长江科学院院报
長江科學院院報
장강과학원원보
JOURNAL OF YANGTZE RIVER SCIENTIFIC RESEARCH INSTITUTE
2015年
2期
68-71
,共4页
高密度电法%电阻率%挡墙%潜水位%空洞
高密度電法%電阻率%擋牆%潛水位%空洞
고밀도전법%전조솔%당장%잠수위%공동
high-density electrical method%electrical resistivity%retaining wall%potential water level%cavity
常规电法测量挡墙存在施工效率低的缺点,而高密度电法主要是以各种地下地质体的电性差异为基础,根据在施加电场作用下地层传导电流的分布规律,推断地下具有不同电阻率地质体的赋存情况,测量效率优于常规电法。将高密度电法用于南十里长沟主流左岸挡墙测量中,结果表明:挡墙高度约为2.3 m,墙后土体中潜水位埋深为3.1~3.8 m,挡墙体内部及内侧土体中空洞总体不发育,局部存在欠密实或空洞,挡墙厚度变化不大。高密度电法所得检测结果与地质雷达所得结果以及开挖所得结果一致,表明高密度电法应用于挡墙测量中是可行的。
常規電法測量擋牆存在施工效率低的缺點,而高密度電法主要是以各種地下地質體的電性差異為基礎,根據在施加電場作用下地層傳導電流的分佈規律,推斷地下具有不同電阻率地質體的賦存情況,測量效率優于常規電法。將高密度電法用于南十裏長溝主流左岸擋牆測量中,結果錶明:擋牆高度約為2.3 m,牆後土體中潛水位埋深為3.1~3.8 m,擋牆體內部及內側土體中空洞總體不髮育,跼部存在欠密實或空洞,擋牆厚度變化不大。高密度電法所得檢測結果與地質雷達所得結果以及開挖所得結果一緻,錶明高密度電法應用于擋牆測量中是可行的。
상규전법측량당장존재시공효솔저적결점,이고밀도전법주요시이각충지하지질체적전성차이위기출,근거재시가전장작용하지층전도전류적분포규률,추단지하구유불동전조솔지질체적부존정황,측량효솔우우상규전법。장고밀도전법용우남십리장구주류좌안당장측량중,결과표명:당장고도약위2.3 m,장후토체중잠수위매심위3.1~3.8 m,당장체내부급내측토체중공동총체불발육,국부존재흠밀실혹공동,당장후도변화불대。고밀도전법소득검측결과여지질뢰체소득결과이급개알소득결과일치,표명고밀도전법응용우당장측량중시가행적。
Ordinary electrical method is inefficient in the measurement of retaining wall,while high-density electri-cal method has better efficiency as it is based on the electrical prop of different underground geological bodies ac-cording to the distribution regularity of conduction current of strata.Therefore it was used in the measurement of re-taining wall at the left bank of mainstream Nanshilichanggou River,and the result showed that,the height of the wall is about 2.3m,the depth of potential water level in the earth behind the wall is about 3.1 -3.8m,cavities in the retaining wall and the earth are found in partial positions but are not developed in general,the thickness of the wall does not change a lot.The result is consistent with those from geological radar and practical excavation,indi-cating that high-density electrical method is feasible to measure retaining wall.