Abstract

The aim of this study was to determine how carbon (C) mineralization of acacia (Acacia cyanophylla, Fabaceae) soil are affected by the different temperature (23°C and 28°C) and humidity (80% and 60% of their field capacity) conditions in the laboratory. The acacia soils were collected from Cukurova University campus in the eastern Mediterranean region of Turkey. C mineralization of all soils was determined using CO 2 respiration method. The microbial activity increased together with temperature increases. The microbial activity in the soils humidified to 80% of field capacity was significantly different from field capacity and 60% of field capacity at both 23°C and 28°C temperatures (p<0.001). The ratios (%) of C mineralization of 80% of field capacity at 23°C and 28°C were also significantly higher than all of the others (p<0.001). These findings might suggest that 80% of field capacity of acacia soil is better humidity for microbial activity at both 23°C and 28°C temperatures into 30 days.

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