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Summary:The movement of water in milled peat is of importance to the peat industry particularly in terms of rewetting. Considering the importance of structure with regard to water flow, micromorphology was used to obtain information regarding the nature of milled peat as a porous medium in a manner not available by other means. Peat was sampled from the undisturbed surface of two bogs (raised and fen origin) and from milled peat stockpiles. Thin sections were prepared to describe the nature of the two peat materials (milled and unmilled) in terms of the particle / pore properties and composition. Image analysis and point counting techniques were used to quantify results wherever possible. Although overall macro-porosity was similar for the two stockpiles, particle and pore size distributions varied considerably. Variations arose from the nature of the peat type and its interaction with milling operations with results suggesting that smaller pore sizes relate to a greater propensity to rewet.
ISSN:0032-079X
1573-5036
DOI:10.1023/a:1004709726449