Distinct effects of biochar addition on soil macropore characteristics at different depths in a double-rice paddy field

Soil macropores largely control the water and nutrients transport as well as runoff processes in the soil. Biochar is fre-quently applied to soils to improve the macropore structure, but the effects remain controversial. To clarify depth -dependent soil macropore characteristics affected by biochar addition, the intact soil cores with a depth of 200 mm were collected from biochar-amended paddy field at addition rates of 0, 24, and 48 t ha-1 (CK, BC1, and BC2, respec-tively). The two biochar treatments did not change the overall soil pore indices (e.g., macroporosity, pore number, fractal dimension, and circularity), but showed distinct effects at different soil depths. At a soil depth of 0-50 mm, the biochar treatments had higher macroporosity (8.59-8.85 %) than CK (4.94 %) (p < 0.05), but relatively lower pore circularity (0.83-0.84) than CK (0.88) (p < 0.05). The connectivity of biochar treatments (88-97) was 9.5-10.4 times higher than that of CK (9.3). At a soil depth of 100-200 mm, the biochar treatments exhibited lower macroporosity, macropore number, connectivity, and fractal dimension than CK (p < 0.05). The macropore indices (ex-cept circularity) of BC1 were relatively higher than those of BC2 in the most soil depths. Whether biochar altered the soil macropore indices depended on the addition rate of biochar and soil depth. The expansion and occupying effects of biochar were dominant at soil depths of 0-50 and 100-200 mm, respectively; and the two effects were stronger in BC1 than in BC2. A combination of the expansion and occupying effects occurred at a soil depth of 50-100 mm. The distinct effects of biochar on soil pore structure at different depths could mitigate methane emission and nutrient runoff loss from the double-rice paddy. Therefore, soil depth-dependent macropore structure should be considered when assessing the influence of biochar on soil properties and the associated environmental effects.

Automated summary

This study investigates the effects of biochar on soil macropore characteristics, and finds that the effects of biochar vary with the addition rate and soil depth. In the surface soil, biochar treatments increase macroporosity but decrease circularity, while in deeper soil layers the opposite effects are observed. The expansion and occupying effects of biochar also differ at different depths. Therefore, the depth-dependent macropore structure should be considered when assessing the influence of biochar on soil properties and environmental effects.