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基于氢氧稳定同位素的武汉北部新城地表水-地下水转换关系研究

杨艳林, 靖晶, 赵永波, 何军, 杜小锋. 2022. 基于氢氧稳定同位素的武汉北部新城地表水-地下水转换关系研究[J]. 中国地质, 49(3): 706-715. doi: 10.12029/gc20220303
引用本文: 杨艳林, 靖晶, 赵永波, 何军, 杜小锋. 2022. 基于氢氧稳定同位素的武汉北部新城地表水-地下水转换关系研究[J]. 中国地质, 49(3): 706-715. doi: 10.12029/gc20220303
YANG Yanlin, JING Jing, ZHAO Yongbo, HE Jun, DU Xiaofeng. 2022. Conversion relationship between surface water and groundwater based on stable isotopes of D and 18O of new town in the northern Wuhan, Hubei[J]. Geology in China, 49(3): 706-715. doi: 10.12029/gc20220303
Citation: YANG Yanlin, JING Jing, ZHAO Yongbo, HE Jun, DU Xiaofeng. 2022. Conversion relationship between surface water and groundwater based on stable isotopes of D and 18O of new town in the northern Wuhan, Hubei[J]. Geology in China, 49(3): 706-715. doi: 10.12029/gc20220303

基于氢氧稳定同位素的武汉北部新城地表水-地下水转换关系研究

  • 基金项目:
    中国地质调查局项目"武汉多要素城市地质调查(DD20190282)"和"武汉滨江城市地质安全调查评价(DD20221743)"资助
详细信息
    作者简介: 杨艳林, 男, 1984年生, 高级工程师, 主要从事水工环地质调查研究; E-mail: yangyanlin@mail.cgs.gov.cn
    通讯作者: 何军, 男, 1984年生, 高级工程师, 主要从事水工环地质调查研究; E-mail: 176041779@qq.com
  • 中图分类号: P592

Conversion relationship between surface water and groundwater based on stable isotopes of D and 18O of new town in the northern Wuhan, Hubei

  • Fund Project: Supported by the project of China Geological Survey (No.DD20190282, No.DD20221743)
More Information
    Author Bio: YANG Yanlin, male, born in 1984, senior engineer, engaged in hydro-environmental geological survey; E-mail: yangyanlinjida@gmail.com .
    Corresponding author: HE Jun, male, born in 1984, senior engineer, engaged in hydro-environmental geological survey; E-mail: 176041779@qq.com
  • 研究目的

    揭示武汉北部新城地表水、地下水的氢氧稳定同位素特征及其相互作用。

    研究方法

    2019年,采集、测定了降水样7件、河水样6件、水库样14件、民井样98件、泉水样3件和钻孔样11件,并收集到武汉站1986—1998年的监测数据50件,以空间分析和流域分析为基础,氢氧稳定同位素分析为手段。

    研究结果

    (1)武汉降水氢氧同位素随季节变化,并表现出“降雨效应”明显、“温度效应”不明显的特点;(2)地表水在枯水期受到强烈的蒸散发,表现出一定的“地貌效应”与“干支流效应”的特征;(3)民井、泉和钻孔等地下水均源于大气降水,表现出“含水层埋深效应”与“山区平原效应”的特点;(4)枯水期,界河流域中界河获得了上游水库和地下水的补给,夏家寺水库流域中夏家寺水库得到了地下水补给。

    结论

    氢氧同位素能显著提高武汉北部新城地表水-地下水相互转换规律的认识。

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  • 图 1  研究区地形地貌及采样点分布

    Figure 1. 

    图 2  武汉地区月降水量、气温、氘氧同位素变化特征

    Figure 2. 

    图 3  降水氘氧同位素的季节变化

    Figure 3. 

    图 4  河流、水库中δ18O、δD同位素及氘过剩值

    Figure 4. 

    图 5  河流、水库样中δ18O、δD同位素样的空间分布

    Figure 5. 

    图 6  井、泉、钻孔样中δ18O-δD同位素及氘过剩值

    Figure 6. 

    图 7  民井、泉和钻孔等采样点的空间分布

    Figure 7. 

    图 8  地表水、地下水中δ18O-δD关系

    Figure 8. 

    图 9  南部流域中δ18O-δD空间分布

    Figure 9. 

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出版历程
收稿日期:  2021-01-18
修回日期:  2022-05-09
刊出日期:  2022-06-25

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