ZHANG Wen-bo, BAI Wei, KONG Ling-wei, et al. Effect of leaching time on physical and mechanical
characteristics of lateritic soil[J]. 2022, 43(2): 443-452.
ZHANG Wen-bo, BAI Wei, KONG Ling-wei, et al. Effect of leaching time on physical and mechanical
characteristics of lateritic soil[J]. 2022, 43(2): 443-452.DOI: 10.16285/j.rsm.2021.1401.
Taking the lateritic soil collected from Miaoling town
Ezhou city
Hubei province as the study object
the free iron oxide in the undisturbed clay was removed by chemical selective dissolution combined with leaching as the treatment method in gradient
and the relationship between the drenching time of dithionite-citrate-bicarbonate (DCB) solution and the iron removal rate was achieved
and the effects of different leaching times on the physical
mechanical properties and the microscopic pore structure of the lateritic soil were analyzed. The experimental results show that the leaching time of DCB solution has a strong correlation with the iron removal rate
and the iron removal rate first increases rapidly and then gradually stabilizes with the time. Since the free iron oxide primarily plays the role of cementation between lateritic soil
the drenching time has a great influence on the physical and mechanical properties of lateritic soil. With the increase of drenching time
the contents of clay particles and colloidal particles gradually increase
the heat resistance increases marginally
and the unconfined compressive strength decreases significantly
while the overall trend of unconfined compressive strength decreases sharply in the early stage and tends to be stable in the later stage. Results of nuclear magnetic resonance (NMR)
differential thermal analysis (DTA) and scanning electron microscopy (SEM) reveal that as the leaching time increases
the internal pores of the Miaoling lateritic soil enlarge
the free water diminishes
the bound water increases
the microscopic morphology of the agglomerate structure is destroyed
the cemented material is significantly reduced
and the structural form gradually converts from a compact granule stacking structure to an aggregate-loose granular structure.