[Distribution and sequestration of straw carbon in surface and deep soil aggregates under different fertilization treatments]

Long-term fertilization causes the differences in water, heat, nutrients and microbial activities between topsoil and deep soil, with consequences on the decomposition and turnover of straw carbon (C) in soils. At a long-term positioning experimental station in Shenyang Agricultural University, we mixed the topsoil (0-20 cm) and deep soil (40-60 cm) samples from different fertilization treatments with长期施肥引起表层和深层土壤水、热、养分和微生物活性的分异,进而影响秸秆碳在土壤中的分解和周转过程。本研究基于沈阳农业大学长期定位实验站,分别将不同施肥处理表层(0～20 cm)和深层(40～60 cm)土壤与