中国地质
中國地質
중국지질
CHINESE GEOLOGY
2015年
1期
300-307
,共8页
岩溶地面塌陷%地面沉降%地下水位%相关%发展趋势
巖溶地麵塌陷%地麵沉降%地下水位%相關%髮展趨勢
암용지면탑함%지면침강%지하수위%상관%발전추세
karst ground collapse%land subsidence%groundwater level%correlation%development trend
提金沙洲可溶性灰岩分布面积广,岩溶洞隙发育,洞隙及地下水的连通性强,上覆第四系松散土体中软土广泛分布,客观存在岩溶地面塌陷及地面沉降的地质环境条件。2007年4月起,受某高铁隧道施工抽排地下水的影响,金沙洲地下水出现异常波动,引发了地面塌陷及地面沉降。文章根据监测数据,经对比分析结果表明,区内岩溶地面塌陷及地面沉降受控于地下水位的变化,地下水位波动至基岩面附近时,是地面塌陷较活跃的时期,地面沉降与地下水位变化呈正向相关。文章进一步对地面沉降与地下水位变化关系的机理进行了探讨,认为目前地下水位尚未恢复正常的区域仍存在地面塌陷及地面沉降的隐患。
提金沙洲可溶性灰巖分佈麵積廣,巖溶洞隙髮育,洞隙及地下水的連通性彊,上覆第四繫鬆散土體中軟土廣汎分佈,客觀存在巖溶地麵塌陷及地麵沉降的地質環境條件。2007年4月起,受某高鐵隧道施工抽排地下水的影響,金沙洲地下水齣現異常波動,引髮瞭地麵塌陷及地麵沉降。文章根據鑑測數據,經對比分析結果錶明,區內巖溶地麵塌陷及地麵沉降受控于地下水位的變化,地下水位波動至基巖麵附近時,是地麵塌陷較活躍的時期,地麵沉降與地下水位變化呈正嚮相關。文章進一步對地麵沉降與地下水位變化關繫的機理進行瞭探討,認為目前地下水位尚未恢複正常的區域仍存在地麵塌陷及地麵沉降的隱患。
제금사주가용성회암분포면적엄,암용동극발육,동극급지하수적련통성강,상복제사계송산토체중연토엄범분포,객관존재암용지면탑함급지면침강적지질배경조건。2007년4월기,수모고철수도시공추배지하수적영향,금사주지하수출현이상파동,인발료지면탑함급지면침강。문장근거감측수거,경대비분석결과표명,구내암용지면탑함급지면침강수공우지하수위적변화,지하수위파동지기암면부근시,시지면탑함교활약적시기,지면침강여지하수위변화정정향상관。문장진일보대지면침강여지하수위변화관계적궤리진행료탐토,인위목전지하수위상미회복정상적구역잉존재지면탑함급지면침강적은환。
Soluble limestone and Quaternary loose soft soil are widely distributed in Jinshazhou. The fractures in limestone are rich and well connected with each other, which leads to a good connection of groundwater. All these factors provide objective geological environment conditions for karst ground collapse and land subsidence. Since April 2007, affected by tunnel groundwater pumping in high-speed rail construction, groundwater has fluctuated abnormally, which has resulted in ground subsidence and land collapse in Jinshazhou. The monitoring data and comparative analysis show that the karst ground subsidence and land collapse are controlled by groundwater level changes. When groundwater level fluctuates near the bedrock surface, the ground collapse occurs easily, and the land subsidence is related to groundwater level change positively. The relationship between land subsidence and groundwater level changes was also studied and, on such a basis, it is held that the area where groundwater has not yet returned to the normal level still has the hidden trouble of ground subsidence and land collapse.