Finite Elements in Water Resources 1982
DOI: 10.1007/978-3-662-02348-8_59
|View full text |Cite
|
Sign up to set email alerts
|

Finite Element Analysis of Soil Moisture Flow and Moisture Stress in a Dessicating Soil

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

1993
1993
2004
2004

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(1 citation statement)
references
References 6 publications
0
1
0
Order By: Relevance
“…These findings naturally led to the notion that the distribution of soil water suction induced by the water absorption of the roots determined the location of inter-row cracks. Theoretical study of inter-row crack formation resulting from water movement has not advanced since Nieber's (1982) pioneering work, which simulated tensile stress generation occurring in the row-middle due to evapo-transpiration. The model succeeded in simulating the phenomenon in which bidirectional unsaturated water flow led to the generation of tensile stress between rows.…”
Section: Introductionmentioning
confidence: 99%
“…These findings naturally led to the notion that the distribution of soil water suction induced by the water absorption of the roots determined the location of inter-row cracks. Theoretical study of inter-row crack formation resulting from water movement has not advanced since Nieber's (1982) pioneering work, which simulated tensile stress generation occurring in the row-middle due to evapo-transpiration. The model succeeded in simulating the phenomenon in which bidirectional unsaturated water flow led to the generation of tensile stress between rows.…”
Section: Introductionmentioning
confidence: 99%