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Experimental investigation of solidifying desert aeolian sand using microbially induced calcite precipitation

机译:微生物诱导方解石沉淀固化沙漠风沙的实验研究

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In this study, five different concentrations of solidification solution (0.5, 1.0, 1.5, 2.0 and 2.5 mol/L urea-CaCl2) were used to solidify desert aeolian sand by microbially induced calcite precipitation (MICP). As the concentration of solidification solution increased, the CaCO3 content increased, sand density increased, permeability was reduced and the unconfined compressive strength increased. Formation of CaCO3 was the primary cause of changes in the sand's properties. Specifically, CaCO3 filled the pores between the sand particles and the pore volume decreased. The CaCO3 formed in response to low concentrations (i.e., 0.5-1.0 mol/L) and high concentrations (i.e., 1.5-2.5 mol/L) of urea-CaCl2 solution played different roles in solidification of the structures. (C) 2018 Elsevier Ltd. All rights reserved.
机译:在这项研究中,使用五种不同浓度的固化溶液(0.5、1.0、1.5、2.0和2.5 mol / L尿素-CaCl2)通过微生物诱导的方解石沉淀(MICP)固化沙漠风沙。随着固化溶液浓度的增加,CaCO3含量增加,砂粒密度增加,渗透率降低,无侧限抗压强度增加。 CaCO3的形成是改变砂子性质的主要原因。具体地,CaCO 3填充砂粒之间的孔,并且孔体积减小。响应于低浓度(即0.5-1.0 mol / L)和高浓度(即1.5-2.5 mol / L)的尿素-CaCl2溶液而形成的CaCO3在结构固化中起着不同的作用。 (C)2018 Elsevier Ltd.保留所有权利。

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