Estimation of Groundwater Recharge from Precipitation and Evapotranspiration by Lysimeter Measurement and Soil Moisture Model-Reference-Cited by-同舟云学术

Estimation of Groundwater Recharge from Precipitation and Evapotranspiration by Lysimeter Measurement and Soil Moisture Model

Published:2008-05 Issue:5 Volume:13 Page:333-340
ISSN:1084-0699
Container-title:Journal of Hydrologic Engineering
language:en
Short-container-title:J. Hydrol. Eng.

Author:

Chen Xi¹²³⁴⁵,Zhang Zhi-Cai¹²³⁴⁵,Zhang Xin-Nan¹²³⁴⁵,Chen Yong-Qin¹²³⁴⁵,Qian Ming-Kai¹²³⁴⁵,Peng Shun-Feng¹²³⁴⁵

Affiliation:

1. Professor, State Key Laboratory of Hydrology, Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098, China (corresponding author). E-mail: xichen@hhu.edu.cn

2. Ph.D. Student, State Key Laboratory of Hydrology, Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098, China.

3. Professor, State Key Laboratory of Hydrology, Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098, China.

4. Associate Professor, Dept. of Geography and Resource Management, The Chinese Univ. of Hong Kong, Hong Kong.

5. Senior Engineer, The Bureau of Hydrology, Huaihe River Commission, Bengbu, Anhui 233001, China.

Publisher

American Society of Civil Engineers (ASCE)

Subject

General Environmental Science,Water Science and Technology,Civil and Structural Engineering,Environmental Chemistry

Link

http://ascelibrary.org/doi/pdf/10.1061/%28ASCE%291084-0699%282008%2913%3A5%28333%29

Reference23 articles.

1. Allen R. G. Howell T. A. Pruitt W. O. Walter I. A. and Jensen M. E. eds. (1991). “Lysimeters for evapotranspiration and environmental measurements.” Proc. Int. Symp. on Lysimetry ASCE New York.

2. Testing a full-range soil-water retention function in modeling water potential and temperature

3. Infiltration into a class of vertically non-uniform soils

4. Evaporation into the Atmosphere

5. Coupling an Advanced Land Surface–Hydrology Model with the Penn State–NCAR MM5 Modeling System. Part I: Model Implementation and Sensitivity

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