首页> 外文期刊>Environmental earth sciences >A field demonstration of groundwater vulnerability assessment using transport modeling and groundwater age modeling, Beijing Plain, China
【24h】

A field demonstration of groundwater vulnerability assessment using transport modeling and groundwater age modeling, Beijing Plain, China

机译:北京平原平原利用运输模型和地下水年龄模型进行地下水脆弱性评估的现场演示

获取原文
获取原文并翻译 | 示例
       

摘要

Groundwater vulnerability is often regarded as the resistance of aquifers to pollutions, which is in fact the groundwater environment vulnerability. Similarly the renewable capacity of groundwater system can be regarded as the indicator for groundwater resources vulnerability. In this paper, the concept of groundwater vulnerability is extended to include both the groundwater environment vulnerability and groundwater resources vulnerability, and the extended overall groundwater vulnerability is assessed by examining the solute transport process from ground surface to the water table (for groundwater environment vulnerability), and evaluating the renewable capacity of groundwater system (for groundwater resources vulnerability). For this case study in Beijing Plain, a 1D-modeling, 2D-mapping model is constructed in HYDRUS to simulate the solute transport process through vadose zone. The transit times and solute concentrations at the water table are selected as the indicators for groundwater environment vulnerability. Meanwhile, a 3D groundwater age model in MODFLOW/MT3DMS is employed to model the age distribution in saturated zone, and the modeled ages are taken as the indicators for groundwater resources vulnerability. These two models are coupled together by exchanging their vertical infiltrations and water table elevations. Overall vulnerability is finally assessed by taking all the indicators into account. The result suggests the overall vulnerability can finely represent the synthetic impact of solute transport characteristics (groundwater environment vulnerability in vadose zone) and groundwater system renewability (groundwater resources vulnerability in saturated zone). The most vulnerable regions of Beijing Plain are mostly in agricultural areas, the medium vulnerable areas mostly appear at pumping sites, and the least vulnerable areas are mostly distributed in recharge regions.
机译:地下水脆弱性通常被认为是含水层对污染的抵抗力,实际上是地下水环境的脆弱性。同样,地下水系统的可再生能力也可以看作是地下水资源脆弱性的指标。本文将地下水脆弱性的概念扩展到既包括地下水环境脆弱性又包括地下水资源脆弱性,并且通过检查从地表到地下水位的溶质运移过程(对于地下水环境脆弱性)来评估扩展的总体地下水脆弱性。 ,并评估地下水系统的可再生能力(针对地下水资源的脆弱性)。对于北京平原的此案例研究,在HYDRUS中构建了一个1D建模,2D映射模型,以模拟溶质在渗流带中的传输过程。选择地下水位的迁移时间和溶质浓度作为地下水环境脆弱性的指标。同时,利用MODFLOW / MT3DMS中的3D地下水年龄模型对饱和带中的年龄分布进行建模,并将建模后的年龄作为地下水资源脆弱性的指标。这两个模型通过交换其垂直入渗量和地下水位高程而耦合在一起。最后,通过考虑所有指标来评估总体脆弱性。结果表明,总体脆弱性可以很好地代表溶质运移特征(渗流带中的地下水环境脆弱性)和地下水系统可再生性(饱和带中的地下水资源脆弱性)的综合影响。北京平原最脆弱的地区主要分布在农业地区,中度脆弱的地区主要分布在抽水站,脆弱程度最低的地区主要分布在补给地区。

著录项

  • 来源
    《Environmental earth sciences》 |2015年第9期|5245-5253|共9页
  • 作者单位

    Chongqing Jiaotong Univ, Key Lab Hydraul & Waterway Engn, Minist Educ, Chongqing, Peoples R China|Peking Univ, Ctr Water Res, Beijing 100871, Peoples R China;

    Peking Univ, Ctr Water Res, Beijing 100871, Peoples R China;

    Peking Univ, Ctr Water Res, Beijing 100871, Peoples R China;

    Peking Univ, Ctr Water Res, Beijing 100871, Peoples R China|Univ Alabama, Dept Geol Sci, Tuscaloosa, AL USA;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Beijing Plain; Groundwater vulnerability; Groundwater age; Solute transport;

    机译:北京平原地下水脆弱性地下水时代溶质运移;
  • 入库时间 2022-08-18 03:31:00

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号