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崇明三岛地面沉降特征及浅部土层沉降原因分析

代如凤 战庆 吴建中 黄鑫磊

华东地质2026,Vol.47Issue(3):520-535,16.
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华东地质2026,Vol.47Issue(3):520-535,16.DOI:10.16788/j.hddz.32-1865/P.2024.09.007

崇明三岛地面沉降特征及浅部土层沉降原因分析

The characteristics of land subsidence and the cause analysis of shallow soil subsidence in Chongming three islands

代如凤 1战庆 2吴建中 2黄鑫磊2

作者信息

  • 1. 上海市地质勘查技术研究院,上海 200072||自然资源部地面沉降监测与防治重点实验室,上海 200072||上海地面沉降控制工程技术研究中心,上海 200072
  • 2. 上海市自然资源调查利用研究院,上海 200072||自然资源部地面沉降监测与防治重点实验室,上海 200072||上海地面沉降控制工程技术研究中心,上海 200072
  • 折叠

摘要

Abstract

Shanghai has been undergoing over a century of land subsidence,which is increasingly complex in terms of its mechanisms and causes in recent years.This study uses long-term settlement data extracted from layered extensometers located in the three monitoring stations on Chongming three islands.This study character-izes deep and shallow soil layer settlement under minimal subsidence conditions.Results show that shallow soil layers settle continuously,while deep layers remain stable or even rebound.Shallow soil layers contribute over 89%to land subsidence,making them the primary contributor.Analysis of shallow soil properties and external drivers reveals the primary causes of shallow soil settlement in Chongming three islands:①Rainfall changes alter phreatic water levels,triggering elastic deformation in shallow sand layers.②Foundation pit construction activi-ties trigger consolidation settlement in clay layers.This creates plastic deformation within compressible soil strata.③Land reclamation projects cause seepage consolidation in soft soils,generating secondary consolidation that decreases over time.These findings reveal new subsidence features in Chongming three islands and clarify shallow layer mechanisms,providing critical reference for developing precise ground subsidence control strate-gies.

关键词

崇明三岛/地面沉降/沉降特征/沉降机理/沉降主导层

Key words

Chongming three islands/land subsidence/subsidence characteristics/subsidence mechanism/dominant layer of subsidence

分类

天文与地球科学

引用本文复制引用

代如凤,战庆,吴建中,黄鑫磊..崇明三岛地面沉降特征及浅部土层沉降原因分析[J].华东地质,2026,47(3):520-535,16.

基金项目

上海市地质学会科研课题"长兴岛全部土层自然沉降特征和机理研究(编号:Dzxh202205)"、国家自然科学基金地质联合重点支持项目"长三角深层地下空间开发地质灾害孕育机制与风险预警(编号:U2444220)"和上海市优秀学术带头人项目"地下水位持续上升引发的地质环境效应及安全预警研究(编号:23XD1402400)"联合资助. (编号:Dzxh202205)

华东地质

2096-1871

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