Lysimeter Water Balance for Bare and Cropped Soil
dc.bibliographicCitation.endpage | 20 | en |
dc.bibliographicCitation.stpage | 20 | en |
dc.bibliographicCitation.title | East African Agricultural And Forestry Journal | en |
dc.contributor.author | Stewart, J.I. | |
dc.contributor.author | Mugah, J.O. | |
dc.date.accessioned | 2015-07-15T08:53:59Z | |
dc.date.available | 2015-07-15T08:53:59Z | |
dc.date.issued | 1979 | en |
dc.description.abstract | Water balance is the algebraic sum of the\total accretion and removal of water within a defined hydrological unit such as a lake a basin, a 1ysimeter, etc., taking into account net changes of storage. Accretion comes mostly from rainfall and irrigation (at least within the tropics), although in extra-tropical areas snow and other forms of precipitation such as dew may be appreciable. Upward movement of water by capillarity from a water table, and lateral seepage from adjacent areas are also possible sources of accretion. | en |
dc.description.notes | For presentation at the Third Annual General Meeting of the Soil Science Society of East Africa, Muguga, Kenya, 25-27 July, 1979 | en |
dc.identifier.citation | Stewart, J.I., Mugah, J.O. (1979). Lysimeter Water Balance for Bare and Cropped Soil. In Proc of the 3rd Annual General Meeting of the Soil Science Society of East Africa, Muguga, Kenya, 20. https://kalroerepository.kalro.org/handle/0/4501 | en |
dc.identifier.issn | 0012-8325 | * |
dc.identifier.uri | https://kalroerepository.kalro.org/handle/0/4501 | |
dc.language.iso | en | en |
dc.rights.uri | http://creativecommons.org/licenses/by/3.0/ | en |
dc.subject.agrovoc | Lysimeters | en |
dc.subject.agrovoc | Water balance | en |
dc.subject.agrovoc | Soil | en |
dc.subject.agrovoc | Hydrological cycle | en |
dc.title | Lysimeter Water Balance for Bare and Cropped Soil | en |
dc.type | Journal Contribution | * |
dc.type.refereed | Refereed | en |
dc.type.specified | Article | en |
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