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A comparative study of two methods for modeling soil water regime in agricultural fields

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dc.contributor.author Tsiros, JX en
dc.contributor.author Elmaloglou, S en
dc.contributor.author Ambrose Jr ,RB en
dc.date.accessioned 2014-06-06T06:43:35Z
dc.date.available 2014-06-06T06:43:35Z
dc.date.issued 1998 en
dc.identifier.issn 09204741 en
dc.identifier.uri http://dx.doi.org/10.1023/A:1008073824019 en
dc.identifier.uri http://62.217.125.90/xmlui/handle/123456789/1376
dc.subject Agricultural land en
dc.subject Comparative study en
dc.subject Modeling en
dc.subject Soil water en
dc.subject Statistical analysis en
dc.subject Water budget en
dc.subject.other Agrometeorology en
dc.subject.other Richards' equation en
dc.subject.other Water balance en
dc.subject.other Agriculture en
dc.subject.other Graph theory en
dc.subject.other Mathematical models en
dc.subject.other Meteorology en
dc.subject.other Moisture en
dc.subject.other Soils en
dc.subject.other Statistical methods en
dc.subject.other Water resources en
dc.subject.other agricultural land en
dc.subject.other comparative study en
dc.subject.other modeling en
dc.subject.other soil water en
dc.subject.other statistical analysis en
dc.subject.other water budget en
dc.title A comparative study of two methods for modeling soil water regime in agricultural fields en
heal.type journalArticle en
heal.identifier.primary 10.1023/A:1008073824019 en
heal.publicationDate 1998 en
heal.abstract Two methods widely used in agrometeorogical simulation models for describing field soil water regimes are compared and evaluated based on their ability to predict experimental data from a single field study. The first method is based on a numerical solution to the Richards' equation for describing water movement in the soil profile, while the second method is based on soil-water capacity terms. The evaluation of the performance of the two methods is based on goodness-of-fit statistics and graphical analysis. Results indicate that the first method is more accurate for both the upper and the lower soil zones; the second method, despite its low performance in the upper soil zone can adequately describe soil moisture conditions in the lower soil zones. Recommendations are made for model use based on comparison results, the intended model use, and the difficulty in the acquisition of required model inputs. en
heal.journalName Water Resources Management en
dc.identifier.issue 4 en
dc.identifier.volume 12 en
dc.identifier.doi 10.1023/A:1008073824019 en
dc.identifier.spage 285 en
dc.identifier.epage 293 en


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