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dc.contributorMartius, Christopheren_US
dc.contributorPark, Soo Jinen_US
dc.contributorHendrickx, Jan M. H.en_US
dc.creatorAkramkhanov, Akmalen_US
dc.date.accessioned2017-07-23T21:48:30Z
dc.date.available2017-07-23T21:48:30Z
dc.identifierhttps://www.researchgate.net/publication/236343243_Environmental_factors_of_spatial_distribution_of_soil_salinity_on_flat_irrigated_terrainen_US
dc.identifierhttps://mel.cgiar.org/reporting/download/hash/bJwBRMNIen_US
dc.identifier.citationAkmal Akramkhanov, Christopher Martius, Soo Jin Park, Jan M. H. Hendrickx. (19/4/2011). Environmental factors of spatial distribution of soil salinity on flat irrigated terrain. Geoderma, 163, pp. 55-62.en_US
dc.identifier.urihttps://hdl.handle.net/20.500.11766/7174
dc.description.abstractInefficient irrigation and the excessive use ofwater on agricultural land in the Aral Sea Basin over several decades have led to saline soils. The main objective of this paper is to identify the environmental predictors to model the spatial distribution of soil salinity in a highly irrigated landscape. Soil salinity at farm scale was measured in the topsoil (Total Dissolved Solids, TDS) and down to a depth of 1.5mby electromagnetic conductivitymeter (CMv) over a regular grid covering an area of approximately 15 km2 in Khorezm Province, Uzbekistan. Six nested samplings within selected grids were conducted to reveal short-distance variation. Apart from widely-used terrain indices and those acquired from remote sensing, data on distance to drainage channels and long-term average groundwater observations were used to account for local parameters possibly influencing soil salinity. Topsoil salinity (TDS) was seen to be highly variable even at short distances (40 m)compared to average bulk soil salinity (CMv). CMv readings were better correlated with factors obtained from remote sensing and distance to drains than TDS. This might be attributable to the fact that topsoil salts are dynamic in nature, and land management practices (e.g. leaching, cultivation, and irrigation) might have contributed considerably to spatial variation. The CMv shows the average amount of saltwithin a larger soil volume and to greater depth and is less affected by land management than topsoil salinity, which is reflected in the TDS. Most terrain indices showed a lowcorrelation with topsoil and bulk salinity. There was a strong indication that the effects ofwatermanagement are dominant and tend to outweigh the effects of environmental factors. The very low R2 for relationship of TDS with environmental factors is evidence that taking TDS samples close to the soil surface is not a goodway to assess salinity trends in irrigated land. These findings have important implications for salinity survey methods on flat irrigated terrain: CMv seems to be a more reliable predictor than environmental proxy factors, even if the latter are easier to determine.en_US
dc.formatDOCen_US
dc.languageenen_US
dc.publisherElsevieren_US
dc.rightsCC-BY-NC-4.0en_US
dc.sourceGeoderma;163,(2011) Pagination 55-62en_US
dc.subjectkhorezmen_US
dc.subjectspatial interpolationen_US
dc.subjectaral sea basinen_US
dc.subjectvariabilityen_US
dc.titleEnvironmental factors of spatial distribution of soil salinity on flat irrigated terrainen_US
dc.typeJournal Articleen_US
dcterms.available2011-04-19en_US
dcterms.extent55-62en_US
cg.creator.idAkramkhanov, Akmal: 0000-0002-4316-5580en_US
cg.subject.agrovocsoil degradationen_US
cg.contributor.centerInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.contributor.centerUniversity of Bonn - Uni-Bonnen_US
cg.contributor.centerSeoul National University - SNUen_US
cg.contributor.centerNew Mexico Institute of Mining and Technology - NMTen_US
cg.contributor.crpCGIAR Research Program on Dryland Systems - DSen_US
cg.contributor.funderInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.contributor.projectCommunication and Documentation Information Services (CODIS)en_US
cg.contributor.project-lead-instituteInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.coverage.regionCentral Asiaen_US
cg.coverage.countryUZen_US
cg.contacta.akramkhanov@cgiar.orgen_US
cg.isijournalISI Journalen_US
dc.identifier.statusOpen accessen_US
mel.impact-factor4.036en_US
cg.issn0016-7061en_US
cg.journalGeodermaen_US
cg.volume163en_US


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