Changes of Vertical Groundwater Recharge with Increase in Thickness of Vadose Zone Simulated by One-Dimensional Variably Saturated Flow Model

Siyuan Huo; Menggui Jin; Xing Liang; Dan Lin

doi:10.1007/s12583-014-0486-7

Volume 25 Issue 6

Dec 2014

Turn off MathJax

Article Contents

Journal of Earth Science > 2014 > 25(6): 1043-1050.

Siyuan Huo, Menggui Jin, Xing Liang, Dan Lin. Changes of Vertical Groundwater Recharge with Increase in Thickness of Vadose Zone Simulated by One-Dimensional Variably Saturated Flow Model. Journal of Earth Science, 2014, 25(6): 1043-1050. doi: 10.1007/s12583-014-0486-7

Citation:

Siyuan Huo, Menggui Jin, Xing Liang, Dan Lin. Changes of Vertical Groundwater Recharge with Increase in Thickness of Vadose Zone Simulated by One-Dimensional Variably Saturated Flow Model. Journal of Earth Science, 2014, 25(6): 1043-1050. doi: 10.1007/s12583-014-0486-7

Citation:

Siyuan Huo, Menggui Jin, Xing Liang, Dan Lin. Changes of Vertical Groundwater Recharge with Increase in Thickness of Vadose Zone Simulated by One-Dimensional Variably Saturated Flow Model. Journal of Earth Science, 2014, 25(6): 1043-1050. doi: 10.1007/s12583-014-0486-7

PDF( 502 KB)

Changes of Vertical Groundwater Recharge with Increase in Thickness of Vadose Zone Simulated by One-Dimensional Variably Saturated Flow Model

doi: 10.1007/s12583-014-0486-7

Siyuan Huo^{1, 2},
Menggui Jin^{1, 2
,
,},
Xing Liang^{1, 2},
Dan Lin^{1, 2, 3}

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
3.
Zhejiang Institute of Geology and Mineral Resource, Hangzhou 310007, China

More Information

Corresponding author: Menggui Jin, mgjin@cug.edu.cn
Received Date: 12 Dec 2013
Accepted Date: 02 Apr 2014
Publish Date: 01 Dec 2014

Abstract

Abstract

The thickness of vadose zone plays a critical role in vertical groundwater recharge. The decline of water table since the past decades due to long-term groundwater over-exploitation has resulted in deep vadose zone in North China Plain. One-dimensional variably saturated flow models were established by Hydrus-1D software and simulations were run under steady and continuous declining water table respectively to estimate the impact of increase in thickness of vadose zone on recharge process, quantity and recharge time. Luancheng area was selected to estimate recharge quantity considering steady and continuous declining water table. The simulation results show that the increase in thickness of vadose zone delays recharge process to water table. The recharge quantity decreases first and then remains stable with the decline of water table. Under the condition of declining water table, the evaluation of recharge by the flux at water table overestimates the recharge quantity. The average annual recharge rate of Luancheng area is 134 mm/a.
- North China Plain,
- declining water table,
- vertical groundwater recharge,
- numerical simulation,
- Hydrus-1D

FullText(HTML)

References(30)

References

Allen, R. G., Pereira, L. S., Raes, D., et al., 1998. Irrigation and Drainage Paper No. 56: Crop Evapotranspiration (Guidelines for Computing Crop Water Requirements). FAO, Rome

Botros, F. E., Onsoy, Y. S., Timothy, R., et al., 2012. Richards Equation-Based Modeling to Estimate Flow and Nitrate Transport in a Deep Vadose Zone. Vadose Zone Journal, 11(4): 1–16. doi: 10.2136/vzj2011.0145

Chen, J. F., 2010. Research on Precipitation Recharge. Groundwater, 32(2): 30–31 (in Chinese)

Fan, Q., Wang, J., Lin, W. J., et al., 2006. The Groundwater Recharge Rule Study in the Condition of Aeration Zone Incrassation. Hydrogeology & Engineering Geology, (3): 21–24 (in Chinese with English Abstract)

Feddes, R. A., Kowalik, P. J., Zarandny, H., 1978. Simulation of Field Water Use and Crop Yield. John Wiley Sons, Beijing

Han, S. M., Cheng, Y. S., Hu, C. S., 2005. Relationship between Crop Coefficient and Precipitation Pattern in the Piedmont of Mt. Taihang. Agricultural Research in the Arid Area, 23: 152–158 (in Chinese with English Abstract) http://europepmc.org/abstract/cba/606284

Helling, C. S., Gish, T. J., 1991. Physical and Chemical Processes Affecting Preferential Flow. In: Gish, T. J., Shirmohammadi, A., eds., Preferential Plow: Proceedings of the National Symposium. American Society of Agricultural Engineers, St. Joseph. 77–86

Hu, S. J., Kang, S. Z., Song, Y. D., et al., 2004. Characteristics and Dependence Analysis Reference Crop Evapotranspiration in Alaer Irrigated Area in Tarim River Basin. Journal of Irrigation and Drainage, 23(6): 59–64 (in Chinese with English Abstract)

Li, N., Ren, L., Tang, Z. J., 2013. Modeling and Analyzing Water Flow in Thick Unsaturated Zone during Precipitation and Infiltration. Transactions of the Chinese Society of Agriculture Engineering (Transactions of the CSAE), 29(12): 94–100 (in Chinese with English Abstract) http://www.ingentaconnect.com/content/tcsae/tcsae/2013/00000029/00000012/art00013

Lu, X. H., Jin, M. G., 2007. One-Dimensional Unsaturated Flow Modeling in Luan Representative Zone of the North China Plain. Journal of China University of Geosciences, 18: 59–61

Lu, X. H., Jin, M. G., van Genuchten, M. T., et al., 2011. Groundwater Recharge at Five Representative Sites in the Hebei Plain. Ground Water, 49(2): 286–294. doi: 10.1111/j.1745-6584.2009.00667.x

Mattern, S., Vanclooster, M., 2010. Estimating Travel Time of Recharge Water Through a Deep Vadose Zone Using a Transfer Function Model. Environmental Fluid Mechanics, 10(1–2): 121–135. doi: 10.1007/s10652-009-9148-1

Pang, Z. H., Yuan, L. J., Huang, T. M., et al., 2013. Impacts of Human Activities on the Occurrence of Groundwater Nitrate in an Alluvial Plain: A Multiple Isotopic Tracers Approach. Journal of Earth Science, 24(1): 111–124. doi: 10.1007/s12583-013-0310-9

Qi, D. H., Jin, M. G., Liu, Y. F., 2007. Determination of Preferential Flow in Precipitation Infiltration Recharge. Earth Science-Journal of China University of Geosciences, 32(3): 420–424 (in Chinese with English Abstract) http://www.cnki.com.cn/Article/CJFDTotal-DQKX200703016.htm

Rushton, K., 1997. Recharge from Permanent Water Bodies. In: Simmers, I., ed., Recharge of Phreatic Aquifers in (Semi) Arid Areas. Rorrerdam, AA Balkema

Scanlon, B. R., Healy, R. W., Cook, P. G., 2002. Choosing Appropriate Techniques for Quantifying Groundwater Recharge. Hydrogeology Journal, 10: 18–39. doi: 10.1007/s10040-001-0176-2

Simunek, J., van Genuchten, M. T., Sejna, M., 2008. Development and Applications of the HYDRUS and STANMOD Software Packages and Related Codes. Vadose Zone Journal, 7(2): 587–600. doi: 10.22136/vzj2007.0077

Song, B., Yang, J. Z., Zha, Y. Y., 2012. An Analysis of Groundwater Recharge from Precipitation and Irrigation Based on Ross Numerical Models. China Rural Water and Hydropower, 9: 55–62 (in Chinese with English Abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZNSD201209018.htm

Sun, H. Y., Liu, C. M., Zhang, X. Y., et al., 2004. The Changing Laws of the Diurnal Evapotranspiration and Soil Evaporation between Plants in the Winter Wheat Field of the North China Plain. China Journal of Eco-Agriculture, 12(3): 62–64 (in Chinese with English Abstract) http://www.researchgate.net/publication/291347407_The_changing_laws_of_the_diurnal_evapotranspiration_and_soil_evaporation_between_plants_in_the_winter_wheat_field_of_the_North_China_Plain

Tan, X. C., Yang, J. Z., Song, X. H., et al., 2013. Estimating of Groundwater Recharge in North China Plain. Advances in Water Science, 24(1): 77–84 (in Chinese with English Abstract) http://www.researchgate.net/publication/279603909_Estimation_of_groundwater_recharge_in_North_China_Plain/download

van Genuchten, M. T., 1980. A Closed-Form Equation for Predicting the Hydraulic Conductivity of Unsaturated Soils. Soil Science Society of America Journal, 44: 892–898 doi: 10.2136/sssaj1980.03615995004400050002x

Walvoord, M. A., Plummer, M. A., Phillips, F. M., et al., 2002. Deep Arid System Hydrodynamics 1. Equilibrium States and Response Times in Thick Desert Vadose Zones. Water Resources Research, 38(12): 1–15. doi: 10.1029/2001WR000824

Wang, B. G., 2008. Research on Estimating Methods of Groundwater Recharge: A Case in North China Plain: [Dissertation]. China University of Geosciences, Wuhan (in Chinese with English Abstract)

Wang, B. G., Jin, M. G., Nimmo, J. R., et al., 2008. Estimating Groundwater Recharge in Hebei Plain, China under Varying Land Use Practices Using Tritium and Bromide Tracers. Journal of Hydrology, 356(1–2): 209–222. doi: 10.1016/j.jhydrol.2008.04.011

Wang, J., Cai, H. Y., Kang, Y. X., et al., 2007. Ratio of Soil Evaporation to the Evapotranspiration for Summer Maize Field. Transactions of the CSAE, 23(4): 17–22 (in Chinese with English Abstract) http://dl.sciencesocieties.org/publications/tcsae/abstracts/2007/4/2007.4.004

Wang, Y. Y., Wang, Z. C., Hu, Y. G., 1998. An Analysis of Groundwater Recharge from Precipitation. Groundwater, 20(2): 74–75 (in Chinese)

Zhang, G. H., Fei, Y. H., Shen, J. M., et al., 2007. Influence of Unsaturated Zone Thickness on Precipitation Infiltration for Recharge of Groundwater. Journal of Hydraulic Engineering, 38(5): 611–617 (in Chinese with English Abstract)

Zhang, R. Q., Liang, X., Jin, M. G., et al., 2011. Fundamental of Hydrogeology. 6. Geological Publishing House, Beijing (in Chinese)

Zhang, Z. J., Fei, Y. H., Chen, Z. Y., et al., 2009. Investigation and Assessment of Sustainable Utilization of Groundwater Resources in the North China Plain. Geological Publishing House, Beijing (in Chinese)

Zhou, M., Jin, M. G., Wei, X. Q., et al., 2002. Analysis of Precipitation Recharge Using Observed Data of Lysimeter. Geological Science and Technology Information, 21(1): 37–40 (in Chinese with English Abstract) http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ200201010.htm

Relative Articles

Supplements(0)

Cited By

Proportional views