Carbon and nitrogen cycling in tundra soils - Churchill
The landscapes were divided into five landform units: (1) upper slope, (2) back slope, (3) lower slope, (4) hummock, and (5) interhummock, which represented a great diversity of Static and Turbic Cryosolic soils including Brunisolic, Gleysolic, and Organic subgroups. Soil gross N mineralization was...
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Format: | Dataset |
Language: | English |
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Canadian Cryospheric Information Network
2009
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Online Access: | https://dx.doi.org/10.5443/10960 https://www.polardata.ca/pdcsearch/?doi_id=10960 |