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Spatial variation in the solute transport attributes of adjacent Typic Haplusteps, Mollic Ustifluvents, and Lithic Ustipsamments

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dc.contributor.author Askin, Tayfun
dc.contributor.author Bilgili, Bayram C.
dc.contributor.author Ersahin, Sabit
dc.contributor.author Korkmaz, Kursat
dc.contributor.author Kutlu, Turgut
dc.contributor.author Ozenc, Damla B.
dc.contributor.author Sunal, Seval
dc.contributor.author Tarakcioglu, Ceyhan
dc.date.accessioned 2022-08-15T08:31:03Z
dc.date.available 2022-08-15T08:31:03Z
dc.date.issued 2017
dc.identifier.uri http://doi.org/10.1016/j.geoderma.2016.11.035
dc.identifier.uri https://www.sciencedirect.com/science/article/pii/S0016706116309284?via%3Dihub
dc.identifier.uri http://earsiv.odu.edu.tr:8080/xmlui/handle/11489/1326
dc.description.abstract Spatial variation in water flow and solute transport are important considerations when assessing field-scale re mediation options, and for managing water and chemicals during agricultural production. Here, we evaluated the relationship between laboratory-measured solute transport variables pore-water velocity (v), dispersivity (lambda), and retardation coefficient (R) and land use, soil type, and other independently measured soil properties in adjacent Typic Haplusteps, Mollic Ustifluvents, and Lithic Ustipsamments. We also characterized the spatial variation in v, R, coefficient of hydrodynamic dispersion (D), and lambda. We obtained 100 geo-referenced, undisturbed soil columns (8.4 cm diameter and of varying length) from the topsoil at sites with varying land uses, topographies, and soil types, and synchronized disturbed soil samples to analyze the basic soil properties. We conducted miscible displacement tests on all 100 columns, and predicted the retardation coefficient (R) and D using the computer program CXTFIT, and measured v. All four variables, except R, had strongly right-skewed and kurtotic distributions, and were highly variable. Log lambda (logarithm to base 10) was significantly correlated with land use, with the mean of lambda being significantly greater in grasslands, followed by orchards and croplands. By contrast, v was significantly correlated with soil type, with the mean being significantly greater in Lithic Ustipsamments. Log v (logarithm to base 10) was also significantly correlated with the soil CaCO3 content, log organic matter content, pH, cation exchange capacity, and log electrical conductivity, whereas neither v nor lambda was correlated with soil texture measures. An analysis of the spatial structure of solute transport variables using semivariograms showed that R and lambda had considerably high nugget effect. Log-transformed semivariograms performed well using ordinary point kriging for v and D. However, lambda and R exhibited a very weak spatial dependency that could not be interpolated using ordinary kriging at the current sampling resolution. Therefore, this should be considered when designing future sampling programs to analyze spatial structure-of R and lambda. (C) 2016 Published by Elsevier B.V. en_US
dc.language.iso eng en_US
dc.publisher ELSEVIER, RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS en_US
dc.relation.isversionof 10.1016/j.geoderma.2016.11.035 en_US
dc.rights info:eu-repo/semantics/openAccess en_US
dc.subject Pore-water velocity; Dispersivity; Miscible displacement; Semivariogram; Ordinary point kriging en_US
dc.subject SOIL PROPERTIES; LEACHING CHARACTERISTICS; HYDRAULIC-PROPERTIES; ANION TRANSPORT; STEADY-STATE; FIELD; VARIABILITY; WATER; FLOW; BROMIDE en_US
dc.title Spatial variation in the solute transport attributes of adjacent Typic Haplusteps, Mollic Ustifluvents, and Lithic Ustipsamments en_US
dc.type article en_US
dc.relation.journal GEODERMA en_US
dc.contributor.department Ordu Üniversitesi en_US
dc.contributor.authorID 0000-0001-9352-2710 en_US
dc.contributor.authorID 0000-0002-7839-3153 en_US
dc.contributor.authorID 0000-0003-1846-2097 en_US
dc.identifier.volume 289 en_US
dc.identifier.startpage 107 en_US
dc.identifier.endpage 116 en_US


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