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    • Rangeland Ecology & Management, Volume 60, Number 1 (January 2007)
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    Influence of 90 Years of Protection From Grazing on Plant and Soil Processes in the Subalpine of the Wasatch Plateau, USA

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    Author
    Gill, Richard A.
    Issue Date
    2007-01-01
    Keywords
    subalpine rangeland
    soil carbon
    grazing exclosures
    mineralizable carbon
    hydrology
    
    Metadata
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    Citation
    Gill, 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.
    Publisher
    Society for Range Management
    Journal
    Rangeland Ecology & Management
    URI
    http://hdl.handle.net/10150/643133
    DOI
    10.2111/05-236R2.1
    Additional Links
    https://rangelands.org/
    Abstract
    Human 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.
    Type
    text
    Article
    Language
    en
    ISSN
    0022-409X
    ae974a485f413a2113503eed53cd6c53
    10.2111/05-236R2.1
    Scopus Count
    Collections
    Rangeland Ecology & Management, Volume 60, Number 1 (January 2007)

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