Modified Kostiakov Infiltration Function: Accounting for Initial and Boundary Conditions
The effect of specific initial and boundary conditions is generally not considered when applying the Kostiakov infiltration functions. A methodology is developed to account for changes in water levels and initial soil moisture. First, Richards’ equation is solved numerically to generate a database o...
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Veröffentlicht in: | Journal of irrigation and drainage engineering 2006-12, Vol.132 (6), p.587-596 |
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creator | Furman, A Warrick, A. W Zerihun, D Sanchez, C. A |
description | The effect of specific initial and boundary conditions is generally not considered when applying the Kostiakov infiltration functions. A methodology is developed to account for changes in water levels and initial soil moisture. First, Richards’ equation is solved numerically to generate a database of one-dimensional infiltration values, with varying initial (water content or pressure head) and boundary (ponding depth) conditions for three contrasting soils. These are then used to calibrate corresponding coefficients for modified Kostiakov models and, by considering linear regressions, to obtain simple correction factors. Results show that the correction factors are not universally valid, and only the correction to the Kostiakov
k
parameter shows statistically consistent applicability. However, examples demonstrate potentially significant improvement in the accuracy of irrigation models by correcting the Kostiakov equation to account for initial and boundary conditions. |
doi_str_mv | 10.1061/(ASCE)0733-9437(2006)132:6(587) |
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k
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k
parameter shows statistically consistent applicability. However, examples demonstrate potentially significant improvement in the accuracy of irrigation models by correcting the Kostiakov equation to account for initial and boundary conditions.</description><subject>Agricultural and forest climatology and meteorology. Irrigation. Drainage</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>equations</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>hydrologic models</subject><subject>infiltration (hydrology)</subject><subject>Irrigation. 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A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Modified Kostiakov Infiltration Function: Accounting for Initial and Boundary Conditions</atitle><jtitle>Journal of irrigation and drainage engineering</jtitle><date>2006-12-01</date><risdate>2006</risdate><volume>132</volume><issue>6</issue><spage>587</spage><epage>596</epage><pages>587-596</pages><issn>0733-9437</issn><eissn>1943-4774</eissn><coden>JIDEDH</coden><abstract>The effect of specific initial and boundary conditions is generally not considered when applying the Kostiakov infiltration functions. A methodology is developed to account for changes in water levels and initial soil moisture. First, Richards’ equation is solved numerically to generate a database of one-dimensional infiltration values, with varying initial (water content or pressure head) and boundary (ponding depth) conditions for three contrasting soils. These are then used to calibrate corresponding coefficients for modified Kostiakov models and, by considering linear regressions, to obtain simple correction factors. Results show that the correction factors are not universally valid, and only the correction to the Kostiakov
k
parameter shows statistically consistent applicability. However, examples demonstrate potentially significant improvement in the accuracy of irrigation models by correcting the Kostiakov equation to account for initial and boundary conditions.</abstract><cop>Reston, VA</cop><pub>American Society of Civil Engineers</pub><doi>10.1061/(ASCE)0733-9437(2006)132:6(587)</doi><tpages>10</tpages></addata></record> |
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source | American Society of Civil Engineers:NESLI2:Journals:2014 |
subjects | Agricultural and forest climatology and meteorology. Irrigation. Drainage Agronomy. Soil science and plant productions Biological and medical sciences equations Fundamental and applied biological sciences. Psychology General agronomy. Plant production hydrologic models infiltration (hydrology) Irrigation. Drainage soil water content surface irrigation TECHNICAL PAPERS water flow |
title | Modified Kostiakov Infiltration Function: Accounting for Initial and Boundary Conditions |
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