Contribution of carbonate weathering to the CO2 efflux from temperate forest soils
Temperate forests provide favorable conditions for carbonate bedrock weathering as the soil CO2 partial pressure is high and soil water is regularly available. As a result of weathering, abiotic CO2 can be released and contribute to the soil CO2 efflux. We used the distinct isotopic signature of the...
| Main Authors: | , , , , , |
|---|---|
| Format: | Online |
| Language: | English |
| Published: |
Springer International Publishing
2015
|
| Online Access: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4512732/ |