PDF Download

[1]WU Lina,SUN Congjian,HE Qiang,et al.Analysis of Temporal and Spatial Variation of Hydrochemical Characteristics of the Typical Inland River in the Middle of Tianshan Mountains[J].Research of Soil and Water Conservation,2017,24(05):149-156.

Copy

Analysis of Temporal and Spatial Variation of Hydrochemical Characteristics of the Typical Inland River in the Middle of Tianshan Mountains

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 24 Number of periods: 2017 05 Page number: 149-156 Column: Public date: 2017-10-28

Title:: Analysis of Temporal and Spatial Variation of Hydrochemical Characteristics of the Typical Inland River in the Middle of Tianshan Mountains

Author(s):: WU Lina¹, SUN Congjian^1,2, HE Qiang¹, CHEN Wei¹, ZHANG Yongqing¹; 1. School of Geographical Science, Shanxi Normal University, Linfen, Shanxi 041000, China;
2. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China

Keywords:: Urumqi River; temporal and spatial distribution; Piper; gibbs; control factors

CLC:: S153;P332.7

DOI:: -

Abstract:: Based on the results of water chemistry of six stations in Urumqi River Basin in different seasons of 2011—2013, we analyzed the temporal and spatial characteristics of surface water chemistry in Urumqi River Basin by using water chemistry analysis method and SPSS statistical software in combination with hydrological data. The results show that: (1) the TDS of Urumqi River is lower and the water is slightly alkaline; (2) water hydrochemical characteristics varied over the years, TDS is lower in summer than that in early spring, early summer and autumn; (3) the control ions of the surface water are HCO₃^-, Ca²⁺, SO₄^2-, the icon concentrations decrease in the order: HCO₃^- > Ca²⁺ > SO₄^2- > Cl^- > Na⁺ > Mg²⁺ > K⁺ > CO₃^2-; the main ions changed with years: Ca²⁺ and HCO₃ are the main ions in dry season; while Ca²⁺, HCO₃ and SO₄^2- start to dominate in wet season for the dilution of abundant water; (4) the SO₄^2- concentration suddenly rises in site 1 to site 2 due to the release of sulfuric acid and chloric acid in the gypsum horizon of the river segment; (5) the conclusion indicates that water-rock interaction movement is the main factor controlling the surface water hydrochemical properties.

References:: [1] 夏学齐,杨忠芳,王亚平,等.长江水系河水主要离子化学特征[J].地学前缘,2008,15(5):194-202.
[2] 叶宏萌,袁旭音,葛敏霞,等.太湖北部流域水化学特征及其控制因素[J].生态环境学报,2010,19(1):23-27.
[3] 蒲焘,何元庆,朱国锋,等.丽江盆地地表水—地下水的水化学特征及其控制因素[J].环境科学,2012,33(1):48-54.
[4] 唐玺雯,吴锦奎,薛丽洋,等.锡林河流域地表水化学主离子特征及控制因素[J].环境科学,2014,35(1):131-142.
[5] 周嘉欣,丁永建,曾国雄,等.疏勒河上游地表水水化学主离子特征及其控制因素[J].环境科学,2014,35,(9):3315-3324.
[6] 蒋保刚,闫正,宋献方,等.汉江上游金水河流域河水的化学特征[J].环境化学,2013,32(6):980-986.
[7] 钱程,武雄.盐池内流区地下水水化学特征及其形成作用[J].干旱区资源与环境,2016,3,30(3):169-175.
[8] 乐嘉祥,王德春.中国河流水化学特征[J].地理学报,1963,29(I):2-12.
[9] 郜银梁,陈军锋,张成才,等.黑河中游灌溉区水化学空间变异特征研究[J].干旱区地理,2011,34(4):575-583.
[10] 殷秀兰,凤蔚,王瑞久,等.新疆乌鲁木齐河流域北部平原区水文地球化学[J].地球学报,2015,36(1):77-84.
[11] 刘友存,崔雪丽,郝永红,等.天山乌鲁木齐河上游径流极值变化分析研究[J].冰川冻土,2013,35(5):1248-1258.
[12] Sun Congjian, Li Xingong, Chen Yaning, et al. Climate Change and Runoff Response in an arid Mountain Watershed of the Western Kunlun Mountains[J]. Hydrological Sciences Journal, 2016， DOI:10.1080/02626667.2016.1224885.
[13] 卢颖,郭建强.基于多元统计方法的张掖盆地地下水化学特征分析[J].干旱区资源与环境,2016，30(5):129-134.
[14] 魏忠义.塔里木盆地地表水化学特征及在人类活动影响下的变化[J].干旱区资源与环境,1994,8(2):23-30.
[15] 冯芳,冯起,李忠勤,等.天山乌鲁木齐河流域山区水化学特征分析[J].自然资源学报,2014,29(1):143-155.
[16] 冯芳,冯起,刘贤德,等.天山乌鲁木齐河源1号冰川融水径流水化学特征研究[J].冰川冻土,2014,36(1):183-191.
[17] 冯芳,李忠勤.天山乌鲁木齐河源区径流水化学特征及影响因素分析[J].资源科学,2011,33(12):2238-2247.
[18] Sun congjian, Chen yaning, Li xingong, et al. Analysis on the streamflow components of the Typical inland River, Northwest China[J]. Hydrological Sciences Journal,2014，61(5):970-981. DOI:10.1080/02626667.2014.1000914.
[19] 高业新,王贵玲,刘花台,等.石羊河流域的水化学特征及其地表水与地下水的相互转换[J].干旱区资源与环境,2006,20(6):84-88.
[20] 石维栋,郭建强,张森琦,等.贵德盆地高氟、高砷地下热水分布及水化学特征[J].水文地质工程地质,2010,27(2):36-41.
[21] 毛炜峄,樊静,沈永平,等.近50 a来新疆区域与天山典型流域极端洪水变化特征及其对气候变化的响应[J].冰川冻土,2012,34(5):1037-1046.
[22] 崔玉环,叶柏生,王杰,等.乌鲁木齐河源1号冰川水文断面不同时间尺度径流估算[J].干旱区资源与环境,2013,27(7):119-126.
[23] 吴素芬,刘志辉,韩萍,等.气候变化对乌鲁木齐河流域水资源的影响[J]冰川冻土,2006,28(5):703-706.
[24] 刘光琇,安黎哲,陈桂琛,等.乌鲁木齐河上游植被与环境关系研究[M].兰州:兰州大学出版社,2004.
[25] Meybeck M. Concentrations des eaux fluviales en elements majeurs et apports en solution aux oceans[J]. Rev. Geol. Dyn. Geogr. Phys., 1979, 21(3): 215-246.
[26] Wilhams M W, Yang D, Liu F, et al. Controls on the major ion chemistry of the ürümqi River, Tian Shan, People’s Republic of China[J]. Journal of Hydrology, 1995,172(1/4):209-229.
[27] 谢协忠.水分析化学[M].2版.北京:中国电力出版社,2014.
[28] Kattan Z. Chemical and isotopic compositions of the Euphrates River water, Syria[Z]. Monitoring isotopes in rivers: creation of the global network of isotopes in rivers (GNIR), 2012.
[29] 刘永林,雒昆利,李玲,等.新疆天然水化学特征区域分异及其地质成因[J].地理科学,2016,36(5):794-802.
[30] 盛文坤,朱守森.天山乌鲁木齐河中上游的水化学特征[J].环境科学,1987,8(4):12-18.
[31] Sun Congjian, Chen Yaning, Li Weihong, et al. Isotopic time-series partitioning of streamflow components under regional climate change in the Urumqi River, northwest China[J]. Hydrological Sciences Journal, 2015,61(8)：1443-1459, DOI:10.1080/02626667.2015.1031757.
[32] Gibbs JR.Mechanisms Controlling World Water Chemistry[J].Science, 1970,170(3962):1088-1090.

Similar References:

Memo

Last Update: 1900-01-01