桂西南群发型岩溶内涝形成的水文机制和应急响应OA
Formation hydro-mechanisms and emergency response of clustered karst waterlogging in southwestern Guangxi
极端降雨引发的群发型岩溶内涝呈现链式灾害传递的新特征,其水文机制与应急响应体系亟待深入研究.文章以2025年9-10月桂西南百色市岩溶内涝为对象,通过水文地质调查与监测、遥感解译及水化学追踪,揭示了台风引起的极端降雨条件下岩溶系统的内涝形成及灾害转移机制.研究发现:三次台风过程累计降雨量达689 mm,单日最大169 mm.强降雨引发岩溶含水层管道-裂隙空间的水量超饱和,致使内涝积水下降速度仅2~3 cm·d-1.地下河洪水消退半衰期延长至9.8d,衰退系数降至0.07 d-1,消退速度慢于2023和2024年的最大洪水事件,显示极端水文条件下岩溶管道系统满水且慢流,致灾风险增加.内涝水体滞留最长35 d,导致叶绿素浓度升高,有色溶解有机质平均高于地下水、河流和水库,呈现明显的富营养化趋势.研究揭示了岩溶内涝灾害的气候-水文-水环境的传递机制,研究发现落水洞堵塞、采矿和工程干扰等导致的地下河水文级联响应以及排水功能衰退是加剧内涝的主因.内涝应急处置中抽排水发挥关键作用,单个洼地分级强排260万m3,总排水量500万m3,排水规模前所未有.文章提出了以地下河流域管理为核心的内涝治理框架,强调落水洞-岩溶管道-排泄点自上而下的疏通与流域协同调控的内涝治理方案.
Clustered karst waterlogging triggered by extreme rainfall exhibits noval characteristics of chain-type disaster propagation,underscoring the urgent need for in-depth investigations into its hydrological mechanisms and emergency response systems.This study focuses on the karst waterlogging events in Baise City,southwestern Guangxi,during the period from September to October of 2025,employing hydrogeological surveys and monitoring,remote sensing interpretation,and hydrochemical tracing to reveal the formation and disaster transfer mechanisms of karst waterlogging under extreme rainfall conditions induced by typhoons.The findings indicate that three typhoon processes accumulated 689 mm of rainfall,with a daily maximum of 169 mm.Intense rainfall induced supersaturation of water volumes within the conduit-fracture spaces of karst aquifers,resulting in a decline rate of waterlogging accumulation of merely 2 to 3 cm·d-1.The flood recession half-life of subterranean rivers extended to 9.8 days,with the recession coefficient decreasing to 0.07 d-1,indicating slower recession than the maximum flood events of 2023 and 2024.These observations demonstrate that under extreme hydrological conditions,the karst conduit system operates under a"full water and slow flow"state,increasing disaster risks.The waterlogging water bodies remained stagnant for up to 35 days,leading to elevated chlorophyll concentrations and CDOM(Chromophoric Dissolved Organic Matter)levels averaging higher than those in groundwater,rivers,and reservoirs,indicating a distinct eutrophication trend.This study proposes a climate-hydrology-water environment transmission mechanism for karst waterlogging disasters,identifying that the blockage of sinkholes,mining actvities,and engineering disturbances induce hydrological cascade responses in subterranean rivers and degrade drainage capacity-key factor exacerbating waterlogging.During emergency response to waterlogging,pumping and drainage played a pivotal role,with a single depression achieving staged intensive pumping of 2.6 million m3 and a total drainage volume of 5.0 million m3—marking an unprecedented scale of dewatering operations.The study proposes a waterlogging mitigation framework centered on subterranean river basin management,emphasizing an integrated solution that combines top-down dredging of the sinkholes-karst conduits-discharge outlets continuum with basin-wide collaborative regulation.
姜光辉;郭芳;覃建明;黄永运;陈颢云;张勤军;康志强;张勇;刘小明
广西大学土木建筑工程学院,广西南宁 530004||广西大学广西岩溶区水安全与智慧调控工程研究中心,广西南宁 530004中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室,广西桂林 541004广西大学土木建筑工程学院,广西南宁 530004广西大学土木建筑工程学院,广西南宁 530004广西大学土木建筑工程学院,广西南宁 530004广西壮族自治区地质调查院,广西南宁 530023广西壮族自治区地质调查院,广西南宁 530023广西壮族自治区地质环境监测站,广西南宁 530201广西壮族自治区地质环境监测站,广西南宁 530201
天文与地球科学
2025年百色内涝群发型岩溶内涝地下河系统管理洪水消退系数内涝灾害链式响应
2025 Baise waterlogging eventclustered karst waterloggingsubterranean river system managementflood recession coefficientcascading response of waterlogging disasters
《中国岩溶》 2026 (3)
443-452,10
广西自然科学基金项目(2025GXNSFDA02850008)广西重点研发计划项目(桂科AB24010054)国家自然科学基金资助项目(42272303)中国地质科学院基本科研业务费(JKYZD202414)广西重点岩溶内涝区详细调查项目(12N0075651942025824)
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