防止天津再次发生沉降:新的预巩固头和安全的抽水缓冲器
Kuan Wang1, Guoquan Wang1, Yan Bao2
1Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX, 77204.
Ground water
|March 22, 2024
概括
天津的土地沉降因南北水分转移项目而减少. 深层含水层的新预巩固头表明沉降已经停止,为可持续的地下水管理提供了战略.
科学领域:
- 地质科学 地质科学
- 水文学的水文学
- 遥感 遥感 遥感 遥感
背景情况:
- 中国天津几十年来经历了大量的土地沉降.
- 南向北水分流项目于2014年开始供应地表水.
- 最近的数据显示,自2019年以来,沉降率有所下降.
研究的目的:
- 分析地表水进口对天津土地沉降的影响.
- 在深层水层中识别新的预巩固头,并建立安全的地下水提取限制.
- 制定可持续的地下水管理策略,以防止反复沉降.
主要方法:
- 使用 Sentinel-1A 交叉测量合成孔径雷达 (InSAR) 数据从2014年到2023年.
- 分析了长期的地下水位数据集.
- 开发了用于识别新建立的预巩固头 (NPCH) 和计算安全抽缓冲器 (SPB) 的方法.
主要成果:
- 天津平原的三分之一已经停止退化或正在经历土地反弹.
- 深层含水层系统已经完成了巩固周期,形成了新的预巩固头.
- 确定用于可持续地下水管理的NPCH和SPB的既定方法.
结论:
- 地下水的提取可以通过在新建立的预巩固头上方保持液压头来可持续地管理.
- 安全的抽气缓冲的概念对于防止永久沉降至关重要.
- 这项研究为补贴地区的地下水资源管理提供了一个框架.
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