En-long Liu

Prof. En-long Liu

orcid

Research Focus & Metrics

Academic Career Length

17Years (2010-Present)

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

Representative Publications

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HAHilal Ahmad
Hilal Ahmad
NCNing-shen CHEN
Ning-shen CHEN
Mahfuzur RahmanMahfuzur Rahman
Mahfuzur Rahman
DIDr. Md. Monirul Islam
Dr. Md. Monirul Islam
Hamid Reza PourghasemiHamid Reza Pourghasemi
Hamid Reza Pourghasemi
Ashraf DewanAshraf Dewan
Ashraf Dewan
The China–Pakistan Economic Corridor (CPEC) project passes through the Karakoram Highway in northern Pakistan, which is one of the most hazardous regions of the world. The most common hazards in this region are landslides and debris flows, which result in loss of life and severe infrastructure damage every year. This study assessed geohazards (landslides and debris flows) and developed susceptibility maps by considering four standalone machine-learning and statistical approaches, namely, Logistic Regression (LR), Shannon Entropy (SE), Weights-of-Evidence (WoE), and Frequency Ratio (FR) models. To this end, geohazard inventories were prepared using remote sensing techniques with field observations and historical hazard datasets. The spatial relationship of thirteen conditioning factors, namely, slope (degree), distance to faults, geology, elevation, distance to rivers, slope aspect, distance to road, annual mean rainfall, normalized difference vegetation index, profile curvature, stream power index, topographic wetness index, and land cover, with hazard distribution was analyzed. The results showed that faults, slope angles, elevation, lithology, land cover, and mean annual rainfall play a key role in controlling the spatial distribution of geohazards in the study area. The final susceptibility maps were validated against ground truth points and by plotting Area Under the Receiver Operating Characteristic (AUROC) curves. According to the AUROC curves, the success rates of the LR, WoE, FR, and SE models were 85.30%, 76.00, 74.60%, and 71.40%, and their prediction rates were 83.10%, 75.00%, 73.50%, and 70.10%, respectively; these values show higher performance of LR over the other three models. Furthermore, 11.19%, 9.24%, 10.18%, 39.14%, and 30.25% of the areas corresponded to classes of very-high, high, moderate, low, and very-low susceptibility, respectively. The developed geohazard susceptibility map can be used by relevant government officials for the smooth implementation of the CPEC project at the regional scale.

19 February 2020 in Acta Geotechnica
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Younegn LIUYounegn LIU
Younegn LIU
ELEn-long Liu
En-long Liu
ZYZhenyu Yin
Zhenyu Yin

20 June 2017 in International Journal of Civil Engineering
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TCTie Lin Chen
Tie Lin Chen
CZCheng Zhou
Cheng Zhou
GWGuo-Li Wang
Guo-Li Wang
ELEn-long Liu
En-long Liu
Feng DaiFeng Dai
Feng Dai

24 February 2023 in Acta Geotechnica
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DWDan Wang
Dan Wang
ELEn-long Liu
En-long Liu
CYChengsong Yang
Chengsong Yang
PWPan Wang
Pan Wang
BSBingtang Song
Bingtang Song

4 August 2020 in Acta Mechanica
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JTJianqiu Tian
Jianqiu Tian
ELEn-long Liu
En-long Liu
CHChuan He
Chuan He

30 March 2022 in Scientific Reports
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BXBo Xiang
Bo Xiang
ELEn-long Liu
En-long Liu
LYLiuxin Yang
Liuxin Yang
Freezing–thawing actions can affect the mechanical features of soil greatly, which is vital for the stability of soil slope in cold regions. Firstly, triaxial compression tests on sand samples under undrained conditions were performed to investigate the influences of freezing–thawing cycles, which shows that the freezing–thawing actions can weaken their strength and stiffness, and with the increasing freezing–thawing cycles, both the deviatoric stress and pore water pressure decrease gradually. Then, the double hardening constitutive model was revised to model the influences of freezing–thawing cycles in consideration of the influences of freezing–thawing actions, and the model was also validated by the test results. Finally, the proposed constitutive model was incorporated into a finite element code to numerically simulate the distribution of displacement and pore water pressure of sand slope subjected to freezing–thawing cycles, which shows that the freezing–thawing actions accelerate the dissipation of the pore water pressure and enlarge the displacement of the slope. The study here can provide a help in designing and construction of civil engineering in cold regions.