## Abstract Subsurface flow through peat plays a critical role in the hydrology of organicβcovered, permafrost terrains, which occupy a large part the continental arctic, subβarctic, and boreal regions. Hillslope drainage in these terrains occurs predominantly through the active flow zone between t
β¦ LIBER β¦
Profiles of Water Content and Pore Size in Sphagnum and Peat, and their Relation to Peat Bog Ecology
β Scribed by Hayward, P. M.; Clymo, R. S.
- Book ID
- 120141882
- Publisher
- The Royal Society
- Year
- 1982
- Tongue
- English
- Weight
- 729 KB
- Volume
- 215
- Category
- Article
- ISSN
- 0080-4649
No coin nor oath required. For personal study only.
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