One gram of each soil sample was serially diluted.
Three kg of each soil was mixed with biochar treatments.
The descriptions of each soil type were compared with statistical analyses of laboratory data of each soil type and a semidetailed land characterization of the area.
All the experiments of each soil were carried out in triplicate.
One gram of each soil sample was suspended in 9 mL of sterilized distilled water.
The behavior observed in Fig. 3 can be interpreted from the physicochemical characteristics of each soil.
Descriptive statistics of each soil variable revealed that soil properties in UGS varied widely (Table 1).
The base of each soil pit was leveled with its original soil.
The data of each soil profile were analyzed considering the completely randomized design, with seven replicates.
The representative locations of each soil layer could be used to estimate the mean SWC well.
The pore structure of each soil layer was studied by the mercury intrusion porosimetry test (MIP) and the pore distribution of each soil layer was studied by the fractal theory.
