期刊
INTERNATIONAL JOURNAL OF WILDLAND FIRE
卷 13, 期 2, 页码 195-199出版社
CSIRO PUBLISHING
DOI: 10.1071/WF03068
关键词
soil heating; aggregate stability; water repellency; hydrophobicity; pore size distribution; hydraulic conductivity; organic matter
类别
Two forest soils rich in organic matter but differing in texture (sandy loam and silty loam) were heated under controlled laboratory conditions in order to examine the consequences of the heating effect that accompanies the passage of a fire on the physical properties of soil. Three samples of both soils were heated for 30 min in a muffle furnace at temperatures of 25, 170, 220, 380 and 460degreesC. At each temperature, the following parameters were determined: dry aggregate size distribution, water aggregate stability, total porosity, pore size distribution, water repellency and hydraulic conductivity. Heating the soils at 170 and 220degreesC caused no significant changes in aggregate size distribution or total porosity but increased water aggregate stability and the volume of pores 0.2-30 mum. Also, increased water repellency and strongly decreased the hydraulic conductivity. All parameters underwent much more dramatic changes at 380 and 460degreesC that can be ascribed to the combustion of organic matter. At such temperatures, water repellency was destroyed and the low hydraulic conductivity can be attributed to the aggregate breakdown observed under dry and wet conditions.
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