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海河流域地下水资源特征和开发利用潜力

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文章导航 > 中国地质 > 2021 > 48(4): 1032-1051

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杨会峰, 孟瑞芳, 李文鹏, 李泽岩, 支传顺, 包锡麟, 李长青, 柳富田, 吴海平, 任宇. 2021. 海河流域地下水资源特征和开发利用潜力[J]. 中国地质, 48(4): 1032-1051. doi: 10.12029/gc20210404
引用本文: 杨会峰, 孟瑞芳, 李文鹏, 李泽岩, 支传顺, 包锡麟, 李长青, 柳富田, 吴海平, 任宇. 2021. 海河流域地下水资源特征和开发利用潜力[J]. 中国地质, 48(4): 1032-1051. doi: 10.12029/gc20210404
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YANG Huifeng, MENG Ruifang, LI Wenpeng, Li Zeyan, ZHI Chuanshun, BAO Xilin, LI Changqing, LIU Futian, WU Haiping, REN Yu. 2021. Groundwater resources of the Haihe River Basin and its development potential[J]. Geology in China, 48(4): 1032-1051. doi: 10.12029/gc20210404
Citation: YANG Huifeng, MENG Ruifang, LI Wenpeng, Li Zeyan, ZHI Chuanshun, BAO Xilin, LI Changqing, LIU Futian, WU Haiping, REN Yu. 2021. Groundwater resources of the Haihe River Basin and its development potential[J]. Geology in China, 48(4): 1032-1051. doi: 10.12029/gc20210404
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海河流域地下水资源特征和开发利用潜力

  • 1.

    中国地质科学院水文地质环境地质研究所, 河北 石家庄 050061

  • 2.

    京津冀平原地下水与地面沉降国家野外科学观测研究站, 河北 石家庄 050061

  • 3.

    中国地质环境监测院, 北京 100081

  • 4.

    天津地质调查中心, 天津 300170

  • 5.

    中国国土勘测规划院, 北京 100035

  • 基金项目:
    中国地质调查局项目（DD20190336，DD20160230）及自然资源部自然资源专项调查项目（B202012）联合资助
详细信息
    作者简介: 杨会峰, 男, 1977年生, 博士, 高级工程师, 主要从事水文地质与水资源研究工作; E-mail: yanghuifeng@mail.cgs.gov.cn
    通讯作者: 孟瑞芳, 男, 1988年生, 硕士, 助理研究员, 主要从事水资源研究工作; E-mail: mengruifang@mail.cgs.gov.cn

  • 中图分类号: P641

Groundwater resources of the Haihe River Basin and its development potential

  • 1.

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

  • 2.

    National Observation and Research Station on Groundwater and Land Subsidence in Beijing-Tianjin-Hebei Plain, Shijiazhuang 050061, Hebei, China

  • 3.

    Chinese Institute of Geo-Environment Monitoring, Beijing 100081, China

  • 4.

    Tianjin Geological Survey Center, Tianjin 300170, China

  • 5.

    China National Land Survey and Planning Institute, Beijing 100035, China

  • Fund Project: Supported by the project of China Geological Survey (No.DD20190336, No.DD20160230), special investigation project of natural resources of Ministry of Natural Resources (No.B202012)
More Information
    Author Bio: YANG Huifeng, male, born in 1977, doctor, senior engineer, engaged in hydrogeology and water resources; E-mail: yanghuifeng@mail.cgs.gov.cn .
    Corresponding author: Meng Ruifang, male, born in 1988, master, assistant researcher, engaged in the research of water resources; E-mail: mengruifang@mail.cgs.gov.cn

    摘要

  • 海河流域水资源严重短缺，地下水长期超采是制约社会经济可持续发展的主要瓶颈。开展流域地下水资源及开发利用潜力研究，对支撑服务地下水超采治理、地下水资源可持续利用和生态环境保护都具有重要意义。经系统评价，海河流域天然资源量252.99×108 m3，生态水位约束条件下的浅层地下水开采资源量172.98×108 m3，可更新的深层水可利用量4.68×108 m3。海河流域山区地下水质量总体较好，Ⅰ~Ⅲ类水占比40.83%，平原区浅层地下水质量较差，Ⅰ~Ⅲ类水占比14.10%，深层地下水质量优于浅层地下水，Ⅰ~Ⅳ类水占比74.25%。海河流域山区地下水开采潜力总体较小，燕山和太行山北部山区，地下水资源禀赋较差，基本无开采潜力，太行中部山区地下水开采程度较高，无开采潜力或开采潜力较小，太行南部山区地下水资源禀赋良好，开采潜力较大；平原区浅层地下水在不同水文地质单元开采潜力差异较大，山前平原浅层地下水长期超采形成大范围降落漏斗，无开采潜力或潜力较小，中东部平原浅层地下水资源禀赋较差，以微咸水为主，开采潜力较小，山东省鲁北平原区浅层地下水开采程度较低，聊城—德州一带开采潜力较大；雄安新区地下水总体无开采潜力。平原区深层地下水基本无开采潜力。

    There is serious shortage of water resources in the Haihe River Basin, and long-term over exploitation of groundwater is the bottleneck for the sustainable social and economical development. Therefore, it is of great significance to carry out study on groundwater resources and utilization potential of the river basin, for dealing with the groundwater overexploitation, and ensuring the sustainable use of groundwater resources and the protection of the ecological environment. The systematic evaluation shows that there is 252.99×108 m3 of groundwater natural resources in the Haihe River Basin, and 172.98×108 m3 of exploitable resources under ecological water level constraints, and 4.68×108 m3 availability of deep water. The quality of groundwater in the mountainous areas of Haihe River Basin is generally good, type Ⅰ-Ⅲ groundwater accounting for 40.83%, and the quality of the shallow groundwater in the plain area is worse; type Ⅰ-Ⅲ groundwater accounts for 14.10%, meanwhile the quality of deep groundwater is better than the shallow groundwater; and type Ⅰ-Ⅳ groundwater accounts for 74.25%. The overall potential of groundwater exploitation in the mountainous areas of Haihe River Basin is relatively small. There is almost no exploitation potential in Yanshan and the north part of Taihang Mountain because of poor groundwater resource. There is no or little exploitation potential in the central part of Taihang Mountain because of a high degree of groundwater exploitation. There is comparatively great exploitation potential in the southern Taihang Mountain because of abundant groundwater resource. The exploitation potential of shallow groundwater in different hydrogeological units in the plain area is quite different. Because of large-scale groundwater drop funnel caused by long-time over exploitation, the shallow groundwater in the piedmont plain has no more exploitation potential. Meanwhile, there is little exploitation potential in the central and eastern plain, with mainly brackish water. Because of a low degree of groundwater exploitation in the Lubei plain, the exploitation potential of Liaocheng-Dezhou is comparatively great. There is no exploitation potential in Xiong'an New District. There is no exploitation potential of deep groundwater in the plain area.

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  • 图 1  海河流域地理位置图

    Figure 1. 

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    图 2  海河流域水文地质图

    Figure 2. 

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    图 3  海河流域降水量变化趋势

    Figure 3. 

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    图 4  海河流域主要河流出山口实测径流量

    Figure 4. 

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    图 5  海河流域地下水开采量变化趋势

    Figure 5. 

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    图 6  海河流域平原地下水位动态曲线

    Figure 6. 

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    图 7  海河流域天然资源模数分区图

    Figure 7. 

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    图 8  海河流域地下水资源量（按行政区）

    Figure 8. 

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    图 9  深层水可利用量

    Figure 9. 

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    图 10  地下水质量图

    Figure 10. 

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    图 11  海河流域浅层地下水开采潜力图

    Figure 11. 

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    表 1  平原区地下水降落漏斗面积演变

    Table 1.  Evolution of groundwater depression cone in plain area

    下载: 导出CSV

    表 2  地下水资源量及其分布（按地下水资源区，TDS≤2 g/L）

    Table 2.  groundwater resources and distribution(according to groundwater resource division)

    下载: 导出CSV

    表 3  浅层地下水开采潜力状况

    Table 3.  Potential of shallow groundwater exploitation

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    表 4  深层地下水开采潜力状况

    Table 4.  Exploitation potential of deep groundwater

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