ENGINEERING GEOLOGICAL STUDY ON THE SLOPE FAILURE ALONG THE KIMANIS TO KENINGAU HIGHWAY, SABAH, MALAYSIA

R. Roslee, F. Tongkul
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引用次数: 1

Abstract

The geology along the Kimanis to Keningau Highway provides a favourable setting for engineering geological instability. The area is underlain by the Crocker Formation (Late Eocene to Early Miocene age) to vary recent Quaternary alluvial materials which are still being deposited. Crocker Formation consists mostly of interbedded grey sandstones and grey mudstones or shales. The sandstones are texturally immature where angular to subrounded quarts grains are cemented by clay minerals and occasionally by calcite. The Crocker Formation has also undergone intense deformation. The tectonic complexities influenced the physical and mechanical properties of the rocks, resulting in a high degree of weathering and instability. The weathered materials are unstable and may experience sliding due to by high pore pressure and intensively geomorphological processes. In this study, a total of 28 selected critical slope failures were studied and classified into two main groups: rock slope and soil slope. Failures in soil slopes (including embankments) are 18 (64 %) whereas 10 of all failures (36 %) of rock slope. Soil slope failures normally involved large volumes of failed material as compared much rock slopes, where the failures are mostly small. Of the 18 failures in soil slopes, 6 (33 %) are embankment failures making them 21 % of all types of failures. Kinematics rock slope analyses indicates that the variable potential of circular, planar, wedges and toppling failures modes as well as the combination of more than one mode of aforementioned failure. Rock and soil slopes stability analysis indicates that the factor of safety value as unsafe (0.50 to 0.96). The main factors causing slope failure occurrences in the study area are natural (geology, meteorology, topography and drainage system) and human factors (lack of proper planning, human activities and community’s attitude). Development planning has to consider the hazard and environmental management program. This engineering geological study should be prioritized and take into consideration in the initial step in all infrastructures program and it may play a vital role in landslide hazard and risk assessment to ensure the public safety.
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马来西亚沙巴州基马尼斯至肯宁高公路沿线边坡破坏的工程地质研究
基马尼斯至肯宁高公路沿线的地质条件为工程地质失稳提供了有利条件。该地区位于克罗克组(始新世晚期至中新世早期)之下,变化了第四纪冲积物,这些冲积物仍在沉积。克罗克组主要由灰色砂岩和灰色泥岩或页岩组成。砂岩在结构上是不成熟的,角状到次圆形的石英颗粒被粘土矿物胶结,偶尔被方解石胶结。克罗克组也经历了剧烈的变形。构造的复杂性影响了岩石的物理和机械特性,导致了高度的风化和不稳定。由于高孔隙压力和强烈的地貌作用,风化材料不稳定,可能发生滑动。本研究选取了28个临界边坡失稳类型进行研究,并将其分为岩质边坡和土质边坡两大类。土质边坡(包括路堤)的破坏有18个(64%),而岩石边坡的破坏有10个(36%)。与岩石边坡相比,土壤边坡的破坏通常涉及大量的破坏物质,而岩石边坡的破坏大多很小。在18种土质边坡破坏中,有6种(33%)是路堤破坏,占所有类型破坏的21%。岩质边坡运动学分析表明,圆形破坏模式、平面破坏模式、楔形破坏模式和倾倒破坏模式的变化潜力以及上述几种破坏模式的组合。岩土边坡稳定性分析表明,安全系数为不安全(0.50 ~ 0.96)。导致研究区边坡破坏发生的主要因素有自然因素(地质、气象、地形、排水系统)和人为因素(缺乏适当的规划、人类活动和社区态度)。发展规划必须考虑危害和环境管理方案。该工程地质研究应在所有基础设施规划中优先考虑,在滑坡危害和风险评估中发挥重要作用,确保公共安全。
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