2021
DOI: 10.1007/s12205-021-1247-7
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Physio-Chemical Properties, Consolidation, and Stabilization of Tropical Peat Soil Using Traditional Soil Additives — A State of the Art Literature Review

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Cited by 19 publications
(14 citation statements)
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“…The observed strength enhancement due to SF may be associated with the formation of calcium silicate hydrate (C–S–H) gel and calcium silicate (CS) [ 7 , 52 ], while the combined effect of SF and OPC may be associated with the formation of calcium silicate (CS) and hydrated components as a result of hydration, i.e., calcium aluminate hydrate (C–A–H), calcium silicate hydrate (C–S–H) gel, and AFt formation. [ 1 ]. Moreover, the development of greater interfacial confinement bonding, roughness, contact area, and friction mobilization upon the loading of the stabilized peat yielded higher CBR values [ 53 ].…”
Section: Resultsmentioning
confidence: 99%
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“…The observed strength enhancement due to SF may be associated with the formation of calcium silicate hydrate (C–S–H) gel and calcium silicate (CS) [ 7 , 52 ], while the combined effect of SF and OPC may be associated with the formation of calcium silicate (CS) and hydrated components as a result of hydration, i.e., calcium aluminate hydrate (C–A–H), calcium silicate hydrate (C–S–H) gel, and AFt formation. [ 1 ]. Moreover, the development of greater interfacial confinement bonding, roughness, contact area, and friction mobilization upon the loading of the stabilized peat yielded higher CBR values [ 53 ].…”
Section: Resultsmentioning
confidence: 99%
“…Histosol, moss, bogs, fen, and mires are widely classified as peat soil that originates from the anaerobic decaying of plants and animals. Peat soil is considered the most undesirable base material for any sort of construction activity [ 1 ]. The poor engineering properties associated with peatland, i.e., high water content and high void ratio, result in low shear strength and compressible behavior, making it unable to bear infrastructure loads.…”
Section: Introductionmentioning
confidence: 99%
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“…Generally, the average liquid limit for peat varies from 200 to 600% in the tropical region, while for bog peat, it is in the range of 800 to 1500 % [16], [17]. The liquid limit of tropical peat soil in Malaysia ranges from 130 % to 400% [18], [19], while [20] stated that the liquid limit for peat soil is 149% and 162%.…”
Section: Liquid Limitmentioning
confidence: 99%
“…The organic content of various peat soil types varies in the range of (25-98.46%) [17]. The organic content of Malaysian peat soils ranges from 70% to 98% [26][27][28]19].…”
Section: Organic Contentmentioning
confidence: 99%