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Combined geophysical and geotechnical investigation of pavement failure for sustainable construction of Owo-Ikare highway, Southwestern Nigeria

机译:尼日利亚西南部欧比尔岛高速公路可持续建设路面故障的地球物理和岩土工程研究

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Very low frequency electromagnetic (VLF-EM) and electrical resistivity methods involving 54 Schlumberger Vertical Electrical Sounding (VES) and 2-D geoelectrical resistivity imaging using dipole-dipole array were utilised along unstable (US) and stable sections (SS) of Owo-Ikare highway to establish causes of its persistent failure. Engineering evaluation of eighteen soil samples from test pits excavated on selected US and SS were investigated. VLF-EM models, geoelectric sections and 2-D resistivity structures revealed existence of conductive subsurface structures, suspected weak zones beneath the US. The road pavement is constructed on poor clayey subgrade ?with low resistivity values (<100 Ohm-m) which precipitate instability of the highway. Subgrade soils below US have poor geotechnical properties characterized by high moisture content, liquid limit (43.6–63.8% and 20.1–25.2%), plasticity index (13.4–34.4% and 6.5–8.3%), percentage fines (40–67% and 28–30%), A-7-5 to A-7-6 clayey soils, high linear shrinkage (>10%), low compacted density, low CBR, volume changes (Mv) and impervious soils against those of SS. . Thus, deep-weathering, fractured bedrock, uneven bedrock topography with subsurface structures, water-saturated clayey subgrade and unsuitability of the soils for subgrade and subbase road construction are responsible for instability of the road. Replacement of soil beneath the unstable sections and effective drainage enhances its stability.
机译:非常低频电磁(VLF-EM)和涉及使用偶极 - 偶极阵列的54斯克洛伯格垂直电气探测(VES)和2-D电阻率成像的电阻器方法沿着不稳定(US)和owo的稳定部分(SS)使用ikare高速公路建立了持续失败的原因。研究了从选定的美国和SS上膨胀的测试坑中的18种土壤样品的工程评估。 VLF-EM型号,电气电路和二维电阻率结构揭示了导电地下结构的存在,在美国下方的疑似弱区。道路路面是在较差的粘土路基上构建?具有低电阻率值(<100欧姆-M),其沉淀出高速公路的不稳定性。美国低于美国的降土性质具有较差的岩土性能,其特征在于含水量高,液体限制(43.6-63.8%和20.1-25.2%),可塑性指数(13.4-34.4%和6.5-8.3%),粒度百分比(40-67% 28-30%),A-7-5至A-7-6粘土土壤,高线性收缩(> 10%),低压缩密度,低CBR,体积变化(MV)和SS的渗透性土壤。 。因此,深化风化,破碎的基岩,不均匀的基岩地形与地下结构,水饱和的粘土路基和不适合的路基和子巴士道路建设负责道路的不稳定。在不稳定的部分下方的土壤替代,有效的排水增强了其稳定性。

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