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穆兴平原北部地下水年龄及更新性

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苏晨, 程中双, 郑昭贤, 陈宗宇. 2019. 穆兴平原北部地下水年龄及更新性[J]. 中国地质, 46(2): 328-336. doi: 10.12029/gc20190209
引用本文: 苏晨, 程中双, 郑昭贤, 陈宗宇. 2019. 穆兴平原北部地下水年龄及更新性[J]. 中国地质, 46(2): 328-336. doi: 10.12029/gc20190209
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SU Chen, CHENG Zhongshuang, ZHENG Zhaoxian, CHEN Zongyu. 2019. Groundwater age and renewability in the north of Muling-Xingkai plain[J]. Geology in China, 46(2): 328-336. doi: 10.12029/gc20190209
Citation: SU Chen, CHENG Zhongshuang, ZHENG Zhaoxian, CHEN Zongyu. 2019. Groundwater age and renewability in the north of Muling-Xingkai plain[J]. Geology in China, 46(2): 328-336. doi: 10.12029/gc20190209
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穆兴平原北部地下水年龄及更新性

  • 1.

    中国地质科学院水文地质环境地质研究所

  • 2.

    自然资源部地下水科学与工程重点实验室

  • 基金项目:
    中国地质调查局地质调查项目(DD20160311)和国家自然科学基金(41702283)资助
详细信息
    作者简介: 苏晨, 1985生, 男, 硕士, 助理研究员, 主要从事地下水资源评价研究; E-mail:sc.1219@163.com
    通讯作者: 程中双, 1989年生, 男, 硕士, 研究实习员, 主要从水同位素水文学研究; E-mail:zshuangcheng@hotmail.com

  • 中图分类号: P641

Groundwater age and renewability in the north of Muling-Xingkai plain

  • 1.

    Institute of Hydrogeology & Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, 050061, Hebei, China

  • 2.

    Key Laboratory of Groundwater Science and Engineering, Ministry of Natural Resource, Shijiazhuang, 050061, Hebei, China

  • Fund Project: Supported by China Geological Survey Project (No. DD20160311), National Natural Science Foundation of China (No.41702283)
More Information
    Author Bio: SU Chen, male, born in 1985, associate researcher, engages in groundwater resource assessment; E-mail: sc.1219@163.com .
    Corresponding author: CHENG Zhongshuang, male, born in 1989, assistant researcher, engages in the study of isotope hydrology; E-mail: zshuangcheng@hotmail.com

    摘要

  • 地下水年龄结构是了解一个地区地下水资源开采可持续性的重要基础。穆兴平原地下水开采量增加以及地下水环境恶化，对该地区可持续发展有一定制约，为此在2016年采集CFCs样品31组和3H样品60组，估算了研究区地下水年龄。结果表明，穆兴平原北部地下水年龄为21年到大于65年，由西北部和穆棱河向平原中部及乌苏里江逐渐变老，更新性变差，主要受到大气降水和地表河水补给，但是由于地表覆盖一层黏性土，地下水中缺失小于10年的水；不同井深样品中二者及NO3-浓度的变化，表明在60 m以上地下水的防污性能较差，而在100 m以下则较好，饮用水源井深需超过100 m。

    The age structure of aquifer is an important basis for understanding the sustainability of groundwater exploitation. Increasing groundwater pumping with deteriorate groundwater environment in the Muling-Xingkai Plain (MXP) has restricted to some extent the sustainable development of the region.31 groups of CFCs and 60 groups of 3H samples were collected to delineate groundwater flow systems. Estimated groundwater age ranges from 21 years to more than 70 years in the northern part of the MXP.Younger water occurs in northwest piedmont and hilly areas as well as Muling River, while older water occurs in the central part of the plain and the Wusuli River. This reflects long flow paths associated with regional flow. Although groundwater is mainly recharged by rain and surface water, ground water younger than 10 years was not found for the unsaturated zone consisting of silty clay. The variations of 3H and CFCs combined NO3- with wells depth indicate that the aquifer sensitivity of groundwater system above 60m is low and it is high below 100m. Wells for drinking water should exceed 100m.

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  • 图 1  穆兴平原北部地下水采样点分布

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  虎林大气降水氚特征(1952—2016年)

    Figure 2. 

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    图 3  穆兴平原北部地下水年龄CFCs输出曲线(a)、氚浓度输出曲线(b)

    Figure 3. 

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    图 4  穆兴平原北部地下水年龄分布特征(井深 < 60 m)

    Figure 4. 

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    图 5  穆兴平原北部3H、NO3-和CFCs含量水井深变化特征

    Figure 5. 

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    表 1  穆兴平原北部地下水分析结果

    Table 1.  Analytical results for groundwater samples in the north of MXP

    下载: 导出CSV

    表 2  不同示踪剂地下水年龄估算分布频率

    Table 2.  The statistical characteristics of calculated groundwater age by different tracers

    下载: 导出CSV
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收稿日期:  2018-09-04
修回日期:  2019-03-15
刊出日期:  2019-04-25

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