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Mitigation of Alkali Induced Heave in Rectorite Soil with Fly Ash

机译:粉煤灰缓解累积土中碱引起的隆起。

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Mechanisms that control the volume changes behavior of foundation soils are well understood. The changes that occur in the behavior of soil due to migration of pollutants are not well understood. The extent of changes that occur in the presence of small concentration of contaminants can be predicted based on changes in the thickness of double layer and associated fabric changes. Interactions that occur with strong contaminants depends on the type of soil, type and concentration of contamination and duration of interaction etc It has been shown that different concentrations (1N and 4N) of sodium hydroxide solution causes abnormal changes on volume change behaviour of soil due to mineralogical changes. An attempt is made in this paper to stabilize contaminated soil using fly ash, after establishing its stability in alkali solutions. It was found that the effectiveness of fly ash to control the alkali induced heave increases with fly ash content incorporated into the soil. X-ray diffraction studies reveal that the mineralogical changes that occur in soil due to alkali interaction are inhibited by the presence of fly ash.
机译:控制基础土壤体积变化行为的机理已广为人知。由于污染物的迁移,土壤行为发生的变化尚不十分清楚。可以基于双层厚度的变化和相关的织物变化来预测在存在低浓度污染物的情况下发生的变化的程度。与强污染物发生的相互作用取决于土壤的类型,污染物的类型和浓度以及相互作用的持续时间等。研究表明,不同浓度(1N和4N)的氢氧化钠溶液会导致土壤体积变化行为的异常变化,原因是矿物学变化。在建立粉煤灰在碱溶液中的稳定性之后,本文尝试使用粉煤灰稳定被污染的土壤。已经发现,粉煤灰控制碱诱导的升沉的有效性随掺入土壤中的粉煤灰含量的增加而增加。 X射线衍射研究表明,由于碱相互作用而在土壤中发生的矿物学变化受到粉煤灰的存在的抑制。

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