Abstract
The accepted theory of percolation of fluids through porous materials (which is based on Darcy’s law of resistance) indicates that the velocities can be calculated from a velocity-potential which, in two-dimensional motion, is plane-harmonic within the fluid field. The associated stream function, and the fluid pressure, are also plane-harmonic, so in cases where all boundaries are known their determination is an ordinary problem in plane-potential theory. But in cases where a free surface exists (as in the percolation of water through earth dams), its shape is not known a priori, consequently orthodox methods cannot be applied. Here the relaxation method developed in earlier papers is shown to be applicable without special assumptions, and to yield results of more than sufficient accuracy. Three typical examples are treated, the third involving ‘refraction’ of the lines of flow and pressure at the junction of two materials of different porosity.
Reference13 articles.
1. B oussinesq J . 1904 J ■
2. C asagrande A. 1937 J •
3. M a t h . puresappl. (5) 10 11-16 363-394. NewEngl. Wat. Wks Ass. 51 131-172.
4. Proc. Roy;Southw R .;Soc. A,1938
5. LXXII.On the steady two-dimensional motion of ground-water with a free surface
Cited by
35 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献