首页> 外文会议>The proceedings of the eighteenth (2008) international offshore and polar engineering conference (ISOPE-2008) >Calcium Leaching Properties of Lime-treated Soil by Infiltration of Tidal River Water
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Calcium Leaching Properties of Lime-treated Soil by Infiltration of Tidal River Water

机译:潮水渗入石灰处理过的土壤中钙的浸出特性

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At present, the leakage is found in foundation of the dike constructed 20 years ago. The dike is constructed along the river in which directly connect to the Ariake Sea surrounded by a vast flat coastal area with very large tidal range. The Ariake clay and lime admixture were used as a main material for the foundation of the dike. The sludge material was found on the surface of lime-treated soil at the leaking point. This condition could weaken the treated soil in the foundation, and subsequently reduce the stability of the dike. In this study, in order to verify the cause of sludge materials leach from lime-treated soil, both water quality analysis in the field and two leaching test (solvent: NaCl and H_2O_2) at the laboratory were performed. There is tendency of Ca~(2+) leach from lime-treated soil due to the high concentration of NaCl and H_2O_2 solvent. The results indicated that the infiltration of tidal river water to the lime-treated soil induces increasing in the leaching of Ca~(2+) in which could reduce the strength of the treated soil.
机译:目前,泄漏是在20年前建造的堤坝的基础上发现的。堤坝沿河而建,在河中直接与有明海沿岸广阔的平坦沿海地区包围的有明海相连。 Ariake粘土和石灰混合物被用作堤坝基础的主要材料。在泄漏点的石灰处理过的土壤表面发现了污泥物质。这种情况可能会削弱地基中处理过的土壤,从而降低堤防的稳定性。在这项研究中,为了验证污泥材料从石灰处理过的土壤中渗出的原因,在实验室中进行了现场水质分析和两次浸出试验(溶剂:NaCl和H_2O_2)。由于高浓度的NaCl和H_2O_2溶剂,从石灰处理的土壤中存在Ca〜(2+)浸出的趋势。结果表明,潮水渗入石灰处理过的土壤中导致Ca〜(2+)的淋溶增加,从而降低了处理过的土壤的强度。

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