Lysimeter Water Balance for Bare and Cropped Soil

dc.bibliographicCitation.endpage20en
dc.bibliographicCitation.stpage20en
dc.bibliographicCitation.titleEast African Agricultural And Forestry Journalen
dc.contributor.authorStewart, J.I.
dc.contributor.authorMugah, J.O.
dc.date.accessioned2015-07-15T08:53:59Z
dc.date.available2015-07-15T08:53:59Z
dc.date.issued1979en
dc.description.abstractWater 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.notesFor presentation at the Third Annual General Meeting of the Soil Science Society of East Africa, Muguga, Kenya, 25-27 July, 1979en
dc.identifier.citationStewart, 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/0/4501en
dc.identifier.issn0012-8325*
dc.identifier.urihttps://kalroerepository.kalro.org/handle/0/4501
dc.language.isoenen
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/en
dc.subject.agrovocLysimetersen
dc.subject.agrovocWater balanceen
dc.subject.agrovocSoilen
dc.subject.agrovocHydrological cycleen
dc.titleLysimeter Water Balance for Bare and Cropped Soilen
dc.typeJournal Contribution*
dc.type.refereedRefereeden
dc.type.specifiedArticleen

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