ZHENG Juan, WU Xiao, LAI Xiuying, CHEN Shuo. Experimental Study on Micro Deformation Characteristics of Remolded Saturated Cohesive Soil at Different Loading Rates[J]. INDUSTRIAL CONSTRUCTION, 2022, 52(4): 122-125,73. doi: 10.13204/j.gyjzG21021603
Citation:
ZHENG Juan, WU Xiao, LAI Xiuying, CHEN Shuo. Experimental Study on Micro Deformation Characteristics of Remolded Saturated Cohesive Soil at Different Loading Rates[J]. INDUSTRIAL CONSTRUCTION, 2022, 52(4): 122-125,73. doi: 10.13204/j.gyjzG21021603
ZHENG Juan, WU Xiao, LAI Xiuying, CHEN Shuo. Experimental Study on Micro Deformation Characteristics of Remolded Saturated Cohesive Soil at Different Loading Rates[J]. INDUSTRIAL CONSTRUCTION, 2022, 52(4): 122-125,73. doi: 10.13204/j.gyjzG21021603
Citation:
ZHENG Juan, WU Xiao, LAI Xiuying, CHEN Shuo. Experimental Study on Micro Deformation Characteristics of Remolded Saturated Cohesive Soil at Different Loading Rates[J]. INDUSTRIAL CONSTRUCTION, 2022, 52(4): 122-125,73. doi: 10.13204/j.gyjzG21021603
The remolded saturated cohesive soil with the same initial state was consolidated at different loading rates, and the specimens were measured by nuclear magnetic resonance (NMR) in different loading stages. And then the relation of transverse relaxation time T2 distribution or T2 spectrum area change with porosity was qualitatively analyzed to study its microscopic response of deformation.The results showed that the T2 spectrum of saturated remolded cohesive soil in the initial stage of consolidation was consisted of two peaks. With the development of consolidation, the large pores gradually closed to small pores, and the final T2 spectrum turned out to be a single peak; for faster loading soil specimens influenced by lagging of drainage at the beginning of loading,the change trend of the T2 spectrum was not obvious.And after a long time of constant loading, the final shape for the T2 spectrum of the soil specimens was very similar regardless of the loading rate.It indicated that the loading rate only influenced the intermediate state of the soil specimens, the final state was dominated by the initial state of the specimens.
TIAN H H,WEI C F,WEI H Z,et al.Freezing and thawing characteristics of frozen soils:bound water content and hysteresis phenomenon[J].Cold Regions Science and Technology,2014,103:74-81.
AN R,KONG L W,LI C S.Pore distribution characteristics of thawed residual soils in artificial frozen-wall using NMRI and MIP measurements[J].Applied Sciences,2020,10(2):544.