Zhao Wei, Lin Jian, Wang Shu-Fang, Liu Ji-Lai, Chen Zhong-Rong, Kou Wen-Jie
Beijing Institute of Hydrogeology and Engineering Geology, Beijing 100195, China.
Huan Jing Ke Xue. 2013 Apr;34(4):1277-83.
Groundwater system in the plain area of Beijing can be divided into six subsystems. Due to the different hydrogeological conditions of the subsystems, the degrees to which human activities affect the subsystems are also diverse. In order to evaluate the influence of human activities on each subsystem, the first and second aquifer with relatively poor water quality were chosen to be the evaluating positions, based on the data of groundwater sampled in September, 2011. With respect to human activities affect index such as total hardness, TDS, sulfate and ammonium, variation coefficient methods were used to calculate the weight of each index. Then scores were obtained for each index with national standard as reference, and superposition calculations were used to gain comprehensive scores, finally the groundwater quality conditions were evaluated. Contrast analyses were used to evaluate the incidence of human activities with groundwater subsystems as evaluation unit and water quality partitions as evaluation factors. The results indicate that the influence of human activities on the first aquifer is greater than that of the second aquifer, the Yongding river groundwater subsystems and the Chaobai river groundwater subsystems are affected more than other groundwater subsystems.
北京平原地区的地下水系统可分为六个子系统。由于各子系统水文地质条件不同,人类活动对各子系统的影响程度也存在差异。为评估人类活动对各子系统的影响,依据2011年9月采集的地下水数据,选取水质相对较差的第一、第二含水层作为评价点位。针对总硬度、溶解性总固体、硫酸盐、铵等人类活动影响指标,采用变异系数法计算各指标权重。然后以国家标准为参照得出各指标得分,通过叠加计算得到综合得分,最终对地下水水质状况进行评价。以地下水子系统为评价单元、水质分区为评价因素,采用对比分析评估人类活动的影响情况。结果表明,人类活动对第一含水层的影响大于第二含水层,永定河地下水子系统和潮白河地下水子系统受影响程度高于其他地下水子系统。