人民黄河Issue(7)：60-64,5.DOI:10.3969/j.issn.1000-1379.2014.07.019
那陵郭勒河冲洪积扇地表水-地下水转化关系
Study on the Interaction Relationship Between Surface Water and Groundwater in Nalingguole River Alluvial-Oroluvial Fan
摘要
Abstract
On the Basis of the hydrogen and oxygen stable isotopes data about water in the Nalingguole River(called the Na River for short)alluvi-al-proluvial fan area,this study illustrated the interaction relationship between groundwater and surface water along the Na River in alluvial-proluvi-al fan area. The results demonstrate that groundwater in the alluvial-proluvial fan is mainly recharged by atmospheric precipitation and snowmelt from the southern mountains. Groundwater and surface water have the same origin and the interactions between them occur repeatedly. It shows dif-ferent kinds of conversion modes in different sections of the Na River alluvial-proluvial fan area. In the upper reaches of the river(the mountain zone),the hydraulic connection between surface water and groundwater is weak. In the middle reaches of the river(the uplift zone),groundwater recharges the surface water. In the downstream of the river(middle of the alluvial-proluvial fan),groundwater is recharged by surface water. In the front of the alluvial-proluvial fan,the groundwater overflows and forms springs,then springs are collected into the surface water.关键词
冲洪积扇/氢氧稳定同位素/地表水地下水转化/那陵郭勒河Key words
alluvial-proluvial fan/hydrogen and oxygen stable isotope/interaction between surface water and groundwater/Nalingguole River分类
建筑与水利引用本文复制引用
朱谱成,苏小四,张世广,黄勇,杨峰田,徐威..那陵郭勒河冲洪积扇地表水-地下水转化关系[J].人民黄河,2014,(7):60-64,5.基金项目
中国地质调查局地质调查工作项目（1212011121279）；教育部新世纪优秀人才支持计划项目（NCET -11-0200）。 （）
