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The modeling of water transfer in the unsaturated zone uses techniques and methods of the soil physics to solve the Richards-s equation. However, there is a disaccord between the size of the measurements provided by the soil physics and the size of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::03f386732758fb213ba96a4f347cd6ac
Publikováno v:
International Review of Mechanical Engineering; Jul2013, Vol. 7 Issue 5, p857-863, 7p
Publikováno v:
Diffusion and Defect Data Part A: Defect and Diffusion Forum; January 2014, Vol. 348 Issue: 1 p113-120, 8p