Numerical Analysis of Groundwater Flow with Density Difference Using Characteristic Finite Element Method: Application to Two-Phase Flow of Fresh and Salt Water-Reference-Cited by-同舟云学术

Numerical Analysis of Groundwater Flow with Density Difference Using Characteristic Finite Element Method: Application to Two-Phase Flow of Fresh and Salt Water

Published:1984 Issue:1 Volume:26 Page:12-22
ISSN:0029-0602
Container-title:THE JOURNAL OF THE JAPANESE ASSOCIATION OF GROUNDWATER HYDROLOGY
language:en
Short-container-title:

Author:

FUJINAWA Katsuyuki¹

Affiliation:

1. National Research Institute of Agricultural Engineering

Publisher

Japanese Association of Groundwater Hydrology

Reference6 articles.

1. Bear, J. and G. Dagan. (1964): Moving interface in coastal aquifers. I Hydraul. Div. Am. Soc. Civ. Eng., 90 (HY4), 193-216.

2. De Josselin de Jong, G. (1981): The simultaneous flow of fresh and salt water in aquifers of large horizontal extention determined by shear flow and vortex theory. Proceedings of Euromech, 143, A. A. Balkema, 75-82.

3. Fujinawa, K. (1983): A‘ characteristic’ finite element method for dispersion-convection equation. Jour. of Japanese Association of Groundwater Hydrology, 25, 93-108.

4. Liu, FL-F., A. H-D. Cheng and J. A. Liggett (1981): Boundary integral equation solutions to moving interface between two fluids in porous media. Water Resour. Res., 17, 1445-1452.

5. Shamir, U. and G. Dagan (1971): Motion of the seawater interface in coastal aquifers: A numerical solution. Water Resour. Res., 7, 644-657.

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