Constructing and Testing of a Facility for Measuring Water and Agrochemical Transport through the Vadose Zone

dc.contributor.author Olson, Dean
dc.contributor.author Kanwar, Rameshwar
dc.contributor.author Bischoff, John
dc.contributor.department Department of Agricultural and Biosystems Engineering (ENG)
dc.date 2018-02-14T08:39:19.000
dc.date.accessioned 2020-06-29T22:40:14Z
dc.date.available 2020-06-29T22:40:14Z
dc.date.copyright Wed Jan 01 00:00:00 UTC 1997
dc.date.embargo 2014-07-20
dc.date.issued 1997
dc.description.abstract <p>A large borehole cavity was constructed to study the transport of agricultural chemicals through the vadose zone and to the shallow groundwater system. A metal culvert (3.05 m dia and 3.65 m long) was installed vertically in the excavated cavity to provide a permanent structure. Stainless steel suction lysimeters were installed radially from the cavity wall to collect water samples for chemical analysis from the vadose zone and the shallow groundwater system at five depths in the soil profile. A monitoring system consisting of electronic tensiometers and a data logger were also installed to measure soil water pressure head at three depths in the vadose zone.<br /><br />A rainfall simulation experiment was conducted to test the performance of this large field monitoring system. Field data on the water and chemical transport through the vadose zone were collected during and after the rain simulation period. A rainfall of 127 mm was applied during a 7.5 h period over the area where suction lysimeters were installed at various depths. Chloride was applied with the rain water while bromide was applied to the soil surface (prior to rainfall) at a rate of 175 kg/ha. Metolachlor and metribuzin were applied at the experimental site three weeks prior to conducting this rainfall simulation experiment. Increased chloride concentrations were detected at 180 and 240 cm depths within three hours of initiating rainfall. Bromide was detected at 240 cm depth within three hours of initiating rainfall and increased from 0 to nearly 20 mg L–1 in about seven hours. Herbicide was detected at 120 cm depth in about an hour. Breakthrough curves for chloride and bromide indicated that preferential flow can cause rapid transport of agricultural chemicals to the shallow groundwater system. The results of this rainfall simulation study indicated that this field monitoring facility works well and has the potential for future field scale studies on chemical transport to shallow groundwater systems.</p>
dc.description.comments <p>This article is <em>Transactions of the ASAE</em> 40 (1997): 961–969, doi:<a href="http://dx.doi.org/10.13031/2013.21347" target="_blank">10.13031/2013.21347</a>. Posted with permission.</p>
dc.format.mimetype application/pdf
dc.identifier archive/lib.dr.iastate.edu/abe_eng_pubs/488/
dc.identifier.articleid 1774
dc.identifier.contextkey 5811405
dc.identifier.s3bucket isulib-bepress-aws-west
dc.identifier.submissionpath abe_eng_pubs/488
dc.identifier.uri https://dr.lib.iastate.edu/handle/20.500.12876/1259
dc.language.iso en
dc.source.bitstream archive/lib.dr.iastate.edu/abe_eng_pubs/488/1997_Olson_ConstructionTesting.pdf|||Sat Jan 15 00:28:41 UTC 2022
dc.source.uri 10.13031/2013.21347
dc.subject.disciplines Agriculture
dc.subject.disciplines Bioresource and Agricultural Engineering
dc.subject.disciplines Water Resource Management
dc.subject.keywords Bore hole cavity
dc.subject.keywords Suction lysimeter
dc.subject.keywords Preferential flow
dc.subject.keywords Rainfall simulation
dc.subject.keywords Caisson lysimeter
dc.title Constructing and Testing of a Facility for Measuring Water and Agrochemical Transport through the Vadose Zone
dc.type article
dc.type.genre article
dspace.entity.type Publication
relation.isAuthorOfPublication 5210e67e-b8da-4e17-be3f-843a09381196
relation.isOrgUnitOfPublication 8eb24241-0d92-4baf-ae75-08f716d30801
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