[1]李娟,叶立,张维江.宁夏中部干旱风沙区降雨入渗补给系数的估算[J].水土保持研究,2009,16(01):22-26.
　LI Juan,YE Li,ZHANG Wei-jiang.The Estimation of the Rainfall Infiltration Coefficient of Arid Aeolian Sand Region in the Middle Area of Ningxia[J].Research of Soil and Water Conservation,2009,16(01):22-26.
点击复制

宁夏中部干旱风沙区降雨入渗补给系数的估算

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 16 期数: 2009年01期 页码: 22-26 栏目: 出版日期: 2009-02-20
Title:
The Estimation of the Rainfall Infiltration Coefficient of Arid Aeolian Sand Region in the Middle Area of Ningxia
作者:
李娟1, 叶立2, 张维江1
1. 宁夏大学 土木与水利工程学院, 银川 750021;
2. 宁夏第二测绘院, 银川 750021
Author(s):
LI Juan1, YE Li2, ZHANG Wei-jiang1
1. Civil and Water Conservancy Engineering College of Ningxia University, Yinchuan 750021, China;
2. The Second Surveying and Mapping Unit, Yinchuan 750021, China
关键词:
干旱风沙区; 降雨入渗补给系数; 起始有效雨量
Keywords:
arid aeolian sand region; the coefficient of rainfall infiltration; the beginning effective rainfall
分类号:
S157;S273
摘要:
降雨入渗补给量是干旱地区地下水资源的重要组成部分，降雨入渗补给系数取用的正确与否直接关系到降雨入渗补给量的估算。宁夏中部干旱风沙区地下水资料相对较少，只能采用现场观测与验证结合的方式进行确定。利用宁夏盐池县猫头梁降雨资料与地下水动态观测资料对宁夏中部干旱风沙区的降雨入渗补给系数进行估算，并用宁夏同心县长沙河流域地下水资料进行验证，得出宁夏中部干旱风沙区的降雨入渗补给系数0.119～0.257，为该地区水资源评价工作提供依据。
Abstract:
The water resource infiltrated by rainfall is an important part of the underground water resource, which is affected by the coefficient of rainfall infiltration. The data of underground water resource in the arid aeolian sand region of Ningxia is limited; the coefficient of rainfall infiltration only can be decided through observing and verifying. The thesis estimates the coefficient of rainfall infiltration in the Middle Area of Ningxia with the precipitation data and dynamic observed records of groundwater of Maotouliang in Yanchi County, then test it with the observed records of Changshahe watershed in Tongxin County, and conclud that the coefficient of rainfall infiltration in the Middle Area of Ningxia is 0.119～0.257, which can offer reliable reference for the further study on the evaluation work of the water resources.

参考文献/References:

[1] 王志强.江汉平原四湖地区地下水参数的分析[J].水文, 1995(4):35-39.
[2] 张平, 李日运.降雨入渗补给地下水的影响因素[J].辽宁大学学报自然科学版, 1999(2):118-122.
[3] 陈志辉.黑河干流平原区大气降水入渗补给潜水机制的研究[J].甘肃地质学报, 1997(6):37-40.
[4] 齐仁贵.用地下水动态资料分析降雨入渗对地下水的补给[J].武汉水利电力大学学报, 1999, 6(3):58-62.
[5] 梁文彪.应用回归分析方法推求降水入渗补给系数[J].地下水, 2002, 24(2):71-73.
[6] 金光炎, 汪家权等.地下水计算参数的测定与估计[J].水科学进展, 1997, 8(1):17-24.
[7] 张维江, 李娟, 王东, 等.宁夏中部风沙区地表径流预报模型研究[J].人民黄河, 2004, 26(2):35-37.
[8] 全达人.地下水利用(3版)[M].北京:中国水利水电出版社, 1996:69-73.

相似文献/References:

[1]卜崇德,张维江.宁夏中部干旱风沙区地下水资源估算方法研究[J].水土保持研究,2004,11(03):41.
　BU Chong-de,ZHANG Wei-jiang.Study on Estimated Method of Groundwater Resources of Arid Aeolian Sand Region in the Middle Area of Ningxia[J].Research of Soil and Water Conservation,2004,11(01):41.
[2]何全发,王占军,蒋齐,等.干旱风沙区人工柠条林对退化沙地改良效果的关联度分析与综合评价[J].水土保持研究,2007,14(01):234.
　HE Quan-fa,WANG Zhan-jun,JIANG Qi,et al.Garagana Plantation of Arid Aeolian Sand Region for Degraded Sand Land Improve Comprehensive Appraisement and Grey Correlative Analysis[J].Research of Soil and Water Conservation,2007,14(01):234.
[3]郗伟华,刘任涛,刘佳楠,等.干旱风沙区立地条件、季节变化对柠条灌丛“虫岛”效应的影响[J].水土保持研究,2018,25(02):162.
　XI Weihua,LIU Rentao,LIU Jianan,et al.Comparison of ‘Arthropod Island’ Acted by Caragana Shrub Canopy Under Different Microsite Conditions Across Seasonal Changes in Desertified Region[J].Research of Soil and Water Conservation,2018,25(01):162.
[4]郗伟华,刘任涛,赵娟,等.干旱风沙区路域柠条灌丛林地土壤重金属分布及其与土壤分形维数的关系[J].水土保持研究,2018,25(06):196.
　XI Weihua,LIU Rentao,ZHAO Juan,et al.Distribution of Soil Heavy Metal Contents in Caragana korshinskii Shrub Habitats on the Proximity of Expressway and Its Relationship With Soil Fractal Dimension in Deserted Region[J].Research of Soil and Water Conservation,2018,25(01):196.

备注/Memo

收稿日期:2008-4-25。
基金项目:“十一五”科技支撑计划“宁夏河东沙地退化草地植被恢复与利用技术研究与试验示范（盐池）”（2006BAD26B0702）
作者简介:李娟（1981- ），女，宁夏中卫人，硕士，主要从事旱区水资源和水土保持与荒漠化防治方面的教学与研究工作。E-mail：lijuanshuibao@163.com

更新日期/Last Update: 1900-01-01