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Permafrost Thaw Causes Large Carbon Loss in Boreal Peatlands While Changes to Peat Quality are Limited
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Rapid, ongoing permafrost thaw of peatlands in the discontinuous permafrost zone is exposing a globally significant store of soil carbon (C) to microbial processes. Mineralization and release of this...
Reviewing and analyzing shrinkage of Peat and Other Organic Soils in Relation to Selected Soil Properties
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Peat and other organic soils (e.g., organo-mineral soils) show distinctive volume changes through desiccation and wetting. Important processes behind volume changes are shrinkage and swelling. There...
Video - Carbon Accumulation and the Return of Microbial Function in Soils
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The resource link will access Part 1 of this presentation. Part 2 can be accessed here. Mark Tibbett's presentation is focused around one question: can we change the amount of carbon in soil through...
Wetlands and Methane [Technical Report]
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To reduce global greenhouse gas emissions, conservation and restoration of wetlands play a key role. This report outlines the contribution of wetlands to global methane output; differences between...