FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2038459574> ?p ?o ?g. }

• W2038459574 endingPage "327" @default.
• W2038459574 startingPage "320" @default.
• W2038459574 abstract "Warmer regions generally exhibit greater rates of soil respiration and organic matter decomposition than colder regions. In the Great Plains of the United States, soil organic matter declines from the northern part of the region to the south, suggesting greater decomposition rates in areas with warmer temperatures. Our study used a regional data set of aboveground net primary production, soil organic carbon, soil texture, and climate to evaluate the environmental controls over areal patterns in decomposition rates, (k; expressed as grams per year per gram of initial mass), throughout the U.S. Great Plains. We conducted multiple regression analyses of steady-state k with respect to mean annual temperature, mean annual precipitation, and percentage soil clay content to examine both the combined and individual effects of these independent variables on regional decomposition rates. Our results indicated that precipitation contributes more than either temperature or soil texture to areal patterns of decomposition rates in the U.S. Great Plains, explaining >30% of the areal variability in k. Decomposition rates increased with increasing precipitation and with decreasing soil clay content. Temperature explained <8% of the regional variability in k. Ancillary analyses that related temperature and aboveground net primary production in the region indicated that plant productivity declines with increasing temperatures. This suggests that the reduction in soil organic matter to the south in the U.S. Great Plains may be due to reduced plant inputs rather than to increases in decomposition rates. The response of decomposition to temperature is probably constrained by moisture in this water-limited region. Therefore, changes in decomposition rates resulting from temperature dynamics are likely to be minimal unless they are accompanied by sufficient changes in precipitation." @default.
• W2038459574 created "2016-06-24" @default.
• W2038459574 creator A5005851906 @default.
• W2038459574 creator A5011342074 @default.
• W2038459574 creator A5027055807 @default.
• W2038459574 date "2002-02-01" @default.
• W2038459574 modified "2023-10-10" @default.
• W2038459574 title "REGIONAL PATTERNS OF DECOMPOSITION AND PRIMARY PRODUCTION RATES IN THE U.S. GREAT PLAINS^*" @default.
• W2038459574 cites W1530186548 @default.
• W2038459574 cites W1964589705 @default.
• W2038459574 cites W1968331277 @default.
• W2038459574 cites W1972550021 @default.
• W2038459574 cites W1974951470 @default.
• W2038459574 cites W1984000471 @default.
• W2038459574 cites W1989324207 @default.
• W2038459574 cites W1989949238 @default.
• W2038459574 cites W1993038060 @default.
• W2038459574 cites W1994954836 @default.
• W2038459574 cites W1995024181 @default.
• W2038459574 cites W1997567356 @default.
• W2038459574 cites W2000736780 @default.
• W2038459574 cites W2000804828 @default.
• W2038459574 cites W2000972784 @default.
• W2038459574 cites W2002498775 @default.
• W2038459574 cites W2004380929 @default.
• W2038459574 cites W2004813502 @default.
• W2038459574 cites W2010267689 @default.
• W2038459574 cites W2013041530 @default.
• W2038459574 cites W2014461778 @default.
• W2038459574 cites W2014780221 @default.
• W2038459574 cites W2017701964 @default.
• W2038459574 cites W2018672425 @default.
• W2038459574 cites W2018815339 @default.
• W2038459574 cites W2020971327 @default.
• W2038459574 cites W2024415358 @default.
• W2038459574 cites W2024926004 @default.
• W2038459574 cites W2026401710 @default.
• W2038459574 cites W2029909553 @default.
• W2038459574 cites W2033946197 @default.
• W2038459574 cites W2034159032 @default.
• W2038459574 cites W2035351022 @default.
• W2038459574 cites W2039832476 @default.
• W2038459574 cites W2043986368 @default.
• W2038459574 cites W2052691919 @default.
• W2038459574 cites W2053296331 @default.
• W2038459574 cites W2054403544 @default.
• W2038459574 cites W2059248319 @default.
• W2038459574 cites W2062637792 @default.
• W2038459574 cites W2065086590 @default.
• W2038459574 cites W2070380004 @default.
• W2038459574 cites W2070413911 @default.
• W2038459574 cites W2070639535 @default.
• W2038459574 cites W2078506217 @default.
• W2038459574 cites W2089940084 @default.
• W2038459574 cites W2091179790 @default.
• W2038459574 cites W2094895535 @default.
• W2038459574 cites W2103958763 @default.
• W2038459574 cites W2107199069 @default.
• W2038459574 cites W2114627689 @default.
• W2038459574 cites W2117160001 @default.
• W2038459574 cites W2118710522 @default.
• W2038459574 cites W2127486632 @default.
• W2038459574 cites W2141646072 @default.
• W2038459574 cites W2144261495 @default.
• W2038459574 cites W2154652352 @default.
• W2038459574 cites W2163906077 @default.
• W2038459574 cites W2246020467 @default.
• W2038459574 cites W2331160901 @default.
• W2038459574 cites W2464646929 @default.
• W2038459574 doi "https://doi.org/10.1890/0012-9658(2002)083[0320:rpodap]2.0.co;2" @default.
• W2038459574 hasPublicationYear "2002" @default.
• W2038459574 type Work @default.
• W2038459574 sameAs 2038459574 @default.
• W2038459574 citedByCount "39" @default.
• W2038459574 countsByYear W20384595742012 @default.
• W2038459574 countsByYear W20384595742013 @default.
• W2038459574 countsByYear W20384595742014 @default.
• W2038459574 countsByYear W20384595742015 @default.
• W2038459574 countsByYear W20384595742016 @default.
• W2038459574 countsByYear W20384595742017 @default.
• W2038459574 countsByYear W20384595742020 @default.
• W2038459574 countsByYear W20384595742021 @default.
• W2038459574 countsByYear W20384595742022 @default.
• W2038459574 countsByYear W20384595742023 @default.
• W2038459574 crossrefType "journal-article" @default.
• W2038459574 hasAuthorship W2038459574A5005851906 @default.
• W2038459574 hasAuthorship W2038459574A5011342074 @default.
• W2038459574 hasAuthorship W2038459574A5027055807 @default.
• W2038459574 hasConcept C100970517 @default.
• W2038459574 hasConcept C107054158 @default.
• W2038459574 hasConcept C110872660 @default.
• W2038459574 hasConcept C124681953 @default.
• W2038459574 hasConcept C127313418 @default.
• W2038459574 hasConcept C139719470 @default.
• W2038459574 hasConcept C153294291 @default.
• W2038459574 hasConcept C154414509 @default.
• W2038459574 hasConcept C158787203 @default.
• W2038459574 hasConcept C159390177 @default.

• next