Peatlands are characterised as habitats where waterlogged and low
oxygen conditions result in the accumulation of organic matter.
This organic material is the peat, the partially decomposed remains
of vegetation, and peat accumulations can be tens of meters deep,
with peat to at least 30 to 40 cm depth typically being used to
classify an ecosystem as a peatland. This book examines the
microbial ecology of peat swamp forests, new methods for the
waterproofing of construction materials with organic peat
compounds, and the fundamentals of obtaining sorption materials
from mineral peat-based compositions and their industrial
applications.
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