Lingwei Kong

Prof. Lingwei Kong

Institute of Rock and Soil Mechanics, Chinese Academy of Sciences
orcid

Research Focus & Metrics

Academic Career Length

26Years (2001-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 October 2013 in Journal of Rock Mechanics and Geotechnical Engineering
Verified
Journal Article
Open access
WBWei Bai
Wei Bai
LKLingwei Kong
Lingwei Kong
AGAiguo Guo
Aiguo Guo
Natural soils of various types have different electrical properties due to the composition, structure, water content, and temperature. In order to investigate the electrical properties of lateritic soil, electrical conductivity experiments have been conducted on a self-developed testing device. Test results show that the electrical conductivity of laterite increases with the increase of water content, degree of saturation and dry density. When the water content is below the optimum water content, the electrical conductivity of soils increases nonlinearly and the variation rate increases dramatically. However, when the water content, degree of saturation, or dry density increases to a certain value, the electrical conductivity tends to be a constant. In addition, soil electrical conductivity increases with the increase of temperature, and it is observed that the electrical conductivity decreases with the increase of the number of wetting–drying cycles.

1 June 2022 in Journal of Rock Mechanics and Geotechnical Engineering
Verified
Journal Article
Open access
RARan An
Ran An
LKLingwei Kong
Lingwei Kong
XZXianwei Zhang
Xianwei Zhang
CLChengsheng Li
Chengsheng Li

1 February 2018 in Canadian Geotechnical Journal
Verified
Journal Article
Closed access
LKLingwei Kong
Lingwei Kong
HSHossain Md. Sayem
Hossain Md. Sayem
HTHuihui Tian
Huihui Tian
Due to the formational environment and climatic variability, granite residual soils with grain-size distribution ranging from gravel to clay undergo multiple drying–wetting cycles. The influences of multiple drying–wetting cycles on the soil-water characteristic curve (SWCC) and pore-size distribution (POSD) of undisturbed granite residual soils are investigated using the pressure plate test and nuclear magnetic resonance (NMR) spin-spin relaxation time (T2) distribution measurement, respectively. Results show that the water-retention capacity and air-entry value decrease and pores become more uniform with increasing drying–wetting cycles. After four drying–wetting cycles, the soil reaches a nearly constant state. The POSD change of multiple drying–wetting cycle samples is consistent with the SWCC of the soils. Furthermore, a modified van Genuchten model in terms of cumulative pore volume is used to obtain the best-fit POSD of the drying–wetting cycle samples. The shape and changing tendency of both curves of SWCC and POSD are quite similar and achieved a better correlation. It can be concluded that the SWCC is strongly dependent on the POSD of the soil and NMR T2 relaxometry can be used as an alternative to the assessment of microstructural variation of residual soils subjected to the periodic drying and wetting process.

7 August 2015 in Bulletin of Engineering Geology and the Environment
Verified
Journal Article
Closed access
PDF file
Xianwei ZhangXianwei Zhang
Xianwei Zhang
LKLingwei Kong
Lingwei Kong
XCX. L. Cui
X. L. Cui
SYS. Yin
S. Yin


1 February 2017 in Soils and Foundations
Verified
Journal Article
Open access
Xianwei ZhangXianwei Zhang
Xianwei Zhang
LKLingwei Kong
Lingwei Kong
AYA.W. Yang
A.W. Yang
HSH.M. Sayem
H.M. Sayem