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dc.contributor.authorGill, Richard A.
dc.date.accessioned2020-09-05T07:39:33Z
dc.date.available2020-09-05T07:39:33Z
dc.date.issued2007-01-01
dc.identifier.citationGill, R. A. (2007). Influence of 90 years of protection from grazing on plant and soil processes in the subalpine of the Wasatch Plateau, USA. Rangeland Ecology & Management, 60(1), 88-98.
dc.identifier.issn0022-409X
dc.identifier.doi10.2111/05-236R2.1
dc.identifier.urihttp://hdl.handle.net/10150/643133
dc.description.abstractHuman communities in the Intermountain West depend heavily on subalpine rangelands because of their importance in providing water for irrigation and forage for wildlife and livestock. In addition, many constituencies are looking to managed ecosystems to sequester carbon in plant biomass and soil C to reduce the impact of anthropogenic CO2 on climate. This work builds on a 90-year-old grazing experiment in mountain meadows on the Wasatch Plateau in central Utah. The purpose of this study was to evaluate the influence of 90 years of protection from grazing on processes controlling the input, output, and storage of C in subalpine rangelands. Long-term grazing significanty reduced maximum biomass in all years compared with plots within grazing enclosures. For grazed plots, interannual variability in aboveground biomass was correlated with July precipitation and temperature (R2 – 0.51), while there was a weak correlation between July precipitation and biomass in ungrazed plots (R2 – 0.24). Livestock grazing had no statistically sinificant impacts on total soil C or particulate organic matter (POM), although grazing did increase active soil C and decrease soil moisture. Grazing significantly incrased the proportion of total soil C pools that were potentially mineralizable in the laboratory, with soils from grazed plots evolving 4.6% of total soil C in 1 year while ungrazed plots lost 3.3% of total soil C. Volumetric soil moisture was consistently higher in ungrazed plots than grazed plots. The changes in soil C chemistry may have implications for how these ecosystems will respond to forecast climate change. Because grazing has resulted in an accumulation of easily decomposable organic material, if temperatures warm and summer precipitation increases as is anticipated, these soils may become net sources of CO2 to the atmosphere creating a positive feedback between climate change and atmospheric CO2.
dc.language.isoen
dc.publisherSociety for Range Management
dc.relation.urlhttps://rangelands.org/
dc.rightsCopyright © Society for Range Management.
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectsubalpine rangeland
dc.subjectsoil carbon
dc.subjectgrazing exclosures
dc.subjectmineralizable carbon
dc.subjecthydrology
dc.titleInfluence of 90 Years of Protection From Grazing on Plant and Soil Processes in the Subalpine of the Wasatch Plateau, USA
dc.typetext
dc.typeArticle
dc.identifier.journalRangeland Ecology & Management
dc.description.collectioninformationThe Rangeland Ecology & Management archives are made available by the Society for Range Management and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform August 2020
dc.source.volume60
dc.source.issue1
dc.source.beginpage88-98
refterms.dateFOA2020-09-05T07:39:33Z


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