联合GNSS、GRACE与测井资料监测京津冀地下水储量时空变化

doi:10.3799/dqkx.2025.270

联合GNSS、GRACE与测井资料监测京津冀地下水储量时空变化

doi: 10.3799/dqkx.2025.270

邹蓉¹,
秦旭¹,
杨凡¹,
陈超²,
曹家铭³,
汪超¹,
王琪¹

1 中国地质大学(武汉)地球物理与空间信息学院, 地球内部多尺度成像湖北省重点实验室, 湖北武汉 430074;
2 武汉理工大学资源与环境工程学院, 武汉 430070;
3 重庆市测绘科学技术研究院, 自然资源部智能城市时空信息与装备工程技术创新中心, 重庆 401121

基金项目:

国家自然科学基金(No:42274009,42474006)

中国大陆构造环境监测网络项目(No:CMONOC2025-1-5)

详细信息

作者简介:
邹蓉（1980-），女，副教授，研究方向为水文过程与地壳形变的相互作用。ORCID：0000-0002-8415-9478. Email: zourong@cug.edu.cn

中图分类号: P341
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出版历程
- 收稿日期: 2025-10-30

摘要

摘要: 京津冀地区因地下水长期超采，已引发一系列地质与生态问题。为精准监测该区域地下水的时空变化，本文基于GRACE、GNSS与实测水井数据，反演2011—2020年京津冀地下水储量变化，并探讨了南水北调工程与人为用水对地下水的影响。GRACE反演结果与760口实测井水位数据相关性高达0.86，反演结果可靠；京津冀地下水位下降速率分别为-13.1 mm/a、-12.9 mm/a和-16.4 mm/a，其中邯郸—邢台一带地下水储量亏损最为严重，最大亏损速率高达-40 mm/a；GNSS垂向位移显示，2018年后GNSS基岩站隆升速率减缓，土层站沉降速率减缓，共同印证地下水亏损态势有所缓解。本文系统分析了京津冀地区近10年来地下水持续亏损的情况，揭示了2018年后地下水亏损情况好转的主因是农业用水的减少而不是南水北调工程，为科学评估与合理利用地下水提供有力支撑。
- GNSS /
- GRACE /
- 京津冀 /
- 地下水

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