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尼泊尔城市河流走廊地表水和地下水水质的时空格局评估及影响地下水系统管理策略的因素

Assessment of spatial-temporal patterns of surface and ground water qualities and factors influencing management strategy of groundwater system in an urban river corridor of Nepal.

作者信息

Kannel Prakash Raj, Lee Seockheon, Lee Young-Soo

机构信息

Water Environment & Remediation Research Center, Korea Institute of Science and Technology, Cheongryang, Seoul, Republic of Korea.

出版信息

J Environ Manage. 2008 Mar;86(4):595-604. doi: 10.1016/j.jenvman.2006.12.021. Epub 2007 Feb 6.

Abstract

This study examined the spatial-temporal variations and factors influencing the management of groundwater along a section of the Bagmati river corridor in the Kathmandu valley (Nepal). The results showed that rural areas were less polluted than urban areas. In urban areas, the biochemical oxygen demand (BOD), total nitrogen (TN) and total phosphorus (TP) concentrations ranged from 8.41 to 29.74 mg/L, 6.7 to 128.96 mg/L and 0.06 to 1.5 mg/L, respectively. In rural areas, the BOD, TN and TP concentrations ranged from 0.78 to 18.25 mg/L, 4.8 to 11.56 mg/L and 0.07 to 0.65 mg/L, respectively. The level of organics was higher in the pre-monsoon season, while the level of nutrients was higher in post-monsoon season. A comparison of the groundwater and surface water in the upstream rural areas revealed that the TP concentration was higher in the groundwater than in the surface water, which was attributed to the sorption of phosphorus on iron, aluminum or calcium compounds contained in the surface water, which depends upon the temperature, pH and dissolved oxygen. In urban areas, a few wells were found at groundwater levels lower than the corresponding surface water levels and were subjected to a high risk of pollution. Overall, these findings reinforce the notion that the management of surface and ground waters in an integrated approach is essential for attaining sustainable development of groundwater systems.

摘要

本研究考察了尼泊尔加德满都谷地巴格马蒂河走廊某一区域地下水管理的时空变化及影响因素。结果表明,农村地区的污染程度低于城市地区。在城市地区,生化需氧量(BOD)、总氮(TN)和总磷(TP)浓度分别在8.41至29.74毫克/升、6.7至128.96毫克/升和0.06至1.5毫克/升之间。在农村地区,BOD、TN和TP浓度分别在0.78至18.25毫克/升、4.8至11.56毫克/升和0.07至0.65毫克/升之间。季风前季节有机物含量较高,而季风后季节营养物质含量较高。对上游农村地区的地下水和地表水进行比较发现,地下水中的TP浓度高于地表水中的TP浓度,这归因于磷在地表水中所含铁、铝或钙化合物上的吸附,而这取决于温度、pH值和溶解氧。在城市地区,发现一些井的地下水位低于相应的地表水位,且面临着较高的污染风险。总体而言,这些发现强化了这样一种观念,即采用综合方法管理地表水和地下水对于实现地下水系统的可持续发展至关重要。

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