This paper describes the heat transfer mechanisms operating as heat moves d
ownward in the soil along steep temperature gradients during both wildfires
and prescribed fires. The transfer of heat downward in the upper part of t
he soil is enhanced by the vaporization and movement of water and organic c
ompounds. Available information on the changes in the chemistry of vaporize
d organic compounds is summarized and discussed. An operational theory desc
ribing the formation of a highly water repellent soil condition during Ale
is presented. The relationship between the formation of this fire-related w
atershed condition and subsequent surface runoff and erosion from wildland
ecosystems is explored. Worldwide literature describing fire-induced water
repellency is reviewed and summarized. (C) 2000 Elsevier Science B.V. All r
ights reserved.