首页> 外文期刊>KSCE journal of civil engineering >Sedimentation Behavior of Clays in Response to Pore-Fluid Chemistry: Effect of Ionic Concentration and pH on Its Trends
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Sedimentation Behavior of Clays in Response to Pore-Fluid Chemistry: Effect of Ionic Concentration and pH on Its Trends

机译:黏土在孔隙流体化学反应中的沉降行为:离子浓度和pH值对其变化趋势的影响

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摘要

This study investigates the effect of pore fluid chemistry on the sedimentation trends and liquid and plastic limits within the new fines classification framework for four clayey soils with different specific surface and mineralogy. The sedimentation tests and fall cone tests are performed with seven different ionic concentrations (c = 1 × 10~(-5) ~ 1.8 M) and the four target pH values (pH = 3,5,7, and 9) for each of the ionic concentrations. Three different sedimentation trends such as flocculated, dispersed, and mixed (at c = 0.0015-to-0.003 M) modes are observed at different ion concentrations and pH conditions of the pore fluids. Three sedimentation parameters named A_1, A_2 and A_3 are defined from the sedimentation curve. The relationship between them implies the salient features of the sedimentation trend for tested clayey soils. These parameters confirm the observed sedimentation modes and the critical ionic concentration; c* ~ 3 × 10~(-3) M for AMK and EPK (high specific surface) and c* ~ 1.5 × 10~(-3) M for LKW and MI (low specific surface) where notable fabric change occurs. The higher specific surface clays are classified as intermediate electrical sensitive clays whereas the lower specific surface clays are categorized into low electrical sensitivity fines in the new classification chart. A complementary data analysis for the sedimentation parameters and the new fines classification chart reveals that the robust link between distinct sedimentation trends and salient features of clay particles captured in the new fines classification chart can be useful to predict the sedimentation modes of clays with different pore fluid chemistry.
机译:本研究研究了孔隙流体化学对4种不同比表和矿物学的粘性土在新的细粒分类框架下沉积趋势以及液塑极限的影响。沉降试验和落锥试验在七种不同的离子浓度(c = 1 × 10~(-5) ~ 1.8 M)和四种目标pH值(pH = 3,5,7和9)下进行。在孔隙流体的不同离子浓度和pH条件下,观察到絮凝、分散和混合(c = 0.0015至0.003 M)三种不同的沉降趋势。根据沉降曲线定义了三个沉降参数,分别命名为A_1、A_2和A_3。它们之间的关系暗示了测试粘性土壤沉积趋势的显着特征。这些参数证实了观察到的沉降模式和临界离子浓度;对于AMK和EPK(高比表面积),c*~3×10~(-3)M,对于LKW和MI(低比表)的c*~1.5×10~(-3)M,其中织物发生了明显的变化。在新的分类图中,高比表粘土被归类为中等电敏粘土,而低比表粘土被归类为低电敏细粉。对沉积参数和新细粒分类图的补充数据分析表明,新细粒分类图中捕获的不同沉积趋势与黏土颗粒显著特征之间的稳健联系有助于预测不同孔隙流体化学的黏土沉降模式。

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