首页> 外文会议>Highway Geology Symposium; 20071016-18; Pocono Manor,PA(US) >Geotechnical Investigations for Realignment of I-76 Across The New Baltimore Landslide, SW Pennsylvania
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Geotechnical Investigations for Realignment of I-76 Across The New Baltimore Landslide, SW Pennsylvania

机译:在宾夕法尼亚州西南部新巴尔的摩滑坡上进行I-76调整的岩土工程勘察

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The Pennsylvania Turnpike Commission (PTC) plans to widen 1-76 due to increased traffic in Somerset County. The New Baltimore landslide, which has caused serious problems for the turnpike since its construction in 1939, is located near mile marker 128 in Somerset County. The landslide extends 2000 feet (610 m) upslope and 1000 feet (305 m) laterally, and moves 5 to 10 inches (13 to 25 cm) per year. The design plan for widening the turnpike may require cutting into the slope between mile markers 128 and 129 on the east-bound side of the turnpike, thereby passing through the New Baltimore landslide. A matter of significant concern is reactivation of the landslide upon realignment, adding to the existing instability. This research project is being conducted to determine the engineering properties of rocks and stability of slopes located between the mile markers mentioned above. Field work is currently being conducted to find the upper limit of the landslide. Preliminary discontinuity data are being analyzed to evaluate various modes of slope failure. A subsurface investigation, consisting of 12 borings and installation of 6 slope inclinometers and 1 piezometer, was conducted by American Geotechnical and Environmental Services, Inc. of Pennsylvania. Laboratory tests were conducted on the core samples to determine slake durability and unconfined compressive strength. The results of the study completed so far show that the bedrock geology of the New Baltimore landslide site consists of the Upper Devonian Catskill Formation which contains inter-bedded sequences of claystone, siltstone, and sandstone units. The slake durability index of claystone ranges from 72% to 99% whereas the unconfined compressive strength of the sandstone/siltstone units ranges from 8900 psi (61 MPa) to 25600 (177 MPa) psi. The inclinometer data show that there is small movement along the weaker claystone/clayey siltstone units (where gouge was encountered during drilling) and this is being closely monitored. This study is still in progress. The results of the study will be used to develop remedial measures for the New Baltimore landslide so that the interstate highway can be realigned safely.
机译:宾夕法尼亚州收费公路委员会(PTC)计划由于萨默塞特郡的交通增加而扩大1-76。自1939年修建以来,新巴尔的摩滑坡就一直对收费公路造成严重问题,它位于萨默塞特郡128英里处。滑坡向上延伸2000英尺(610 m),横向延伸1000英尺(305 m),每年移动5至10英寸(13至25 cm)。加宽收费公路的设计计划可能需要切入收费公路东行的英里标记128和129之间的坡度,从而穿过新巴尔的摩滑坡。重大关切的问题是重新调整后重新激活滑坡,增加了现有的不稳定性。正在进行该研究项目,以确定岩石的工程特性和位于上述英里标记之间的斜坡的稳定性。目前正在实地调查以找到滑坡的上限。初步的不连续性数据正在分析,以评估各种形式的边坡破坏。宾夕法尼亚州的美国岩土工程与环境服务公司进行了地下勘测,包括12个钻孔以及6个倾斜测斜仪和1个测压仪的安装。在核心样品上进行了实验室测试,以确定耐久性和无侧限抗压强度。迄今完成的研究结果表明,新巴尔的摩滑坡场的基岩地质包括上泥盆统卡茨基尔组,其中包含层间层序的粘土岩,粉砂岩和砂岩单元。黏土的抗老化性指数范围为72%至99%,而砂岩/粉砂岩单元的无限制抗压强度范围为8900 psi(61 MPa)至25600(177 MPa)psi。测斜仪的数据显示,沿较弱的粘土岩/粘土粉砂岩单元(在钻探过程中碰到了凿子)有很小的运动,并且对此进行了密切监视。这项研究仍在进行中。研究结果将用于制定新巴尔的摩滑坡的补救措施,以便可以安全地重新调整州际公路。

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