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Laboratory-prepared iron oxide coatings on sands: Submicron-scale small-strain stiffness

机译:实验室在沙子上制备的氧化铁涂层:亚微米级小应变刚度

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Chemical weathering of iron-bearing rock minerals results in the formation of iron oxides, which can chemically adsorb onto soil surfaces, and/or absorb into their molecular structure. The objective of this paper is to use laboratory-prepared, iron oxide-coated sand to study the role of iron oxide coatings on the smallstrain stiffness of coarse-grained soil. Ottawa sands were geochemically coated with iron oxides of goethite and hematite via a heterogeneous suspension reaction in the laboratory. Specimen preparation techniques were chosen to ensure that the soils were not cemented during preparation. SEM images, ICP analysis, and geotechnical index tests were used to characterize the submicron-scaled iron oxide coatings, and the bender element method was used to measure the shear wave velocities of uncoated and the two iron oxide coated sands. Contact mechanics and submicron scale mechanistic approaches were explored to interpret the experimental data, and results indicated that small-strain stiffness of iron oxide coated sands was higher than that of uncoated sands. Results also suggested that a small-strain stiffness behavioral hierarchy associated with iron oxide thermodynamic stability may exist. This study demonstrated that iron oxide coatings significantly influence sand grain-to-grain behavior, even in the absence of cementation or augmented contact area effects, due to an increase in the number of particle contacts present in the iron oxide coated sands.
机译:含铁岩石矿物的化学风化导致形成氧化铁,这些氧化铁可以化学吸附到土壤表面和/或吸收到其分子结构中。本文的目的是使用实验室制备的氧化铁涂层砂来研究氧化铁涂层对粗粒土小应变刚度的作用。在实验室中,渥太华砂通过针状和赤铁矿的非均相悬浮反应被地球化学覆盖。选择标本制备技术以确保在制备过程中不将土壤胶结。使用SEM图像,ICP分析和岩土工程指标测试来表征亚微米级氧化铁涂层,并使用弯管元法测量未涂覆砂岩和两种涂覆氧化铁砂的剪切波速度。探索了接触力学和亚微米尺度机理来解释实验数据,结果表明,氧化铁涂层砂的小应变刚度高于未涂层砂。结果还表明,可能存在与氧化铁热力学稳定性相关的小应变刚度行为等级。这项研究表明,由于存在氧化铁涂层的沙子中存在的颗粒接触数量增加,即使在没有胶结或接触面积增加的情况下,氧化铁涂层也会显着影响砂子的晶粒行为。

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