“…Microbial CH 4 oxidation depends on several abiotic variables such as the soil's water content, temperature, CH 4 concentration, oxygen (O 2 ) availability, and nutrients concentrations Bogner et al, 1997b;Börjesson et al, 1998a;Börjesson et al, 2004;Christophersen et al, 2000;Czepiel et al, 1996a;De Visscher et al, 2001;Figueroa, 1993;Hilger et al, 2000;Kightley et al, 1995;Nozhevnikova et al, 1993;Watzinger et al, 2005;Whalen et al, 1990). Less attention has been paid to soil texture and physical characteristics such as compaction and air-filled porosity (Figueroa, 1993;Kightley et al, 1995), which all affect the movement of gases in soil (Hillel, 1998) and thus CH 4 oxidation in the field.…”