نمایش مختصر رکورد

dc.contributor.authorNOSHADI, M.en_US
dc.contributor.authorFOROUHARFAR (HAMILTON), F.en_US
dc.contributor.authorAMIN, S.en_US
dc.contributor.authorMAFTOUN, M.en_US
dc.date.accessioned1399-07-09T09:06:20Zfa_IR
dc.date.accessioned2020-09-30T09:06:20Z
dc.date.available1399-07-09T09:06:20Zfa_IR
dc.date.available2020-09-30T09:06:20Z
dc.date.issued2011-03-01en_US
dc.date.issued1389-12-10fa_IR
dc.date.submitted2012-10-08en_US
dc.date.submitted1391-07-17fa_IR
dc.identifier.citationNOSHADI, M., FOROUHARFAR (HAMILTON), F., AMIN, S., MAFTOUN, M.. (2011). Measuring and Simulating 2,4-D Residues in Silty Clay Soil Profile Under Two Water Regimes Using a LEACHP Model. Iran Agricultural Research, 30(12), 33-46. doi: 10.22099/iar.2012.492en_US
dc.identifier.issn1013-9885
dc.identifier.urihttps://dx.doi.org/10.22099/iar.2012.492
dc.identifier.urihttp://iar.shirazu.ac.ir/article_492.html
dc.identifier.urihttps://iranjournals.nlai.ir/handle/123456789/354927
dc.description.abstractThe extensive use of pesticides in agriculture is compromising soil and water quality. One major concern is protecting water resources from contamination. The main objective of this research was measuring 2,4- D in a silty clay soil and simulating temporal transportation of this herbicide in soil using a LEACHP model, in a corn root zone field. 2,4- D was applied at 3.5 kg a.i./ha, followed by two irrigation treatments in a completely randomized design with three replications. 2,4- D concentrations were measured during the growing season by obtaining soil samples from each plot through a 1 m depth. The measured data showed a temporal reduction of 2,4-D concentrations in the soil down to a maximum depth of 40 cm for both irrigation treatments. Total concentration of 2,4 -D in the soil profile 8, 13, 23, 30, 37, and 57 days after application for normal irrigation were 18.5, 16.36, 11.67, 10.47, 8.47 and 3.2 mg kg 1, respectively and deficit irrigation showed 20.2, 16.7, 11.22, 10.05, 8.8 and 7.3 mg kg 1, respectively for the same dates and soil depth. According to our study region, the half life of 2,4- D for 0 10 cm and 10 20 cm of soil depths in a normal irrigation level were 7 and 33 days and in a deficit irrigation level were 9 and 34.65 days, respectively. The statistical parameters including RMSE, CRM and d were used to compare simulated with measured data. These parameters were 0.67, 0.5 and 0.87 for normal irrigation and 0.8, 0.61 and 0.88 for deficit irrigation. The LEACHP model simulations were in agreement with actual observations.en_US
dc.format.extent403
dc.format.mimetypeapplication/pdf
dc.languageEnglish
dc.language.isoen_US
dc.publisherShiraz Universityen_US
dc.publisherدانشگاه شیرازfa_IR
dc.relation.ispartofIran Agricultural Researchen_US
dc.relation.ispartofتحقیقات کشاورزی ایرانfa_IR
dc.relation.isversionofhttps://dx.doi.org/10.22099/iar.2012.492
dc.subject4-Den_US
dc.subjectDegradationen_US
dc.subjectPesticidesen_US
dc.subjectIrrigationen_US
dc.subjectLEACHPen_US
dc.titleMeasuring and Simulating 2,4-D Residues in Silty Clay Soil Profile Under Two Water Regimes Using a LEACHP Modelen_US
dc.typeTexten_US
dc.typeFull Articleen_US
dc.contributor.departmentDepartment of Water Engineering, College of Agriculture, Shiraz University, Shiraz, I.R. Iranen_US
dc.contributor.departmentDepartment of Water Engineering, College of Agriculture, Shiraz University, Shiraz, I.R. Iranen_US
dc.contributor.departmentDepartment of Water Engineering, College of Agriculture, Shiraz University, Shiraz, I.R. Iranen_US
dc.contributor.departmentDepartment of Soil Science, College of Agriculture, Shiraz University, Shiraz, I.R. Iranen_US
dc.citation.volume30
dc.citation.issue12
dc.citation.spage33
dc.citation.epage46


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