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- W71282095 abstract "From the discussion, it can be concluded that residual soils, or at least those of granite origin, behave like overconsolidated soils with their preconsolidation pressures predominately controlled by the interparticle bonding and consequently the degree of weathering. As the material becomes more weathered, the primary bonding is gradually destroyed or partially replaced by the secondary bonding which deteriorates upon soaking. For soils with low degree of weathering the primary bonding effect predominates and the preconsolidation pressure could be extremely high. Thus, they should be treated as rocks. For soils with high degree of weathering and predominantly secondary bonding effect, their preconsolidation pressures vary with the degree of weathering. They can be treated as overconsolidated soils with their behaviour greatly influenced by soaking which acts like weathering in reducing the preconsolidation pressure of the soil.(A) For the covering abstract see IRRD 820605." @default.
- W71282095 created "2016-06-24" @default.
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- W71282095 date "1990-01-01" @default.
- W71282095 modified "2023-09-26" @default.
- W71282095 title "WRITTEN DISCUSSION: PRECONSOLIDATION OF RESIDUAL SOILS. GEOMECHANICS IN TROPICAL SOILS. PROCEEDINGS OF THE SECOND INTERNATIONAL CONFERENCE ON GEOMECHANICS IN TROPICAL SOILS, SINGAPORE, 12-14 DECEMBER 1988. VOLUME 2" @default.
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