Depletion of soil carbon and aggregation after strong warming of a subarctic Andosol under forest and grassland cover
<p>The net loss of soil organic carbon (SOC) from terrestrial ecosystems is a likely consequence of global warming and may affect key soil functions. The strongest changes in temperature are expected to occur at high northern latitudes, with forest and tundra as prevailing land cover types. Ho...
Main Authors: | C. Poeplau, P. Sigurðsson, B. D. Sigurdsson |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2020-03-01
|
Series: | SOIL |
Online Access: | https://www.soil-journal.net/6/115/2020/soil-6-115-2020.pdf |
Similar Items
-
Impact of Soil Warming on the Plant Metabolome of Icelandic Grasslands
by: Albert Gargallo-Garriga, et al.
Published: (2017-08-01) -
Soil Organic Carbon Depletion from Forests to Grasslands Conversion in Mexico: A Review
by: Deb Raj Aryal, et al.
Published: (2018-11-01) -
Biogeochemistry of Icelandic Andosols
by: Guicharnaud, Rannveig A.
Published: (2009) -
Oxygen depletion in subarctic peatland thaw lakes
by: Bethany N. Deshpande, et al.
Published: (2017-06-01) -
Insect herbivory dampens Subarctic birch forest C sink response to warming
by: Tarja Silfver, et al.
Published: (2020-05-01)