Steady Infiltration from Buried, Surface, and Perched Point and Line Sources in Heterogeneous Soils: II. Flow Details and Discussion1
- J. R. Philip and
- R. I. Forrester2
Part I (Philip, 1972) developed physically relevant source solutions of the quasilinearized steady infiltration equation, generalized to apply to heterogeneous soils with conductivity depending exponentially on both moisture potential and depth. This paper discusses the results in further detail, and includes graphs of a wide range of solutions.Please view the pdf by using the Full Text (PDF) link under 'View' to the left.
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