Abstract
The authors demonstrate the importance of the simulation of the water quantity exchange between river water and groundwater to a better understanding of the hydrologic relations between a river and nearby aquifer where groundwater is pumped extensively but only seasonally. And MODFLOW is used to design the stream-aquifer model in which the pumpage of more than 1000 wells was simulated. The river gaining and river losing processes were analyzed. Simulation results suggest that continuation of over-extraction of groundwater will gradually increase the depletion volume in the river year after year and more depletion will occur in later years. The exchange manner between groundwater and the Platte River differs from place to place. The Platte River loses water to the adjacent aquifer in the west part of the study area, and gains water from the adjacent aquifer in the east part of the study area.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
Theis C V. The effect of a well on the flow of a nearby stream [J]. American Geophysical Union Transactions, 1941, 22(3): 734–738.
Glover R E and Balmer G G. River depletion resulting from pumping a well near a river[J]. American Geophysical Union Transaction, 1954, 35(3): 468–470.
Hantush M S. Depletion of Storage, Leakance, and river flow by gravity wells in sloping sands[J]. Journal of Geophysical Research, 1964, 69(12): 2551–2560.
Hunt B. Unsteady stream depletion from ground water pumping[J]. Ground Water, 1999, 37(1): 98–104.
Sophocleous M, Koussis A, Martin J L, et al. Evacuation of simplified stream-aquifer depletion models for water rights administration[J]. Ground Water, 1995, 33(4): 579–588.
Chen X H and Yin Y. Streamflow depletion: modeling of reduced baseflow and induced stream infiltration from seasonally pumped wells[J]. Journal of American Water Resources Association, 2001, 37(1): 185–195.
Chen X H, Goeke J and Summerside S. Hydraulic properties and uncertainty analysis for an unconfined alluvial aquifer [J]. Ground Water, 1999, 37(6): 845–854.
Harbaugh W A and McDonald G M., User’s documentation for MODFLOW-96, an update to the U S Geological Survey Modular Finite-Difference Ground-Water Flow Model[R]. U S Geological Survey, Open-File Report 96-485, Reston, Virginia, 1996. 2–56.
Author information
Authors and Affiliations
Additional information
Foundation item: United State Geological Survey Grant (No. 1434-HQ-96-GR-02683)
Biography of the first author: SHU Long-cang, Dr., professor, born in 1964, majoring in groundwater resources evaluation and management.
Rights and permissions
About this article
Cite this article
Shu, Lc., Chen, Xh. Simulation of water quantity exchange between groundwater and the Platte River water, central Nebraska. J Cent. South Univ. Technol. 9, 212–215 (2002). https://doi.org/10.1007/s11771-002-0029-8
Received:
Issue Date:
DOI: https://doi.org/10.1007/s11771-002-0029-8