矿化(土壤科学)
土壤水分
化学
微生物
孵化
微生物种群生物学
土壤呼吸
营养物
环境化学
耕地
农学
动物科学
生态学
生物
细菌
生物化学
农业
有机化学
遗传学
作者
Zhongwang Jing,Ruirui Chen,Shiping Wei,Youzhi Feng,Jiabao Zhang,Xiangui Lin
标识
DOI:10.1016/j.soilbio.2016.11.014
摘要
Despite our current understanding of soil C and N interactions, less is known about the response and feedback of C mineralization to soil P availability driven by microorganisms. To better understand these interactions, soils with long-term P-sufficient NPK fertilization (available P: 13.4 mg kg−1) and P-deficient NK fertilization (available P: 0.96 mg kg−1) were incubated with and without glucose. CO2 emissions were monitored to characterize C mineralization during the incubation. The soil bacterial community structure, quantity and metabolic activity were evaluated using high-throughput sequencing, qPCR and microcalorimetric dynamics. Compared with P-sufficient soils, P-deficient soils had significantly lower basal respiration, but a significantly higher net mineralization of added glucose, probably due to higher energy cost of soil microorganisms. Glucose addition promoted microbial biomass and activity, particularly in P-deficient soils, and this improvement was maintained for at least 70 days. Shifts in bacterial community composition were induced by a predominance of several specific taxonomic groups, all of which were capable of solubilizing P in soils. P-deficiency decreases the retention of exogenous labile C into soil. Adding labile C to P-deficient soils may shift P from relatively unavailable soil-bound pools into microbial biomass pools through pool cycling. Our results indicated negative effects of P-deficiency on soil C retention, as well as positive effects of labile C on soil P availability in arable soils.
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