在城市地区使用地质物理方法评估地面沉降区
Lara De Giorgi1, Dora Francesca Barbolla1, Chiara Torre2
1Institute of Heritage Science, National Research Council, Prv.le Lecce-Monteroni c/o Campus Universitario Ecotekne, 73100 Lecce, Italy.
Sensors (Basel, Switzerland)
|June 27, 2024
概括
城市空洞存在地质风险. 在加利波利进行的地质调查显示,在洞穴倒塌16年后,地下水分增加,这凸显了对地下结构的持续监测的需要.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 城市规划是城市规划.
背景情况:
- 城市地区面临着沉没洞穴的地质风险,通常与过去的人类和自然活动有关.
- 地下洞穴经常被用作废弃的垃圾填埋场,在人口密的中心构成重大风险.
- 2007年在加利波利发生的空洞崩造成了结构损坏,强调了研究和监测的必要性.
研究的目的:
- 评估城市地区地下空洞在崩塌后的演变.
- 评估地质物理方法在监测空洞稳定性随时间推移中的有效性.
- 了解与城市地质风险相关的地下条件变化.
主要方法:
- 使用地面穿透雷达 (GPR) 进行的地球物理调查于2007年进行,并于2022年重复.
- 对16年间隔获得的GPR数据进行比较分析.
- 地质和洞穴学描述和城市洞穴的目录.
主要成果:
- GPR数据比较显示,2007年至2022年间,腔结构没有显著变化.
- 与2007年相比,2022年检测到地下水分的增加.
- 研究区域容易受到与地下空洞相关的地质风险.
结论:
- 持续监测和保护地下空洞对于城市风险管理至关重要.
- 像GPR这样的地质物理方法是评估地下条件变化的宝贵工具.
- 地下水分增加可能表明城市地质环境中的风险正在演变.
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