『Abstract
After vegetation fires considerable amounts of severely or partly
charred necromass (referred to here as char) are incorporated
into the soil, with long-term consequences for soil C and N dynamics
and thus N availability for primary production and C and N transport
within the soil column. Considering results reported in the pyrolysis
literature in combination with those obtained from controlled
charring of plant materials and soil organic matter (SOM), it
has become clear that common models claiming char as a graphite-like
material composed mainly of highly condensed polyaromatic clusters
may be oversimplified,. Instead, I suggest a concept in which
char is a heterogeneous mixture of heat-altered biopolymers with
domains of relatively small polyaromatic clusters, but considerable
substition with N, O and S functional groups. Such a concept allows
fast oxidation facilitating both microbial attack and dissolution.
although, char is commonly believed to degrade more slowly than
litter, over the long term and under oxic conditions, char may
degrade to an extent that it becomes indistinguishable from naturally
formed SOM. Oxygen depletion or environments with low microbial
activity may be necessary for char to survive without major chemical
alteration and in considerable amounts for millennia or longer/
Keywords: Pyrolysis; Charcoal; Black carbon; Black nitrogen; Aromatic;
Alkyl』
Introduction
Ecological importance of vegetation fires past and present
Fire severity spectrum and temperature regime
Impact of fire on soil properties
Liming effect
Nutrient availability
Accumulation of hydrophobic compounds
Impact on soil biology and enzyme activity
Impact of fire on SOM content
Impact of fire on SOM quality
Cellulose and pectin
Lignin and chlorogenic acid
Proteins and amino acids
Maillard reaction
Charring of plants residues and SOM
Char content in soils
Chemical alteration of SOM in fire-affected soils
Direct effects on bulk soil organic carbon
Solubility of SOM
Alteration of the organic N fraction
Impact of recovery time
Stability of char
Conclusions
Molecular structure of char and its impact on char quantification
in SOM
Importance of “black nitrogen”
Charcoal structure and its short-term impact on SOM properties
Impact of char input on quality and quantity of SOM
Degradability and solubility of char residues
References