Sensible Heat Balance Measurements of Soil Water Evaporation beneath a Maize Canopy

dc.contributor.author Xiao, X.
dc.contributor.author Heitman, J. L.
dc.contributor.author Sauer, T. J.
dc.contributor.author Ren, T.
dc.contributor.author Horton, Robert
dc.contributor.department Department of Agronomy
dc.date 2018-01-25T07:53:42.000
dc.date.accessioned 2020-06-29T23:04:52Z
dc.date.available 2020-06-29T23:04:52Z
dc.date.issued 2014-01-01
dc.description.abstract <p>Soil water evaporation is an important component of the water budget in cropped fields; few methods are available for continuous and independent measurement. A sensible heat balance (SHB) approach has been demonstrated for continuously determining soil water evaporation under bare surface conditions. Applicability of SHB measurements beneath a crop canopy cover has not been evaluated. We tested SHB using heat-pulse sensors to estimate evaporation beneath a full maize (<em>Zea mays</em> L.) canopy. We also implemented a modified SHB approach incorporating below-canopy net radiation, which extended the range of conditions under which SHB is applicable. Evaporation was measured at three positions: row (R), interrow (I), and interrow with roots excluded (IE). Evaporation rates were generally small, averaging −1 across all dates, positions, and measurement methods during the drying period. The SHB evaporation estimates varied among R, I, and IE, with cumulative totals of 4.4, 7.4, and 7.9 mm, respectively, during a 12-d drying period. Lower soil water contents from plant water uptake reduced evaporation rates at R more appreciably with time than at the other positions; I and IE provided similar evaporation patterns. The SHB evaporation estimates at R and I were compared with microlysimeter data on 8 d. Correlation between approaches was modest (<em>r</em><sup>2</sup> = 0.61) but significant (<em>p</em> < 0.001) when compared separately at R and I positions. Correlation was improved (<em>r</em><sup>2</sup> = 0.81) when evaporation estimates were combined across positions, with differences between SHB and microlysimeters typically within the range of values obtained from microlysimeter replicates. Overall, the results suggest good potential for using SHB and modified SHB approaches to determine soil water evaporation in a cropped field. The SHB approach allowed continuous daily estimates of evaporation, separate from evapotranspiration and without destructive sampling.</p>
dc.description.comments <p>This article is published as Xiao, Xinhua, J. L. Heitman, T. J. Sauer, Tusheng Ren, and Robert Horton. "Sensible heat balance measurements of soil water evaporation beneath a maize canopy." Soil Science Society of America Journal 78, no. 2 (2014): 361-368. doi: <a href="http://dx.doi.org/10.2136" target="_blank">10.2136/sssaj2013.08.0371</a>. Posted with permission.</p>
dc.format.mimetype application/pdf
dc.identifier archive/lib.dr.iastate.edu/agron_pubs/397/
dc.identifier.articleid 1444
dc.identifier.contextkey 11409152
dc.identifier.s3bucket isulib-bepress-aws-west
dc.identifier.submissionpath agron_pubs/397
dc.identifier.uri https://dr.lib.iastate.edu/handle/20.500.12876/4750
dc.language.iso en
dc.source.bitstream archive/lib.dr.iastate.edu/agron_pubs/397/2014_Horton_SensibleHeat.pdf|||Fri Jan 14 23:56:34 UTC 2022
dc.source.uri 10.2136/sssaj2013.08.0371
dc.subject.disciplines Agriculture
dc.subject.disciplines Hydrology
dc.subject.disciplines Soil Science
dc.title Sensible Heat Balance Measurements of Soil Water Evaporation beneath a Maize Canopy
dc.type article
dc.type.genre article
dspace.entity.type Publication
relation.isAuthorOfPublication d3fb0917-6868-417e-9695-a010896cfafa
relation.isOrgUnitOfPublication fdd5c06c-bdbe-469c-a38e-51e664fece7a
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