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Effect of Compaction Degree on Solidification Characteristics of Pb-Contaminated Soil Treated by Cement

机译:压实度对水泥处理的铅污染土壤固化特性的影响

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摘要

Compaction is a necessary step after the solidification/stabilization of contaminated soil. This study analyzed the effect of compaction degree on the solidification characteristics of Pb-contaminated soil. Batch tests were conducted to measure the permeability coefficient, unconfined compressive strength, Pb leaching concentration, and micromorphology of the solidified bodies compacted at different degrees (from 0.90 to 1.00 at an interval of 0.02). The permeability coefficient of the solidified bodies decreased with the increase in penetration time and compaction degree (from 1.80 × 10−6 to 1.19 × 10−7 cm/s). With an increase in compaction degree, the unconfined compressive strength of the solidified bodies increased from 2.20 to 4.90 MPa. In addition, failure strain decreased first and then increased before and after the compaction degree reached approximately 0.95. Pb in soil was effectively stabilized by cement because the leaching concentration of Pb in all the samples was <2.5 mg/L. The leaching concentration of Pb increased first and then decreased before and after the compaction degree reached approximately 0.96, but pH values of lixivium decreased first and then increased. Compaction degree and the hydration products jointly determined the pore distribution and microscopic morphology of the solidified bodies, which comprised intra-particle, inter-particle, and intra-aggregate pores. The hydration products in the solidified bodies mainly consisted of ettringite and C–S–H. Low compaction degree was found to be beneficial for the formation of hydration products, the content and distribution of which jointly determined the leaching concentration of Pb.
机译:压实是固化/稳定受污染土壤之后的必要步骤。本研究分析了压实度对铅污染土壤固化特性的影响。进行批处理测试以测量渗透系数,无侧限抗压强度,Pb浸出浓度以及不同程度压实的凝固体的微观形态(从0.90到1.00,间隔为0.02)。凝固体的渗透系数随渗透时间和压实度的增加而降低(从1.80××10-6到1.19××10-7-7cm / s)。随着压实度的增加,凝固体的无侧限抗压强度从2.20增加到4.90 MPa。另外,在压实度达到约0.95之前和之后,破坏应变先减小然后增加。土壤中的铅通过水泥有效地稳定,因为所有样品中铅的浸出浓度均<2.5 mg / L。在压实度达到约0.96之前和之后,铅的浸出浓度先升高然后降低,而浸膏的pH值先降低然后升高。压实度和水合产物共同决定了凝固体的孔隙分布和微观形貌,其中包括颗粒内,颗粒间和聚集体内部的孔。凝固体中的水合产物主要由钙矾石和C–H–H组成。发现低压实度有利于水合产物的形成,水合产物的含量和分布共同决定了铅的浸出浓度。

著录项

  • 来源
    《Clean》 |2014年第8期|1-7|共7页
  • 作者单位

    State Key Laboratory of Geomechanics and Geotechnical Engineering Institute of Rock and Soil Mechanics Chinese Academy of Sciences Hubei P. R. China;

    State Key Laboratory of Geomechanics and Geotechnical Engineering Institute of Rock and Soil Mechanics Chinese Academy of Sciences Hubei P. R. China;

    State Key Laboratory of Geomechanics and Geotechnical Engineering Institute of Rock and Soil Mechanics Chinese Academy of Sciences Hubei P. R. China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Compaction degree; Leaching concentration; Pb-contaminated soil; Permeability coefficient; Solidification/stabilization;

    机译:压实度;浸出浓度;Pb污染土壤;渗透系数;固溶/稳定;

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