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新疆三工河流域厚层包气带区地下水垂向补给量的厘定

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孙芳强, 尹立河, 王晓勇, 马洪云, 张俊, 董佳秋, 贺帅军. 2017. 新疆三工河流域厚层包气带区地下水垂向补给量的厘定[J]. 中国地质, 44(5): 913-923. doi: 10.12029/gc20170506
引用本文: 孙芳强, 尹立河, 王晓勇, 马洪云, 张俊, 董佳秋, 贺帅军. 2017. 新疆三工河流域厚层包气带区地下水垂向补给量的厘定[J]. 中国地质, 44(5): 913-923. doi: 10.12029/gc20170506
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SUN Fangqiang, YIN Lihe, WANG Xiaoyong, MA Hongyun, ZHANG Jun, DONG Jiaqiu, HE Shuaijun. 2017. Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin, Xinjiang[J]. Geology in China, 44(5): 913-923. doi: 10.12029/gc20170506
Citation: SUN Fangqiang, YIN Lihe, WANG Xiaoyong, MA Hongyun, ZHANG Jun, DONG Jiaqiu, HE Shuaijun. 2017. Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin, Xinjiang[J]. Geology in China, 44(5): 913-923. doi: 10.12029/gc20170506
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新疆三工河流域厚层包气带区地下水垂向补给量的厘定

  • 中国地质调查局干旱-半干旱区地下水与生态重点实验室, 陕西 西安 710054;中国地质调查局西安地质调查中心, 陕西 西安 710054

  • 基金项目:
    国土资源部公益性行业科研专项（201511047）资助
详细信息
    作者简介: 孙芳强, 男, 1975, 博士, 高级工程师, 主要从事水文地质与环境地质方面研究; E-mail:sunfq2003@126.com
    通讯作者: 王晓勇, 男, 1977, 硕士, 高级工程师, 主要从事水文水资源研究; E-mail:Wxiaoyong@cgs.cn

  • 中图分类号: P641

Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin, Xinjiang

  • Arid and Semi-arid Region Ground Water and Ecology Key Laboratory, Xi'an 710054, Shaanxi, China; Xi'an Center, China Geological Survey, Xi'an 710054, Shaanxi, China

  • Fund Project: Supported by Ministry of Land and Resources Nonprofit Industry Research (No. 201511047)
More Information
    Author Bio: SUN Fangqiang, male, born in 1975, doctor, senior engineer, majors in hydrogeology and environmental geology; E-mail: sunfq2003@126.com .
    Corresponding author: WANG Xiaoyong, Wxiaoyong@cgs.cn

    摘要

  • 通过对荒漠区荒地、绿洲区耕地及摞荒地厚层包气带剖面土壤水的含水率、易溶盐离子及稳定同位素（δD、δ18O）的测定和分析，对厚层包气带区土壤水的补给来源及地下水的垂向补给量进行了厘定。结果表明：荒漠区荒地、绿洲区耕地与摞荒地土壤含水率、易溶盐中氯离子与土壤水氢氧同位素在垂向上均呈现旋回变化，每个旋回经历了一次新水入渗补给的过程。绿洲区土壤水与荒漠区土壤补给水中的δD值为-124.10‰~-94.44‰，土壤补给水来源于冬季大气降水或降雪的入渗补给。绿洲内耕地区、摞荒地区及荒漠区地下水垂向入渗补给量分别为1.29~5.53 mm/a、0.52~1.85 mm/a及0.03~0.08 mm/a。

    The authors investigated the origin of soil water and vertical infiltration recharge of groundwater in thick unsaturated zone of arid area based on the characteristics of water content, stable isotopes (δD and δ18O) of soil water and soluble salt ions in soil. The results indicate that the vertical profiles of stable isotopes of soil water depict a cyclic variation as well as water content and chloride of soluble salt ions for the uncultivated regions in desert and cultivated and uncultivated regions in oasis. Each cyclic variation indicates one infiltration event that has involved mixture of newly infiltrated water and existing soil water. The lower value of Cl- content is consistent with the depleted values of δD in each cycle; δD of soil water varies from -124.10‰ to -94.44‰, which suggests that soil water originates from precipitation or snow in winter in desert and in oasis. The vertical infiltration recharge varies in the ranges of 1.29~5.53mm/a, 0.52~1.85mm/a and 0.03~0.08mm/a respectively for the cultivated and uncultivated regions in oasis and the uncultivated regions in desert.

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  • 图 1  各采样剖面分布图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  剖面含水量随深度的变化

    Figure 2. 

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    图 3  剖面Cl-随深度的变化

    Figure 3. 

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    图 4  土壤水中δD、δ18O在垂向剖面上的分布

    Figure 4. 

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    图 5  各剖面δD值及Cl-含量旋回特征

    Figure 5. 

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    图 6  各剖面补给水中δD与δ18O同位素关系

    Figure 6. 

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    图 7  新疆乌鲁木齐地区氢氧同位素年内变化

    Figure 7. 

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    表 1  各采样点土地利用及剖面采样特征

    Table 1.  Land use practices and distribution of samples in different profiles

    下载: 导出CSV

    表 2  各剖面旋回段中补给水δD值及Cl-含量统计

    Table 2.  Statistic characteristics of δD and Cl- for recharge water in different profiles

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    表 3  各剖面旋回段的垂向入渗补给量

    Table 3.  Vertical infiltration recharge in different profiles

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收稿日期:  2017-09-19
修回日期:  2017-10-09
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