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dc.creatorSalazar,Osvaldo
dc.creatorWesstrom,Ingrid
dc.creatorAbraham,Joel
dc.date2011-01-01
dc.date.accessioned2019-04-25T12:39:46Z
dc.date.available2019-04-25T12:39:46Z
dc.identifierhttps://scielo.conicyt.cl/scielo.php?script=sci_arttext&pid=S0718-95162011000200004
dc.identifier.urihttp://revistaschilenas.uchile.cl/handle/2250/60949
dc.descriptionThe relationship between total phosphorus (TP) and molybdate-reactive phosphorus (MRP) concentrations in subsurface drainage waters in the hydrological conditions prevailing during autumn and spring flow events was statistically analysed using multiple linear regression analysis. Data on hydrological conditions in three drainage experimental plots in a loamy sand in south-east Sweden complemented with DRAINMOD-predicted data were used as independent variables. Regression models explained at least 80% of the variation in TP and MRP concentrations in drain outflow, based on adjusted coefficient of determination (R²adj) calculations. DRAINMOD-predicted cumulative infiltration (INFILcum) was identified as the most important hydrological condition controlling TP and MRP concentrations in drain outflow in three autumn events and in two out of three spring events. This suggests that the first infiltrating water found more soluble P forms available for transport, after which TP and MRP concentration in drainage outflows gradually decreased during the flow events.
dc.formattext/html
dc.languageen
dc.publisherChilean Society of Soil Science / Sociedad Chilena de la Ciencia del Suelo
dc.relation10.4067/S0718-95162011000200004
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceJournal of soil science and plant nutrition v.11 n.2 2011
dc.subjectControlled drainage
dc.subjectDRAINMOD
dc.subjectMatrix flow
dc.subjectPreferential flow
dc.subjectSubsurface flow
dc.titleIDENTIFICATION OF HYDROLOGICAL FACTORS CONTROLLING PHOSPHORUS CONCENTRATION IN DRAINAGE WATER IN SANDY SOILS


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