FLY ASH STABILIZED LATERITIC SOIL AS SUBBASE MATERIAL: A REVIEW

N. N. Nik Daud, Mohammad Aliff Rusdi
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Abstract

The aim of this review is to gain insights of the geotechnical properties of lateritic soil that make it suitable to be used as a subbase material, and discuss the improvements done on the properties to further strengthen them. Several additives are reviewed for the lateritic soil stabilization, and fly ash is chosen to be the material of interest. This is so to answer the problem statement of would fly ash be a potential material for soil stabilization. Based on this review, it is understood that lateritic soil is commonly found in tropical and subtropical regions and is classified as sandy clay or silty clay. Studies also have shown that fly ash is potential to be used as a stabilizer in soil improvements. The presence of free lime may react with the silicates and aluminates, resulting to a long-term strength gain in soil. Class C fly ash contains more free lime that would lead to better strength gain in the earlier stage as compared to Class F fly ash. In addition to that, the particle size of the fly ash would also affect the improvement results, as smaller particle size allows more effective surface for the pozzolanic reaction to occur. The significance of this review is to show the potential of fly ash in improving lateritic soil, other than providing more evidence to encourage the incorporation of industrial waste in soil stabilization.
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粉煤灰稳定红土底基材料研究进展
本综述的目的是了解红土土的岩土力学特性,使其适合用作底基材料,并讨论对其性能的改进,以进一步加强它们。综述了几种用于红土稳定的添加剂,并以粉煤灰为研究对象。这就回答了粉煤灰是否有可能成为土壤稳定材料的问题。在此基础上,了解到红土土普遍存在于热带和亚热带地区,可分为砂质粘土或粉质粘土。研究还表明,粉煤灰有潜力用作土壤改良中的稳定剂。游离石灰的存在可能与硅酸盐和铝酸盐发生反应,从而使土壤的长期强度增加。C类粉煤灰含有较多的游离石灰,较F类粉煤灰具有较好的前期强度增益。此外,粉煤灰的粒径也会影响改善效果,粒径越小,火山灰反应发生的有效表面越多。本综述的意义在于表明粉煤灰在改善红土中的潜力,而不是为鼓励工业废物掺入土壤稳定提供更多证据。
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