“…They mainly differed at the end of the sampling period in total organic carbon content (10.9, 13.1, and 13.2 g·kg −1 ), volumetric soil water content (0.19, 0.23, and 0.25 cm 3 ·cm −3 ), total N (1.23, 1.30, and 1.46 g·kg −1 ), and Olsen available P (37.2, 32.5, and 39.9 mg·kg −1 for the CT-, DS-, and DSC-soils, respectively). The differences were significant for all these parameters in the three soils, and positive correlations had previously been found between the amount of soil microorganisms and the organic carbon or water content [39].…”