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Measurement of Peat Soil Shear Strength Using Wenner Four-Point Probes and Vane Shear Strength Methods

机译:用Wenner四点探头和叶片剪切强度方法测量泥炭土剪切强度

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The general objective of this research was to measure the peat soil shear strength using Wenner four-point probes and vane shear strength methods. Specifically, the objective of this study was two-fold, namely, (a) investigating the relationship between laboratory soil resistivity and undrained shear strength and (b) determineing the relationship between in-situ soil resistivity and undrained shear strength. Data were randomly collected over six locations in Meranek, Sarawak, for in-situ test and three repetitions for each data were set based on three parameters. The selected parameters were soil density, moisture content, and salinity for both laboratory and in-situ test using Wenner four-point probes and vane shear method. The soil resistivity and vane shear strength readings for laboratory test were correlated with soil salinity, moisture content, and density. The R2 values showed a good correlation for soil salinity (R2 =0.8468) and density (R2 =0.9475), respectively. However, a weak correlation of R2 =0.1205 was observed for soil moisture. The R2 value for in-situ correlation between soil resistivity and three parameters (soil salinity, moisture content, and density) was R2 =0.8916. It can be concluded that the peat soil shear strengths of the study area using Wenner four-point probes from in-situ were (4.38 ohm.m) and laboratory was (2.47 ohm.m) and when using the vane shear strength method, in-situ was (23 kPA) and laboratory was (5 kPA). This study implies that the peat soil of the study area can be categorized as texture (soft loamy soil) and it is suitable for agriculture instead of construction. The relationship established between Wenner four-point probes and vane shear method can be beneficial for ground engineering design to enhance investigation on site suitability. Future work on DUALEM-421 technique should be emphasised for better subsurface exploration accuracy and resolve peat depth for an in-situ test.
机译:本研究的一般目标是使用Wenner四点探针和叶片剪切强度方法测量泥炭土剪切强度。具体而言,本研究的目的是两倍,即(a)研究实验室土壤电阻率和不介绍的剪切强度与(b)之间的关系,确定原位土壤电阻率和未润湿的剪切强度之间的关系。数据在Meranek,Sarawak中的六个位置随机收集,用于原位测试,并根据三个参数设置每个数据的三个重复。使用Wenner四点探针和叶片剪切方法,所选参数是土壤密度,水分含量和盐度,以及原位测试。用于实验室测试的土壤电阻率和叶片剪切强度读数与土壤盐度,水分含量和密度相关。 R 2值分别显示了土壤盐度(R2 = 0.8468)和密度(R2 = 0.9475)的良好相关性。然而,针对土壤水分观察到R2 = 0.1205的弱相关性。土壤电阻率与三个参数(土壤盐度,水分含量和密度)的原位相关性的R2值为R2 = 0.8916。可以得出结论,使用来自原位的Wenner四点探针的研究区域的泥炭土壤剪切强度(4.38欧姆)和实验室是(2.47欧姆)和使用叶片剪切强度法, -Situ是(23 KPA)和实验室(5 KPA)。本研究意味着研究区的泥炭土可以作为纹理(软壤土)(软壤土)分类,适用于农业而不是建筑。 Wenner四点探头和叶片剪切方法之间建立的关系可以有利于地面工程设计,以提高现场适应性的调查。应强调对Dualem-421技术的未来工作以获得更好的地下勘探精度,并解决原始测试的泥炭深度。

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