Abstract
Transport processes within a liquid-filled fractured reservoir can be modelled using a double-diffusive mechanism in fracture and block. Then it is commonly assumed that the flow in the block is purely one-dimensional (e.g. vertical). Lateral flow within the block will, however, become significant at long times. Avdonin has given an analytic solution for the pressure response in an infinite fissure bounded by two homogeneous half-spaces, allowing vertical flow only in the blocks. We extend this solution to include horizontal flow in the blocks. There are significant qualitative differences between the two cases. In particular, we find that if fluid is injected at a constant rate into the fissure and horizontal flow in the blocks is allowed, then the long-time pressure response of the fissure/block assembly has the same character as that due to a line source in a homogeneous anisotropic porous medium.
Similar content being viewed by others
References
Abramowitz, M. and Stegun, I. A., 1972, Handbook of Mathematical Functions, Dover, New York.
Avdonin, N. A., 1964, Some formulas for calculating the temperature field of a stratum subject to thermal injection, Isv. Vyssh. Uchebn. Zaved. Neft. Gaz. 7, 37–41.
Boulton, N. S. and Streltsova, T. D., 1977, Unsteady flow to a pumped well in a fissured water bearing formation, J. Hydrol. 35, 257–269.
Barenblatt, G. I., Zheltov, Iu. P., and Kocina, I. N., 1960, Basic concepts in the theory of seepage of homogeneous liquids in fissured rocks (strata), J. Appl. Math. Mech. 24, 1286–1303.
Bodvarsson, G. S. and Tsang, C. F., 1982, Injection and thermal breakthrough in fractured geothermal reservoirs, J. Geophys. Res. 87, 1031–1048.
Cinco-Ley, H. and Samaniego-V, F., 1981, Transient pressure analysis for fractured wells, J. Pet. Tech., 1749–1766.
Cinco-Ley, H., Samaniego-V. F., and Dominquez, N. A., 1978, Transient pressure behaviour for a well with a finite-conductivity vertical fracture, Soc. Pet. Eng. J., 265–277.
Erdélyi, A., Magnus, W., Oberhettinger, F., and Tricomi, F. G., 1954, Tables of Integral Transforms, Vol. 1, McGraw-Hill, New York.
Gringarten, A. C. and Ramey, H. J. Jr., 1974, Unsteady-state pressure distributions created by a well with a single horizontal fracture, partial penetration, or restricted entry, Soc. Pet. Eng. J., 413–426; Trans. SPE-AIME, 257.
Gringarten, A. C., Ramey, H. J. Jr., and Raghavan, R., 1974, Unsteady-state pressure distributions created by a well with a single infinite-conductivity vertical fracture, Soc. Pet. Eng. J., 347–360; Trans. SPE-AIME, 257.
McGuinness, M. J., 1986, Pressure transmission in a bounded randomly fractured reservoir of single-phase fluid, Transport in Porous Media 1, 371–397.
Mercer, J. W., Faust, C. R., and Miller, W. J., 1982, Review of simulation techniques for aquifer thermal energy storage (ATES), Adv. Hydrosci. 13, 1–129.
Moench, A. F., 1984, Double-porosity models for a pressured groundwater reserve with fracture skin, Water Resour. Res. 20, 831–846.
Roberts, G. E. and Kaufman, H., 1966, Table of Laplace Transforms, W. B. Saunders, Philadelphia.
Theis, C. V., 1935, The relation between the lowering of the piezometric surface and the rate and duration of the discharge of a well using ground-water storage, Eos Trans. AGU 16, 519–524.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Kissling, W., Young, R.M. Two-dimensional flow in a fractured medium. Transp Porous Med 4, 335–368 (1989). https://doi.org/10.1007/BF00165779
Received:
Revised:
Issue Date:
DOI: https://doi.org/10.1007/BF00165779