首页> 外文期刊>Engineering Geology >A sinkhole susceptibility zonation based on paleokarst analysis along a stretch of the Madrid-Barcelona high-speed railway built over gypsum- and salt-bearing evaporites (NE Spain)
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A sinkhole susceptibility zonation based on paleokarst analysis along a stretch of the Madrid-Barcelona high-speed railway built over gypsum- and salt-bearing evaporites (NE Spain)

机译:沿石膏和含盐蒸发物之上修建的马德里-巴塞罗那高速铁路的一段,基于古岩溶分析,建立了一个塌陷敏感性区(西班牙东北部)

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This paper presents a methodology for producing sinkhole susceptibility zonations along linear infrastructures based on the analysis of the subsidence and dissolution features exposed in the adjacent cuttings and the distribution of karstic depressions. The proposed approach have been applied to a 24 km long stretch of the high-speed Madrid-Barcelona railway built on halite- and glauberite-bearing evaporites of the Tertiary Zaragoza Gypsum Formation. More than 100 km of this railway line have been built over salt-bearing Tertiary evaporites and trains run at a cruising speed of 300 km/h. The susceptibility assessment has been restricted to the sections located in karstic depressions (2.98 km) and trenches excavated in the ground (13.93 km). A low susceptibility has been assigned to the sections built on thickened alluvium of the Huerva fluvial system (0.5 km) and those in which the evaporites exposed in the cuttings do not show evidence of dissolution or subsidence (3.52 km). A total of 4.5 km have received an intermediate susceptibility. The cuttings in these sections show sagging structures, cavities above the railway roadbed, irregular rockhead or shallow alluvium-bedrock boundary. A high susceptibility has been assigned to a total of 6.59 km. These correspond to cavities and collapse structures that reach the railway roadbed (3.61 km) and karstic depressions generated by interstratal karstification and subsidence (2.98 km). The paleokarst and geomorphic evidence in these sections reveals that cavities, either air- or sediment-filled, do exist beneath the railway. The distribution of the karst features and susceptibility zones seems to be controlled to a large extent by the lithostratigraphy of the bedrock; wedging out of the evaporites to the SE and increase in the proportion of halite and glauberite to the NW. The proposed zonation could be used as the basis for the selection of the stretches where further investigations and the application of mitigation measures would have a better cost/benefit ratio.
机译:本文通过分析相邻岩屑中的沉降和溶出特征以及岩溶洼地的分布,提出了一种沿线性基础设施产生塌陷敏感性带的方法。拟议中的方法已被应用到长24公里长的马德里-巴塞罗那高速铁路上,该铁路建立在第三萨拉戈萨石膏地层的含盐和辉沸石的蒸发岩上。这条铁路线的100多公里已在含盐的第三系蒸发物上建造,火车以300 km / h的巡航速度行驶。敏感性评估仅限于岩溶洼地(2.98 km)和地下挖沟(13.93 km)的断面。对Huerva河流系统增厚冲积层上的剖面(0.5 km)的敏感性很低,而在钻屑中暴露的蒸发物未显示出溶解或沉降的证据(3.52 km)。总共4.5公里已达到中等敏感性。这些部分中的切屑显示出垂垂的结构,铁路路基上方的空洞,不规则的岩头或浅冲积层-基岩边界。高敏感度已分配给总计6.59公里。这些对应于到达铁路路基的空洞和坍塌结构(3.61 km)以及由层间岩溶和沉陷产生的岩溶洼地(2.98 km)。这些部分中的古喀斯特和地貌证据表明,在铁路下面确实存在着充满空气或沉积物的空洞。岩溶特征和敏感性区的分布似乎在很大程度上受基岩的岩性地层学控制。从蒸发岩中析出到东南部,并增加了盐岩和钙辉石在西北部的比例。拟议的分区可以用作选择河段的基础,进一步研究和采取缓解措施将有更好的成本/收益比。

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