[1]胡小韦,海米提·依米提,艾尼瓦尔·买买提,等.塔里木胡杨自然保护区地下水理化特性相互关系研究[J].水土保持研究,2007,14(05):320-323.
　HU Xiao-wei,Hamit·Yimit,Anwar·Mohammed,et al.Study on Correlation Between Physics and Chemistry Characteristic of Groundwater in Tarim Populus euphratic Nature Reserve Area[J].Research of Soil and Water Conservation,2007,14(05):320-323.
点击复制

塔里木胡杨自然保护区地下水理化特性相互关系研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 14 期数: 2007年05期 页码: 320-323 栏目: 出版日期: 1900-01-01
Title:
Study on Correlation Between Physics and Chemistry Characteristic of Groundwater in Tarim Populus euphratic Nature Reserve Area
作者:
胡小韦1,2, 海米提·依米提1,2,3, 艾尼瓦尔·买买提1,2, 木巴热克1,2, 冯振忠4
1. 绿洲生态系统安全与可持续发展实验室, 乌鲁木齐 830046;
2. 新疆大学 资源与环境科学学院, 乌鲁木齐 830046;
3. 干旱半干旱区可持续发展国际研究中心, 乌鲁木齐 830046;
4. 塔里木河流域管理局, 新疆 库尔勒 841000
Author(s):
HU Xiao-wei1,2, Hamit·Yimit1,2,3, Anwar·Mohammed1,2, Mubarek1,2, FENG Zhen-zhong4
1. Key Laboratory of Oasis Ecology and Sustainable Development, Urumqi 830046, China;
2. Resource and Environmental College of Xinjiang University, Urumqi 830046, China;
3. International Center for Desert Affairs-Research for Sustainable Development in Semi-Arid and Arid Land, Urumqi 830046, China;
4. The Manage bureau of Tarim Basin in Kuerle, Kuerle, Xinjiang 841000, China
关键词:
地下水; 理化特性; 相关分析; 回归分析
Keywords:
groundwater; physical and chemical characteristic; correlation analysis; regression analysis
分类号:
P641.12
摘要:
通过对塔里木河胡杨林自然保护区地下水理化特性相互关系的研究，结果表明：地下水埋深和pH值与电导率、含盐量、矿化度的相关系数不大。电导率和含盐量、矿化度的相关系数分别为0.974和0.984，含盐量与矿化度相关系数为0.998，以此得出电导率与矿化度、含盐量回归模型。
Abstract:
To study the correlation between physics and chemistry characteristic which were in the Tarim Populus euphratic nature reserve area,the conclusion show that the depth of the groundwater and pH have a poor correlativity with the conductivity,salinity,TDS.The conductivity and salinity,TDS turn the related coefficient is 0.992 and 0.984,the salinity and TDS’s coefficient is 0.998.Therefore,the conductivity and TDS,salinity’s regression model is made.

参考文献/References:

[1] 樊自立, 马英杰, 张宏, 等.塔里木河流域生态地下水位及其合理深度确定[J].干旱区地理, 2004, 27(1):67-69.
[2] 陈永金, 陈亚宁, 李卫红, 等.塔里木河下游地下水化学特征对生态输水的响应[J].地理学报, 2005, (60):51-53.
[3] 宋郁东, 樊自立, 雷志栋, 等.中国塔里木河水资源与生态问题研究[M].乌鲁木齐:新疆人民出版社, 2000.
[4] 李立人.百口泉地下水电导率与溶解性总固体相关性讨论[J].水污染治理油气田环境保护, 1998, (9):3-15.
[5] 陈果平.地下水电导率与总硬度相关关系的研究[J].技术交流, 2000.110-111.
[6] 李立人.地下水电导率与溶解性总固体相关性探讨[J].干旱环境监测, 1999, 13(2):34-35.
[7] 杜鹏飞, 李虹, 海春兴, 等.阴山北麓春季土壤含盐量及其与电导率的关系研究[J].内蒙古师范大学学报(自然科学汉文版), 2006, 35(2):23-25.
[8] 吴诗怡.塔克拉玛干沙漠地下水矿化度与电导率关系的研究[J].中国沙漠, 1996, 16(4):34-36.
[9] 姚井华.用电导率测定地下水矿化度[J].中国环境监测, 1986, 2(2):31-33.
[10] 李刚, 王永冰.昌吉市地下水中离子总量与电导率间关系研究[J].地下水, 1995, 17(4):23-26.
[11] 张宏安, 曹海涛, 李晓铃, 等.塔里木河干流输水堤建设两岸天然植被的影响及保护对策[J].水电站设计.2004, 20(1):56-58.
[12] 伏小石, 张平, 张化, 等.地下水pH值、电导率和浊度实时监测仪器[J].仪表技术与传感器, 2004, 11(3):45-48.
[13] 中国土壤学会农业化学专业委员会.土壤农业化学常规分析方法[M].北京:科学出版社, 1989.199-202.
[14] 吴诗怡.塔克拉玛干沙漠地下水矿化度与电导率关系的研究[J].中国沙漠, 1996, 16(4):87-89.

相似文献/References:

[1]杨红,许模,张劲松.滇东南弥勒盆地蓄水构造特征分析及找水方向[J].水土保持研究,2012,19(06):254.
　YANG Hong,XU Mo,ZHANG Jin-song.Analysis of the Characteristics of Groundwater Storage Structure and Groundwater Exploration in Mile Basin, Southeast Yunnan Province[J].Research of Soil and Water Conservation,2012,19(05):254.
[2]刘东,张健,付强.三江平原井灌区地下水人工回灌量测算[J].水土保持研究,2012,19(02):240.
　LIU Dong,ZHANG Jian,FU Qiang.Estimation of Groundwater Artificial Recharge Quantity in Area of Well Irrigation in Sanjiang Plain[J].Research of Soil and Water Conservation,2012,19(05):240.
[3]金绍兴,秦启文,范致豪,等.屏东平原之地下水经理[J].水土保持研究,1999,6(03):9.
　Shao-Hsing King,Chi-Van Chin,Chih-Hao Fan,et al.Groundwater Management in Pingtung Plain[J].Research of Soil and Water Conservation,1999,6(05):9.
[4]许中立,李正义.边坡稳定逆算分析法之应用探讨[J].水土保持研究,1999,6(03):80.
　Chung-LiHsu,Cheng-Yi Lee.The Application of Back Stability Analysis on Landslide Slope[J].Research of Soil and Water Conservation,1999,6(05):80.
[5]毛学森,刘昌明.太行山山前平原地下水变化趋势与农业持续发展[J].水土保持研究,2001,8(01):147.
　MAO Xuesen,LIU Changming.Ground Water Changing Trends and Agriculture Sustainable Development in Taihang Mountain-foot Plain of North China[J].Research of Soil and Water Conservation,2001,8(05):147.
[6]王恩志,王慧明,李昂,等.石门子水库近坝区渗漏与防渗分析[J].水土保持研究,2001,8(04):79.
　WANG En-zhi,WANG Hui-ming,LI Ang,et al.Analysis on Seepage and Anti-seepage Method of the Areas Near Shimenzi Reservoir[J].Research of Soil and Water Conservation,2001,8(05):79.
[7]唐小娟,吴普特.杨陵区地表水及地下水环境质量评价[J].水土保持研究,2002,9(02):135.
　TANG Xiao-juan,WU Pu-te.Environmental Quality Evaluation of Surface and Groundwater in Yangling[J].Research of Soil and Water Conservation,2002,9(05):135.
[8]罗芳,肖洪浪,齐善忠,等.额济纳三角洲地下水现状分析[J].水土保持研究,2005,12(01):56.
　LUO Fang,XIAO Hong-lang,QI Shan-zhong,et al.Changeable Characteristics of Groundwater and Salt in Erjina Oasis, Arid Northwestern China[J].Research of Soil and Water Conservation,2005,12(05):56.
[9]李海涛,许学工,肖笃宁.武威绿洲水资源利用分析[J].水土保持研究,2005,12(04):128.
　LI Hai-tao,XU Xue-gong,XIAO Du-ning.Analysis of Water Resources Utilization in Wuwei Oasis[J].Research of Soil and Water Conservation,2005,12(05):128.
[10]盛海洋,孟秋立,朱殿华,等.我国地下水开发利用中的水环境问题及其对策[J].水土保持研究,2006,13(01):51.
　SHENG Hai-yang,MENG Qiou-li,ZHU Dian-hua,et al.Environmental Problems of Underground Water Resources Development Use and Prevention and Control[J].Research of Soil and Water Conservation,2006,13(05):51.

备注/Memo

收稿日期:2006-11-8。
基金项目:国家自然科学基金项目（40661002）；自治区高校重点研究项目（XJEDU2006I09）；新疆绿洲生态重点实验室开放课题（XJDX02060401）；“春晖计划”项目（新疆胡杨林资源及其保护）（030144）
作者简介:胡小韦（1982- ），男，新疆阿克苏人，硕士研究生，主要从事干旱区水资源与环境研究。
通讯作者:海米提·依米提，教授，博导。

更新日期/Last Update: 1900-01-01