Journal article

INTERPRETATION OF FIELD-CAPACITY AND MOISTURE EQUIVALENT ON THE BASIS OF THE THEORY OF FLOW


Authors list: BOHNE, K; WEGMANN, C

Publication year: 1986

Pages: 327-336

Journal: Archives of Agronomy and Soil Science

Volume number: 30

Issue number: 6

ISSN: 0365-0340

Publisher: Taylor and Francis Group


Abstract: 
Using an analytical solution of the non-steady-state internal drainage equation according to GARDNER, the calculation of mean diffusivity according to CRANK is an iterative scheme and the .THETA.(h.sigma.) and D(.THETA.) functions according to VAN GENUCHTEN, the internal drainage of 17 soil profiles of different texture was calculated for three groundwater table depths. The results show the time-dependent discharge and are used for discussing the conventional terms field capacity and moisture equivalent.



Citation Styles

Harvard Citation style: BOHNE, K. and WEGMANN, C. (1986) INTERPRETATION OF FIELD-CAPACITY AND MOISTURE EQUIVALENT ON THE BASIS OF THE THEORY OF FLOW, Archives of Agronomy and Soil Science, 30(6), pp. 327-336

APA Citation style: BOHNE, K., & WEGMANN, C. (1986). INTERPRETATION OF FIELD-CAPACITY AND MOISTURE EQUIVALENT ON THE BASIS OF THE THEORY OF FLOW. Archives of Agronomy and Soil Science. 30(6), 327-336.


Last updated on 2025-02-04 at 05:13