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Dynamics of C, N, P and microbial community composition in particulate soil organic matter during residue decomposition

机译:残留物分解过程中颗粒土壤有机质中C,N,P和微生物群落组成的动态

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Decomposing residues can be an important source of nutrients for plants, especially of N and P, but the relationship between N and P release and microbial community dynamics have rarely been studied. Two pea (Pisum sativum L.) residues with contrasting chemical composition, shoots from flowering pea (Pea-Y) with 2.9 mg P and 36 mg N kg-p# and from mature pea (Pea-M) with 0.3 mg P and 13 mg N kg-p#, were added at a rate of 20 g kg soil-p# to a sandy soil low in nutrients. Particulate organic matter (POM) was isolated on days (d) 0, 5, 15, 28, 42 and 61 after residue addition and analysed for C, N, P and microbial community structure (fatty acid methyl ester analysis). The recovery of POM from residue-amended soils decreased over time to 30-40% of added amounts for both residues. Apart from d 0, the N concentration in POM was lower in residue-amended soil than in the control. Due to a rapid decrease in P concentration during the first 5 days in Pea-Y and a slow increase over the whole experiment in Pea-M, P concentrations in POM on d 61 were similar in all treatments. In Pea-Y, the dynamics of C, N and P were coupled, with amounts of C, N and P decreasing during the first 15 days and remaining stable thereafter. In Pea-M, a steady loss of C from POM was contrasted by a slight increase in P. As a result, the C/P ratio decreased from 1,330 on d 0 to 390 on d 61. The C/N ratio of Pea-M decreased only during the second phase of decomposition. The different nutrient dynamics in Pea-Y and Pea-M led to similar amounts of N and P in POM towards the end of the incubation. Microbial community composition in the POM in Pea-Y and Pea-M remained distinct from the control, even though it changed over time. POM was shown to be an important source of potentially available nutrients after addition of plant residues. In the unamended soil, stable nutrient amounts in POM suggested very low net nutrient release from native POM compared to POM after residue addition.
机译:分解残留物可能是植物尤其是氮和磷的重要养分来源,但很少研究氮和磷释放与微生物群落动态之间的关系。化学成分相反的两个豌豆(Pisum sativum L.)残留物,分别是2.9 mg P和36 mg N kg-p#的开花豌豆(Pea-Y)和0.3 mg P和13的成熟豌豆(Pea-M)的芽以20 g kg·kg·p#的量向低养分的沙质土壤中添加mg·N·kg·p#。添加残渣后第0、5、15、28、42和61天(d)分离出颗粒有机物(POM),并分析其C,N,P和微生物群落结构(脂肪酸甲酯分析)。随着时间的推移,残留物改良土壤中POM的回收率下降至两种残留物添加量的30-40%。除d 0以外,残留物改良土壤中POM中的N浓度低于对照。由于在Pea-Y的前5天中P浓度快速下降,而在整个Pea-M中整个实验缓慢增加,因此在第61天,所有处理中POM中的P浓度均相似。在Pea-Y中,C,N和P的动力学耦合在一起,其中C,N和P的数量在前15天中减少,此后保持稳定。在Pea-M中,P的轻微增加形成了C从POM稳定损失的结果。结果,C / P比从d 0的1,330降低到d 61的390。 M仅在分解的第二阶段降低。在培养结束时,豌豆-Y和豌豆-M中不同的营养动力学导致POM中N和P的含量相似。尽管豌豆-Y和豌豆-M的微生物群落组成随时间而变化,但仍与对照区分开来。添加植物残渣后,POM被证明是潜在可用养分的重要来源。在未改良的土壤中,与添加残渣后的POM相比,POM中稳定的养分含量表明从天然POM释放的净养分非常低。

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