[1]夏梦,马龙,吉力力·阿不都外力.玛纳斯河流域中下游平原地区水化学特征及其影响因素[J].水土保持研究,2015,22(02):136-140,146.
　XIA Meng,MA Long,JILILI·Abuduwaili.The Water Chemical Characteristics and Its Influence Factors in Middle and Lower Reaches of Manasi River Basin[J].Research of Soil and Water Conservation,2015,22(02):136-140,146.
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玛纳斯河流域中下游平原地区水化学特征及其影响因素

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 22 期数: 2015年02期 页码: 136-140,146 栏目: 出版日期: 2015-04-28
Title:
The Water Chemical Characteristics and Its Influence Factors in Middle and Lower Reaches of Manasi River Basin
作者:
夏梦1, 马龙2, 吉力力·阿不都外力2
1. 新疆大学 资源与环境科学学院, 乌鲁木齐 830046;
2. 中国科学院 新疆生态与地理研究所 荒漠与绿洲生态国家重点实验室, 乌鲁木齐 830011
Author(s):
XIA Meng1, MA Long2, JILILI·Abuduwaili2
1. College of Resource and Environment Sciences, Xinjiang University, Urumqi 830046, China;
2. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
关键词:
水文学; 水化学特征; 影响因素; 聚类分析; 玛纳斯河
Keywords:
hydrology; hydrochemical characteristics; influencing factors; hierarchical cluster analysis; Manas River
分类号:
X142
摘要:
通过Piper三线图示法、系统聚类等方法对玛纳斯河中下游28个地表水样品离子化学成分进行了分析，研究了玛纳斯河流域冲积平原的水化学分布特征及影响因素。结果表明：1）研究区水体样品pH值差异较小，但矿化度和各离子组成的差别明显，从淡水到高盐矿化度水均有分布。阳离子浓度Na+ > Ca2+ > Mg2+ > K+；阴离子浓度SO42- > Cl- > HCO3-。水样中K+和HCO3-的变异系数相对较小，Cl-和Na+变异系数最大。2）玛纳斯河流域冲积平原地区水化学类型主要有Ca2+-HCO3-，Na+-SO42-，Ca2+-SO42-，Na+-Cl-四种。其中Ca2+-HCO3-型占总水样的78.6%，其中仅有3个样品为Na+-SO42-型，2个样品为Ca2+-SO42-型，1个样品为Na+-Cl-型。聚类分析的结果表明玛纳斯河流域地表水化学特征表现出较为明显的空间分异性。总体来看，玛纳斯流域地表水中部分水样的水化学类型改变，主要是由于水体蒸发强度的差异以及玛纳斯河流域土壤中盐分离子被淋洗，增加了水体中的盐分离子含量从而导致水化学类型呈现出差异性。
Abstract:
Hydrochemical investigations of 28 surface water samples were conducted in middle and lower reaches of Manas River Basin. In this study, hierarchical clustering method and PIPER diagram were used to anayze the hydrochemical characteristics and its influence factors. The result shows that: 1) the pH of water samples in the study area has little difference, but the differences in total dissolved solids (TDS) and major-ion (Mg2+, Ca2+, Na+, K+, SO42-, HCO3- and Cl-) composition were obviously signifcant. In this study area, the fresh water and high salinity water distribute here. The order of the average concentrations of major cations in Manas River Basin is Na+ > Ca2+ > Mg2+ > K+, and the sequence of concentrations for major anions is SO42- > Cl- > HCO3-. The coefficients of variation of K+ and HCO3- are relative small in water samples, otherwise, the ions (Cl- and Na+) have the biggest values among the seven major ions; 2) the surface water of the Manas River Basin belongs to four hydrochemical types (Ca2+-HCO3-, Na+-SO42-, Ca2+-SO42-, Na+-Cl-). The Ca2+-HCO3- type accounts for 78.6% of the total samples, however, there are three water samples with Na+-SO42- type, two samples with Ca2+-SO42- type, and only one sample with Na+-Cl- type in this area. The result of hierarchical clustering analysis showed that chemical characteristics in surface water had obvious spatial variability. Overall, the changes of hydrochemical characteristics of Manas River Basin are mainly due to spatial differences of water evaporation and soil salinity leaching into surface water bodies, which induced the differences in hydrochemical types of surface waters.

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备注/Memo

收稿日期:2014-06-08;改回日期:2014-07-24。
基金项目:中国科学院西部之光（XBBS201106）；国家自然科学基金（41471173）
作者简介:夏梦(1990-),女(回族),新疆乌鲁木齐人,硕士研究生,从事干旱区湖泊资源与环境研究。E-mail:xiamgyh@sina.com
通讯作者:吉力力·阿不都外力(1964-),男(维吾尔族),新疆拜城县人,研究员,博士,主要从事地理生态学方面的研究。E-mail:jilil@ms.xjb.ac.cn

更新日期/Last Update: 1900-01-01