Effect of soil macroaggregates crushing on C mineralization in a tropical deciduous forest ecosystem

Soil aggregates strongly influence C dynamics by affecting microbial activity. Our study tested the effect of soil crushing on C mineralization by laboratory incubation experiments of soil samples from a tropical deciduous forest ecosystem in Western Mexico. Soil samples were taken in January (dry season) and in October (rainy season). For each sampling date, the incubation experiment had a two factorial design with litter and macroaggregates (>250 μm) crushing as the main factors, both with two levels (with and without). At both sampling dates, the soil samples with intact macroaggregates had significantly higher C mineralization than the soil samples in which macroaggregates were crushed. The pH of leached solution was higher in the crushed soil samples than in uncrushed soil samples. The reduction of C mineralization caused by the disruption of soil aggregates is explained by the disturbance of environmental conditions within macroaggregates. The effect of macroaggregates crushing also reduced the differences of C mineralization between both seasons. We concluded that macroaggregates promote microbial activity by reducing the impact of variations in soil chemical and physical environmental conditions.