Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045594039> ?p ?o ?g. }
Showing items 1 to 97 of
97
with 100 items per page.
- W2045594039 endingPage "125" @default.
- W2045594039 startingPage "117" @default.
- W2045594039 abstract "Abstract Determination of carbon and nitrogen levels in soils of ice-free areas of the Transantarctic Mountains, along with their origin, may determine whether these soils serve as a source or sink of carbon with an increasingly warmer climate. Organic and inorganic forms of carbon and nitrogen were measured in five soil chronosequences in the Transantarctic Mountains using flash combustion and spectrometry. Accumulation of coal carbon was significant in the Beardmore Glacier area and was quantified using chemi-thermal oxidation followed by flash combustion. Carbon levels decreased with drift age for two of the sequences. Decreases in carbon in the Hatherton Glacier sequence were due primarily to high levels of carbon in young ice-cored drifts. Carbon content increased with drift age for the Beardmore Glacier sequence due to the presence of coal in older drifts. Nitrogen content increased with age for a majority of the soil chronosequences. Inorganic carbon and all forms of nitrogen were significantly and positively correlated with mean annual precipitation. Our results suggest that carbon levels in similar settings do not significantly change over time; changes in temperature or moisture associated with microclimate likely play a much larger role in carbon and nitrogen levels." @default.
- W2045594039 created "2016-06-24" @default.
- W2045594039 creator A5046558580 @default.
- W2045594039 creator A5072421795 @default.
- W2045594039 date "2013-04-01" @default.
- W2045594039 modified "2023-10-14" @default.
- W2045594039 title "Carbon and nitrogen trends in soil chronosequences of the Transantarctic Mountains" @default.
- W2045594039 cites W1964113292 @default.
- W2045594039 cites W1964448751 @default.
- W2045594039 cites W1967572107 @default.
- W2045594039 cites W1976967435 @default.
- W2045594039 cites W1979549309 @default.
- W2045594039 cites W1985388258 @default.
- W2045594039 cites W1989880911 @default.
- W2045594039 cites W1991668322 @default.
- W2045594039 cites W1994956471 @default.
- W2045594039 cites W2002311269 @default.
- W2045594039 cites W2002824385 @default.
- W2045594039 cites W2006977237 @default.
- W2045594039 cites W2013372631 @default.
- W2045594039 cites W2014391597 @default.
- W2045594039 cites W2019416940 @default.
- W2045594039 cites W2024105528 @default.
- W2045594039 cites W2030775529 @default.
- W2045594039 cites W2036548510 @default.
- W2045594039 cites W2059500851 @default.
- W2045594039 cites W2064945396 @default.
- W2045594039 cites W2077324266 @default.
- W2045594039 cites W2081490078 @default.
- W2045594039 cites W2085672579 @default.
- W2045594039 cites W2089348609 @default.
- W2045594039 cites W2091240280 @default.
- W2045594039 cites W2095065964 @default.
- W2045594039 cites W2095101268 @default.
- W2045594039 cites W2095320760 @default.
- W2045594039 cites W2103036892 @default.
- W2045594039 cites W2115626648 @default.
- W2045594039 cites W2174086427 @default.
- W2045594039 cites W4235322216 @default.
- W2045594039 cites W4238739564 @default.
- W2045594039 cites W4253274671 @default.
- W2045594039 doi "https://doi.org/10.1016/j.geoderma.2013.01.004" @default.
- W2045594039 hasPublicationYear "2013" @default.
- W2045594039 type Work @default.
- W2045594039 sameAs 2045594039 @default.
- W2045594039 citedByCount "14" @default.
- W2045594039 countsByYear W20455940392013 @default.
- W2045594039 countsByYear W20455940392014 @default.
- W2045594039 countsByYear W20455940392015 @default.
- W2045594039 countsByYear W20455940392016 @default.
- W2045594039 countsByYear W20455940392018 @default.
- W2045594039 countsByYear W20455940392021 @default.
- W2045594039 countsByYear W20455940392022 @default.
- W2045594039 countsByYear W20455940392023 @default.
- W2045594039 crossrefType "journal-article" @default.
- W2045594039 hasAuthorship W2045594039A5046558580 @default.
- W2045594039 hasAuthorship W2045594039A5072421795 @default.
- W2045594039 hasConcept C104779481 @default.
- W2045594039 hasConcept C11413529 @default.
- W2045594039 hasConcept C127313418 @default.
- W2045594039 hasConcept C140205800 @default.
- W2045594039 hasConcept C159390177 @default.
- W2045594039 hasConcept C178790620 @default.
- W2045594039 hasConcept C185592680 @default.
- W2045594039 hasConcept C1965285 @default.
- W2045594039 hasConcept C33923547 @default.
- W2045594039 hasConcept C537208039 @default.
- W2045594039 hasConceptScore W2045594039C104779481 @default.
- W2045594039 hasConceptScore W2045594039C11413529 @default.
- W2045594039 hasConceptScore W2045594039C127313418 @default.
- W2045594039 hasConceptScore W2045594039C140205800 @default.
- W2045594039 hasConceptScore W2045594039C159390177 @default.
- W2045594039 hasConceptScore W2045594039C178790620 @default.
- W2045594039 hasConceptScore W2045594039C185592680 @default.
- W2045594039 hasConceptScore W2045594039C1965285 @default.
- W2045594039 hasConceptScore W2045594039C33923547 @default.
- W2045594039 hasConceptScore W2045594039C537208039 @default.
- W2045594039 hasLocation W20455940391 @default.
- W2045594039 hasOpenAccess W2045594039 @default.
- W2045594039 hasPrimaryLocation W20455940391 @default.
- W2045594039 hasRelatedWork W1992551069 @default.
- W2045594039 hasRelatedWork W2037172680 @default.
- W2045594039 hasRelatedWork W2087538975 @default.
- W2045594039 hasRelatedWork W2136841410 @default.
- W2045594039 hasRelatedWork W2314126381 @default.
- W2045594039 hasRelatedWork W2319087986 @default.
- W2045594039 hasRelatedWork W2359257389 @default.
- W2045594039 hasRelatedWork W2466518545 @default.
- W2045594039 hasRelatedWork W3168136444 @default.
- W2045594039 hasRelatedWork W4245982027 @default.
- W2045594039 hasVolume "197-198" @default.
- W2045594039 isParatext "false" @default.
- W2045594039 isRetracted "false" @default.
- W2045594039 magId "2045594039" @default.
- W2045594039 workType "article" @default.