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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...
Guardat en:
| Publicat a: | Biogeochemistry |
|---|---|
| Autors principals: | , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Springer International Publishing
2015
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4512732/ https://ncbi.nlm.nih.gov/pubmed/26213432 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1007/s10533-015-0097-0 |
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