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Freeze-Thaw Performance of Silt Sand Treated with Lignin

机译:用木质素治疗的淤泥沙子的冻融性能

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In cold regions, freeze-thaw action poses a significant hazard to road engineering. In order to avoid the adverse effects of inorganic materials on soil modification, we applied lignin, which is an environmentally friendly and organic polymer, to improve the silt sand from cold regions. The significance of this study is to facilitate the better application of lignin. The macroscopic engineering properties of the soil showed that, before freeze-thaw, as the lignin content increased, thermal conductivity and permeability decreased, pH first increased rapidly and then stabilized between 10 and 11, and dynamic resilient modulus first increased then decreased; after freeze-thaw, as lignin content increased, thermal conductivity and permeability decreased, and dynamic resilient modulus first increased then decreased. The freeze-thaw action reduced the thermal conductivity and dynamic resilient modulus of silt sand treated with lignin and increased its permeability. The test results of soil microstructure indicated that, before freeze-thaw, the silt sand and silt sand treated with lignin were structurally compact; after freeze-thaw, the silt sand showed numerous cracks and pores and had a loose soil structure, whereas the silt sand treated with lignin showed fewer cracks and pores, and its soil structure was more compact under the encapsulation and filling action of cementitious materials. No new chemical elements, mineral components, or functional groups were produced when lignin was mixed with silt sand. The mechanism by which lignin improved the macroengineering properties of silt sand involved the cementitious material produced by the interaction between lignin and soil minerals, which encapsulated the soil particles and filled the interparticle pores. Research results can provide a theoretical reference for engineering application of lignin in cold regions.
机译:在寒冷地区,冻融作用对道路工程构成了重大危害。为了避免无机材料对土壤改性的不利影响,我们应用木质素,即环保和有机聚合物,改善来自寒冷地区的淤泥砂。本研究的重要性是促进更好地应用木质素。土壤的宏观工程性质表明,在冻融之前,随着木质素含量的增加,导热性和渗透性降低,pH首先迅速增加,然后在10和11之间稳定,然后动态弹性模量首先增加然后减少。在冻融后,随着木质素含量的增加,导热性和渗透率降低,动态弹性模量首先增加,然后减少。冻融作用降低了用木质素处理的淤泥砂的导热性和动态弹性模量,增加了其渗透性。土壤微观结构的测试结果表明,在冻融之前,用木质素处理的淤泥沙子和淤泥砂在结构紧凑;冻融后,淤泥沙子显示出众多裂缝和毛孔,具有松散的土壤结构,而用木质素处理的淤泥砂孔显示出较少的裂缝和毛孔,并且在胶凝材料的包封和填充作用下,其土壤结构更紧凑。当木质素与淤泥沙子混合时,不会产生新的化学元素,矿物成分或官能团。木质素改善淤泥砂的大型工艺的机制涉及通过木质素和土壤矿物质之间的相互作用产生的水泥质材料,其封装土壤颗粒并填充颗粒孔。研究结果可以为寒冷地区的木质素应用提供理论参考。

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