塔里木盆地克里雅河流域水化学特征及成因分析

纳麦提·托合提; 张峰

doi:10.13568/j.cnki.651094.651316.2020.03.20.0002

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塔里木盆地克里雅河流域水化学特征及成因分析

更新时间：2026-01-21

- 塔里木盆地克里雅河流域水化学特征及成因分析
- Journal of Xinjiang University (Natural Science Edition in Chinese and English) Vol. 38, Issue 2, Pages: 220-228(2021)
- 作者机构：
  
  1. 喀什大学生命与地理科学学院
  2. 新疆大学绿洲生态教育部重点实验室
- 作者简介：
- 基金信息：
- DOI：10.13568/j.cnki.651094.651316.2020.03.20.0002
  CLC： P342
- Published：2021
- 稿件说明：
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[1]纳麦提·托合提,张峰.塔里木盆地克里雅河流域水化学特征及成因分析[J].新疆大学学报(自然科学版)(中英文),2021,38(02):220-228.
[1]纳麦提·托合提,张峰.塔里木盆地克里雅河流域水化学特征及成因分析[J].新疆大学学报(自然科学版)(中英文),2021,38(02):220-228. DOI： 10.13568/j.cnki.651094.651316.2020.03.20.0002.

DOI：10.13568/j.cnki.651094.651316.2020.03.20.0002.

摘要

为探讨克里雅河流域的水化学特征及其成因

于2014年夏季与2015年冬季实地采集了21个河水、8个地下水和1个高山湖水样品

并对样品的Na+、K+、Mg2+、Ca2+、HCO3~-、CI~-、SO42-、NO3~-等主要阴阳离子和相关的pH值、电导率、TDS值、硬度等因素进行测定

然后分析了流域水化学的时空变化特征、水化学类型以及水化学的成因.结果显示:(1)随着海拔高度的降低

硬度、TDS值和主要离子含量明显增高.(2)夏季除了pH值外

其他参数和主要离子含量均低于冬季

或因夏季径流量大

河水对化学离子的稀释作用较冬季显著而引起.(3)夏季和冬季中上游河水中的阳离子浓度分别为Ca2+>Na~++K+>Mg2+与Na~++K+>Ca2+>Mg2+

阴离子浓度分别为HCO3~->SO42->CI-与HCO3~->CI->SO42-

水化学类型分别为HCO3~--SO42--Ca2+-Na+型和HCO3~--CI~--SO42--Na+-Ca2+型;冬季下游河水中的阴离子和阳离子浓度分别CI->SO42->HCO3~-与Na~++K+>Mg2+>Ca2+

水化学类型为CI~--SO42--Na+-Mg2+型;地下水阴、阳离子浓度分别CI->HCO3~->SO42-与Na~++K+>Mg2+>Ca2+

水化学类型为CI~--SO42--HCO3~--Na+-Mg2+型.(4)中游、上游河水水化学成分受岩石风化作用的控制为主

而地下水和下游河水则以塔里木盆地极端干旱气候的蒸发-结晶作用影响为主.(5)于田绿洲的地下水与河水的水化学特征均表现出来自人类活动的影响.

Abstract

To understand hydrochemical characteristics and its origin of the Keriya River Basin

we conducted field investigation in during summer of 2014 and winter of 2015

and collected 21 surface water samples

8 groundwater samples and 1 high mountain lake water samples.The samples contents of Na+

K+

Mg2+

Ca2+

HCO3~-

CI~-

SO42-

NO3~-and the pH values

conductivity

total dissolved solids(TDS)

hardness were measured.The spatial and temporal variation of water quality

hydrochemical types

origin and its causes were analyzed.The results showed that:(1) Hardness

TDS

major ion contents obviously increased with the decreasing of altitude.(2) Due to the large runoff in summer

the river water has a significant dilution effect on chemical ions.Except the pH values

other parameters and main ion contents are lower than those in winter.(3) The cations in the upper and middle reaches of the river in summer and winter are Ca2+>Na++K+>Mg2+and Na++K+>Ca2+>Mg2+

respectively.The anions are HCO3~->SO42->CI~-and HCO3~->CI~->SO42-

respectively.Hydrochemical types are HCO3~--SO42--Ca2+-Na~+type and HCO3~--CI~--SO4~--Na+-Ca2+type

respectively.In winter

anions and cations in the lower reaches of the river are CI~->SO42->HCO3~-and Na~++K+>Mg2+>Ca2+

respectively.Hydrochemical type is CI~--SO42--Na+-Mg2+ type.In the groundwater

the anions and cations are CI~->HCO3~->SO42- and Na~++K+>Mg2+>Ca2+

respectively.Hydrochemical type is CI~--SO42--HCO3~--Na+-Mg2+ type.(4) Hydrochemical compositions of middle and upper reaches are dominated by rock weathering

but Evaporation and crystallization from the extreme arid climate in the Tarim Basin control the chemical compositions of groundwater and downstream water in the Keriya River.(5)Human agricultural production activities such as pesticides

urea caused groundwater pollution in the Keriya Oasis.

关键词

Keywords

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