首页> 外文期刊>Journal of Hydrology >Estimating groundwater mixing ratios and their uncertainties using a statistical multi parameter approach
【24h】

Estimating groundwater mixing ratios and their uncertainties using a statistical multi parameter approach

机译:使用统计多参数方法估算地下水混合比及其不确定性

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

The estimation of groundwater mixing ratios is a crucial task in groundwater research and management. The quantity as well as the quality of groundwater resources are sensible to, e.g. the admixture river water, the interaction between different groundwater layers and the spatial distribution of such mixing zones. In this paper, we present a procedure to calculate mixing ratios and their uncertainties using a set of chemical and isotopic parameters. The advantages compared to estimations based on only few parameters are better-constrained mixing ratios and the limitation of systematic errors due to the parameter choice. The statistical consistence of the resulting mixing ratios is checked with a chi(2)-test.In particular in larger aquifers, where sampling resolution is often coarse, the composition of end members may vary considerably from one borehole to another due to rock water interaction or varying recharge conditions. After selecting sampling sites where no mixing occurs, the spatial distribution of the end member composition was calculated using Kriging. This provides the best estimates of end member compositions and their uncertainties at any location of the area of investigation.The method is, in principle, applicable for any number of end members. In this paper, the spatial distribution of the interaction of two layers of the Continental Terminal aquifer (Niger, Africa) was investigated. Mixing between the deep CT2 and the shallow CT3 aquifer occurs where the separating layers are thinning out or due to improper sealing of some boreholes. Radiogenic He-4 concentrations, which differ significantly in the two aquifers, were used as independent parameter to crosscheck the mixing calculations. (c) 2004 Elsevier B.V. All rights reserved.
机译:地下水混合比的估算是地下水研究和管理中的关键任务。地下水资源的数量和质量对例如混合河水,不同地下水层之间的相互作用以及这些混合区的空间分布。在本文中,我们提出了使用一组化学和同位素参数来计算混合比及其不确定性的程序。与仅基于少数几个参数进行估计相比,其优势在于混合比例得到了更好的约束,并且由于参数选择而限制了系统误差。通过chi(2)测试检查所得混合比的统计一致性。特别是在较大的含水层中,采样分辨率通常较粗糙,由于岩水相互作用,端部构件的组成可能因一个钻孔而异。或不同的充电条件。在选择不发生混合的采样位置后,使用Kriging计算末端成员组成的空间分布。这样可以在调查区域的任何位置提供对末端成员组成及其不确定性的最佳估计。该方法原则上适用于任何数量的末端成员。本文研究了大陆终端含水层(非洲尼日尔)两层相互作用的空间分布。深层CT2和浅层CT3含水层之间会发生混合,这是在分隔层变薄或某些井眼密封不当的情况下发生的。在两个含水层中显着不同的放射成因He-4浓度用作独立参数,以交叉检查混合计算。 (c)2004 Elsevier B.V.保留所有权利。

著录项

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