefficient show that the area percent having very good and good groundwater quality for irrigation in the Lower Ganga basin is 77.03% and 22.97% respectively. The land-use change dynamics for the between 2000 and 2015 estimated using the transition matrix shows a positive percentage change for settlement (133.50%), wetland (35.04%), and bare area (0.98%); however, several other classes such as the agriculture (- 0.85%), forest (- 0.49%), grassland (- 14.38%), sparse vegetation (- 11.39%), and water (- 4.12%) show a decreasing trend. The highest amount of percentage change was observed in settlement areas which were contributed by other land-use classes such as agriculture (694.43 km), water (41.61 km), forest (16.77 km), and grassland (1.86 km). The results may be useful to the concerned organization for the proper planning and management of water resource for sustainable development.

摘要

恒河流域北部是世界上人口最密集的流域之一。排入恒河干流的大部分农业和工业污染物很可能在恒河流域的下游积聚。在这项研究中,我们使用了来自 495 个采样点的十个参数,以及长期气候数据(GLDAS_NOAH025_M),使用 TOPSIS 模型来了解灌溉适宜性。使用多准则决策(MCDM)模型中的 TOPSIS,根据其排名,从可用的有限数量的替代方案中进行最佳选择。灌溉适宜性参数的熵权重,如电导率(Ec)、钠吸附比(SAR)、镁硬度(MH)、钠百分比(Na%)、总硬度(TH)、凯利比(KR)、渗透率指数(PI)、氯浓度(Cl)、地下水位波动(GWLF)和 Lang 因子(Df)分别为 0.08、0.14、0.02、0.02、0.04、0.08、0.01、0.32、0.29 和 0.01。我们发现,SAR、Cl 和 GWLF 控制着恒河下游的灌溉水质,因为这些参数的熵权重相对较高(超过 0.10)。从计算得出的绩效指数或接近系数得到的结果表明,恒河下游非常适合和适合灌溉的地下水面积百分比分别为 77.03%和 22.97%。使用转移矩阵估计的 2000 年至 2015 年之间的土地利用变化动态显示,定居点(133.50%)、湿地(35.04%)和裸地(0.98%)的正百分比变化;然而,其他几个类别,如农业(-0.85%)、森林(-0.49%)、草地(-14.38%)、稀疏植被(-11.39%)和水(-4.12%)则呈下降趋势。定居点的百分比变化最大,这是由其他土地利用类别如农业(694.43km)、水(41.61km)、森林(16.77km)和草地(1.86km)贡献的。这些结果可能对有关组织在可持续发展方面对水资源进行适当规划和管理有用。

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