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河床垂向渗透系数空间变异性的三维分析

介飞龙 李升

人民黄河2018,Vol.40Issue(4):49-54,6.
人民黄河2018,Vol.40Issue(4):49-54,6.DOI:10.3969/j.issn.1000-1379.2018.04.012

河床垂向渗透系数空间变异性的三维分析

Analysis of Three Dimensional Spatial Variability of Vertical Streambed Hydraulic Conductivity

介飞龙 1李升1

作者信息

  • 1. 新疆大学 地质与矿业工程学院,新疆 乌鲁木齐830046
  • 折叠

摘要

Abstract

The vertical streambed hydraulic conductivity plays an important role and has great significance in the study of the conversion mechanism of streambed water and groundwater. This paper studied on the determination of the Yurungqash River a total of 25 test points of vertical streambed hydraulic conductivity using seepage meter method and standpipe method. It studied the spatial variation characteristics of vertical streambed hydraulic conductivity with different depths,vertical directions of river and route directions,analyzed the influencing fac-tors of variability,and summarized the dimensional effect of the variability of the vertical streambed hydraulic conductivity. The results show that Yurungqash River vertical streambed hydraulic conductivity is affected by many factors,including floods,aeolian sedimentation and wa-ter dynamic effect;in different dimensions,the dominant factors of vertical streambed variability of hydraulic conductivity are different. Vari-ability of vertical streambed hydraulic conductivity can not be determined by a single factor.

关键词

垂向渗透系数/变异性/河床/维度效应/玉龙喀什河

Key words

vertical hydraulic conductivity/variability/streambed/dimensional effect/Yurungqash River

分类

天文与地球科学

引用本文复制引用

介飞龙,李升..河床垂向渗透系数空间变异性的三维分析[J].人民黄河,2018,40(4):49-54,6.

基金项目

国家自然科学基金资助项目(U1603243). (U1603243)

人民黄河

OA北大核心CSTPCD

1000-1379

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