Assessment of liquefaction potential of soil based on standard penetration test for the upper Benue region in Nigeria

被引:7
|
作者
Wadi, Dafalla [1 ]
Wu, Wenbing [1 ]
Malik, Ibrahim [2 ]
Ahmed, Hafizullah Abba [3 ]
Makki, Abdelazim [2 ]
机构
[1] China Univ Geosci, Minist Educ, Engn Res Ctr Rock Soil Drilling Excavat & Protect, Wuhan 430074, Hubei, Peoples R China
[2] Al Neelain Univ, Dept Geol, POB 11121, Khartoum, Sudan
[3] Modibbo Adama Univ Technol, Dept Geol, PMB 2076, Yola, Nigeria
关键词
Subsurface soil; Earthquake; Liquefaction; Safety factor; SPT; Nigeria; SHEAR-WAVE VELOCITY; DETERMINISTIC ASSESSMENT; CYCLIC RESISTANCE; VARIABILITY; EARTHQUAKE; AFRICA; TROUGH; INDEX; CITY;
D O I
10.1007/s12665-021-09565-y
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Determining a specific site 's geotechnical parameters is a crucial step in geotechnical analyses and designs in a seismically active area. In recent years, many parts of Nigeria have been subjected to several earthquakes; therefore, subsurface description has been a challenging task in geotechnical practice in this region. This paper aims to evaluate subsurface formation for soil liquefaction analysis at a sugar plant site located in Nigeria 's Upper Benue region. The study used data from the standard penetration test (SPT) measured at 28 boreholes and soil samples ' laboratory analysis. The liquefaction parameters were derived according to the procedure in Idriss and Boulanger (2014). Soil liquefaction has been evaluated, assuming an earthquake scenario of 7.5 M-w with a peak horizontal acceleration (a(max)) of 0.15 g. Results showed that the subsurface formation between 1.5 and 4.5 m is saturated loose to medium-dense sandy, silty clayey soil, and the liquefaction safety factor is less than 1. The Formation at a depth deeper than 4.5 m comprises very densely to stiff clayey sands with a safety factor higher than 1. The applied approach has been proved to be a rapid and reliable method for investigating sandy soil's liquefaction under the effect of earthquakes.
引用
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页数:11
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