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I-40 along the Cumberland Escarpment Highway Instability, Historic Reviews, and Remedial Concepts

机译:I-40沿着坎伯兰悬崖悬崖公路不稳定,历史评论和补救概念

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The eastern Cumberland Plateau Escarpment, separating the Cumberland Plateau and the Valley and Ridge Physiographic Provinces, has a record of hampering highway construction in central East Tennessee, due to a combination of steep natural slopes, thick accumulations of colluvium, and the presence of swelling clay from the Pennington Formation. In that record is the 1968 construction failure of approximately 370 meters of eastbound Interstate Highway 40 embankment. Planned as an up to 43- meter high embankment across the Escarpment, the Tennessee Department of Transportation (TDOT) responded to the landslide and embankment failure through geometric modifications and slide mass drainage using dewatering wells and horizontal drains. Even with these mitigation measures and periodic installation of additional horizontal drains, movement of the slide mass has continued through the ensuing decades. Measurements in 2010 had shown displacement on the order of 25 millimeters per year, requiring annual resurfacing of the pavement. Interstate Highway 40 (I-40) is a heavily-traveled, east-west interstate through the mid-section of the United States. Traffic safety concerns with a traffic-disruption threat led TDOT to request a detailed review of the available project documentation by Golder Associates Inc. Since the initial slide, limited topographic, geologic, and geotechnical data have been gathered and assimilated for evaluation of the slide. As a result of Golder’s review, additional slope inclinometers and automated vibrating-wire piezometers were installed to better define the conditions and their variation with time. A limited laboratory testing program was conducted for evaluating potential remediation options. Installation of a system of dewatering wells and horizontal drainage was initiated in late 2011 in an effort to mitigate further displacement. Implementation of these drainage measures was still underway at the time of publication. This paper presents the historical background, results from the first year of slope and groundwater monitoring, dewatering program, and feasible remediation options available to TDOT in order to improve the margin of safety on this career-spanning slope failure.
机译:东部坎伯兰高原悬崖悬崖,分离坎伯兰高原和山谷和岭和岭地理省份,在中东田纳西州的禁止公路建设,由于陡峭的天然斜坡,较厚的凝聚累积以及肿胀粘土的存在,以及膨胀粘土的存在从彭宁顿形成。在该记录中,1968年建筑失效大约370米的东行州际公路40辆路堤。在悬崖部(TDOT)抵抗悬崖部门的悬崖部(TDOT)延长至43米高的路堤,使用脱水井和水平排水管通过几何修改和滑动质量排水来响应滑坡和堤防失效。即使采取这些缓解措施和周期性安装额外的水平排水沟,滑动质量的运动也在继续,通过随后的数十年来。 2010年的测量显示了每年25毫米的排量,需要年度重新铺设路面。州际公路40号(I-40)是一流的东西,东西斯特 - 西方州际,通过美国的中间部分。交通安全的疑虑与交通中断威胁LED TDOT要求通过Golder Associates Inc的可用项目文件详细审查。由于初始载玻片,有限的地形,地质和岩土信息,并融合了评估幻灯片。由于Golder的审查,安装了额外的坡度倾角系和自动振动 - 线压电仪以更好地定义条件及其随时间的变化。进行有限的实验室测试计划,以评估潜在的修复方案。 2011年底开始安装脱水井和水平排水系统,以减轻进一步的位移。这些排水措施的实施仍在出版时仍在进行。本文介绍了坡度和地下水监测,脱水方案的第一年的历史背景,可用于TDOT的可行性补救措施,以提高本职业生涯跨越失败的安全范围。

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