碳化作用
多孔性
材料科学
水银孔隙仪
抗压强度
含水量
堆积密度
硅酸盐水泥
碳化
比重
水分
扫描电子显微镜
矿物学
复合材料
水泥
岩土工程
土壤水分
化学
地质学
土壤科学
多孔介质
作者
Yaolin Yi,Kaiwen Lu,Songyu Liu,Abir Al‐Tabbaa
标识
DOI:10.1139/cgj-2015-0135
摘要
A reactive magnesia (MgO) was used to stabilize a natural soil; the MgO-stabilized soil was subjected to forced carbonation with pressurized gaseous CO 2 in a triaxial cell set-up. The change of physical properties, including bulk density, moisture content, dry density, specific gravity, and porosity, of the stabilized soil during carbonation was studied. The mechanical and microstructural properties of the carbonated MgO-stabilized soil were also investigated through unconfined compressive strength (UCS) test, X-ray diffraction analysis (XRD), scanning electron microscopy (SEM), and mercury intrusion porosimetry (MIP). The results indicated that the carbonation of MgO-stabilized soil consumed CO 2 and water, and produced expansive carbonation products; this consequently increased the dry density, and reduced the moisture content, specific gravity, and porosity of the stabilized soil. After being carbonated for only 1.5 h, the MgO-stabilized soil yielded remarkable strength, with UCS higher than that of the 28 day ambient cured Portland cement–stabilized soil, mainly due to the high binding effect of carbonation products and the low porosity of carbonated MgO-stabilized soil. The carbonated MgO-stabilized soil achieved a high degree of carbonation in a few hours (≤12 h), with the maximum CO 2 /MgO ratio in a range of 0.76–1.07.
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