Contribution of carbonate weathering to the CO(2) efflux from temperate forest soils

Temperate forests provide favorable conditions for carbonate bedrock weathering as the soil CO(2) partial pressure is high and soil water is regularly available. As a result of weathering, abiotic CO(2) can be released and contribute to the soil CO(2) efflux. We used the distinct isotopic signature...

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Detalles Bibliográficos
Autores principales: Schindlbacher, Andreas, Borken, Werner, Djukic, Ika, Brandstätter, Christian, Spötl, Christoph, Wanek, Wolfgang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer International Publishing 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4512732/
https://www.ncbi.nlm.nih.gov/pubmed/26213432
http://dx.doi.org/10.1007/s10533-015-0097-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4512732/
https://www.ncbi.nlm.nih.gov/pubmed/26213432
http://dx.doi.org/10.1007/s10533-015-0097-0

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