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Geophysical and intrusive site investigations to detect an abandoned coal-mine access shaft, Apedale, Staffordshire, UK

机译:地球物理和侵入性现场调查,以发现废弃的煤矿通道,英国斯塔福德郡阿佩代勒

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Derelict coal mine workings at Apedale in Staffordshire, United Kingdom were the focus for a multi-disciplinary geophysical and intrusive site investigation. Objectives were to: 1) locate the surface entrance to a coal mine access shaft, 2) determine the inclined shaft's changing depth below present ground level, 3) determine if it was open, partly or fully filled, 4) locate it beneath a known shaft if (1) was unsuccessful and finally 5) compare geophysical mineshaft detection techniques in difficult ground conditions. After initial site reconnaissance, desktop study and modelling, field work collected surface micro-gravity and electrical resistivity imaging (ERI) 2D profiles to locate the shaft and entrance area. The made-ground nature of the site made identification of clear geophysical anomalies challenging. Subsequent intrusive investigations to locate the entrance were unsuccessful. A second phase of fieldwork down a known mineshaft imaged three geophysical anomalies beneath this shaft floor; after comparison with modelled data, subsequent intrusive investigations of the ERI anomaly successfully located the target shaft. Collapsed material was progressively cleared to the surface and a new shaft entrance stabilized. Surface micro-gravity 2D profiles surprisingly did not produce clear target anomalies, likely to be due to the target depth below ground level and the variety of above-ground, relict mine structures present. Surface ERI 2D profiles were less affected by above-ground structures but investigated anomalies were found to be heterogeneous ground materials. Comparisons of 2D micro-gravity, ERI and ground-penetrating radar profiles collected within a mineshaft showed ERI data were optimal. 2D micro-gravity and ERI modelling were shown to aid geophysical interpretations.
机译:英国斯塔福德郡Apedale废弃的煤矿工作是多学科地球物理和侵入性现场调查的重点。目的是:1)定位到煤矿出入口井筒的地面入口; 2)确定倾斜井筒在当前地面以下的变化深度; 3)确定倾斜井筒是否已打开,部分或全部充满; 4)将其放置在已知的地下如果(1)不成功,最后5)比较在困难地面条件下的地球物理矿井探测技术。在最初的现场勘测,桌面研究和建模之后,野外工作收集了表面微重力和电阻率成像(ERI)2D轮廓以定位竖井和入口区域。该地点的地面性质使得识别清晰的地球物理异常具有挑战性。随后的侵入式调查未找到入口。沿已知矿井进行的野外工作的第二阶段,在该井底下成像了三个地球物理异常。与建模数据进行比较之后,随后对ERI异常的侵入式调查成功地确定了目标井。塌陷的物料逐渐清除到表面,新的竖井入口稳定。令人惊讶的是,表面微重力2D剖面不会产生清晰的目标异常,这可能是由于目标深度低于地面深度以及存在的地上,遗迹矿山结构的多样性。表面ERI 2D轮廓受地上结构的影响较小,但调查的异常被发现是异质地面材料。比较矿井内收集的二维微重力,ERI和探地雷达剖面,表明ERI数据是最佳的。显示了2D微重力和ERI建模有助于地球物理解释。

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