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[1]麦麦提吐尔逊·艾则孜,米热古丽·艾尼瓦尔,麦尔丹·阿不拉,等.新疆焉耆盆地地下水地球化学特征[J].水土保持研究,2016,23(04):263-268.
　Mamattursun·Eziz,Mihrigul·Anwar,Mardan·Abla,et al.Geochemical Characteristics of Groundwater in Yanqi Basin, Xinjiang[J].Research of Soil and Water Conservation,2016,23(04):263-268.

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新疆焉耆盆地地下水地球化学特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 23 期数: 2016年04期页码: 263-268 栏目: 出版日期: 2016-08-28

Title:: Geochemical Characteristics of Groundwater in Yanqi Basin, Xinjiang

作者:: 麦麦提吐尔逊·艾则孜^1,2, 米热古丽·艾尼瓦尔³, 麦尔丹·阿不拉², 古丽孜巴·艾尼瓦尔²; 1. 新疆师范大学新疆干旱区湖泊环境与资源重点实验室, 乌鲁木齐 830054;
2. 新疆师范大学地理科学与旅游学院, 乌鲁木齐 830054;
3. 新疆大学资源与环境科学学院, 乌鲁木齐 830046

Author(s):: Mamattursun·Eziz^1,2, Mihrigul·Anwar³, Mardan·Abla², Gulziba·Anwar²; 1. Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Xinjiang Normal University, Urumqi 830054, China;
2. College of Geographical Science and Tourism, Xinjiang Normal University, Urumqi 830054, China;
3. College of Resources and Environmental Sciences, Xinjiang University, Urumqi 830046, China

关键词:: 地下水; 地球化学特征; 统计分析; 焉耆盆地

Keywords:: groundwater; geochemical characteristics; statistical analysis; Yanqi Basin

分类号:: P592;P641.3

摘要:: 采用相关分析法与主成分分析法，研究了新疆焉耆盆地地下水地球化学特征。结果表明：从开都河上游向盆地中部灌溉区，地下水矿化度由0.21 g/L增加到37.45 g/L，地下水水化学类型依次为HCO₃型、HCO₃-SO₄型、SO₄-Cl型以及Cl-SO₄型。研究区各时期地下水阳离子主要以Mg²⁺与Ca²⁺为主，阴离子主要以SO₄^2-与Cl^-为主。地下水矿化度，电导率，Mg²⁺，Ca²⁺，SO₄^2-与Cl^-均呈现强烈的空间变异性，pH值呈现非常弱的空间变异性。草地的地下水矿化度最高，荒漠地下水矿化度最低。地下水矿化度与主要离子含量从高到低依次为：草地、耕地、林地、荒漠。研究区地下水矿化度的大小与Mg²⁺，Ca²⁺，SO₄^2-，Cl^-，HCO₃^-等离子含量水平的高低密切相关。

Abstract:: The Geochemical characteristics of groundwater in Yanqi Basin, Xinjiang, were studied based on correlation analysis and principal component analysis. Results of this study indicated that groundwater salinity increased from 0.21 g/L to 37.45 g/L from the upper reaches of Kaidu River to the irrigation area in the middle of the basin, and hydrochemical types of groundwater gradually changed from HCO₃ type, HCO₃-SO₄ type, SO₄-Cl type to Cl-SO₄ type; cations were mainly Mg²⁺ and Ca²⁺ while anions were mainly SO₄^2- and Cl^- in the study area; groundwater salinity, EC, Mg²⁺, Ca²⁺, SO₄^2- and Cl^- presented strongly spatial variation while pH demonstrated very slightly spatial variation; groundwater salinity of the grassland was the maximum while groundwater salinity of Gobi was the minimum. The abundance of salinity and main ion contents of groundwater for different land use types decreased in the order:grassland > farmland > forest land > Gobi. Groundwater salinity has the significant positive correlation with the concentrations of Mg²⁺, Ca²⁺, SO₄^2-, Cl^- and HCO₃^-.

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备注/Memo

收稿日期:2015-08-06;改回日期:2015-08-22。
基金项目:新疆维吾尔自治区高等学校科研计划项目（XJEDU2014S037）；国家自然科学基金资助项目（41201032，U1138302）
作者简介:麦麦提吐尔逊·艾则孜(1981-),男(维吾尔族),新疆喀什人,副教授,博士,硕士生导师,主要从事干旱区水资源与生态环境演变研究。E-mail:oasiseco@126.com

更新日期/Last Update: 1900-01-01