Ching-Sheng Huang

Prof. Ching-Sheng Huang

College of Hydrology and Water Resources, Hohai University, Nanjing, China

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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1 June 2018 in Ecological Indicators
Verified
Journal Article
Open access
ZLZhenya Li
Zhenya Li
TYTao Yang
Tao Yang
Ching-Sheng HuangChing-Sheng Huang
Ching-Sheng Huang
Chong-Yu XuChong-Yu Xu
Chong-Yu Xu
QSQuanxi Shao
Quanxi Shao
TCTong Cui
Tong Cui

1 June 2018 in Journal of Hydrology
Verified
Journal Article
Closed access
Ching-Sheng HuangChing-Sheng Huang
Ching-Sheng Huang
TYTao Yang
Tao Yang
HYHund-Der Yeh
Hund-Der Yeh

9 June 2018 in Stochastic Environmental Research and Risk Assessment
Verified
Journal Article
Closed access
PDF file
WRWeiwei Ren
Weiwei Ren
TYTao Yang
Tao Yang
Ching-Sheng HuangChing-Sheng Huang
Ching-Sheng Huang
Chong-Yu XuChong-Yu Xu
Chong-Yu Xu
QSQuan Xi Shao
Quan Xi Shao

11 October 2010 in Hydrology and Earth System Sciences
Verified
Journal Article
Open access
PDF file
MCM.-H. Chuang
M.-H. Chuang
Ching-Sheng HuangChing-Sheng Huang
Ching-Sheng Huang
GLG.-H. Li
G.-H. Li
HYHund-Der Yeh
Hund-Der Yeh
In the past, the coastal leaky aquifer system, including two aquifers and an aquitard between them, was commonly assumed to be homogeneous and of infinite extent in the horizontal direction. The leaky aquifer system may however be heterogeneous and of finite extent due to variations in depositional and post depositional processes. In this paper, the leaky aquifer system is divided into several horizontal regions for the heterogeneous aquitard and underlying aquifer. A one-dimensional analytical model is developed for describing the head fluctuation in such a heterogeneous leaky aquifer system. The hydraulic head of the upper unconfined aquifer is assumed constant. It is found that both the length and location of the discontinuous aquitards presented in the coastal area have significant effects on the amplitude and phase shift of the head fluctuation in the lower aquifer. In addition, the influence of the formation heterogeneity on the spatial head distribution is also investigated.

1 May 2011 in Advances in Water Resources
Verified
Journal Article
Closed access
Ching-Sheng HuangChing-Sheng Huang
Ching-Sheng Huang
YCYu-Lin Chen
Yu-Lin Chen
HYHund-Der Yeh
Hund-Der Yeh

7 May 2019 in Water Resources Research
Verified
Journal Article
Open access
PDF file
YLYe‐Chen Lin
Ye‐Chen Lin
Ching-Sheng HuangChing-Sheng Huang
Ching-Sheng Huang
HYHund-Der Yeh
Hund-Der Yeh
This study proposes a new mathematical model for describing the drawdown distribution due to a constant rate pumping (CRP) in an unconfined aquifer considering the lagging theory. We introduce two lag times in Darcy's law and in turn in a free surface equation to reflect the effects of the capillary fringe and the capillary suction on the water table motion. The present free surface equation can reduce to those used in previous studies. The Laplace and Weber transform methods are used to derive the semianalytical solution to the model including the effect of wellbore storage. The algorithm of numerical Laplace inversion is applied to obtain the transient solution of the model. We find that the delay index, commonly used in the literature, is equivalent to the lag time associated with the effect of the capillary suction. The sensitivity analysis is performed to assess the drawdown behavior in response to the change in each aquifer parameter. The drawdown distributions predicted by the present solution agree fairly well to the field data taken from CRP tests at Cape Cod, Massachusetts; the Canadian Forces Base Borden, Ontario; and Saint Pardon de Conques, Gironde (France). The lag times determined by both CRP tests seem to decrease linearly with increasing distance on the logarithmic scale from the pumping well. The consideration of two lag times considerably improves the accuracy in estimated specific yields.