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Biochar amendment to soils with contrasting organic matter level: effects on N mineralization and biological soil properties

机译:生物炭对具有对比有机物质水平的土壤的修正:对氮矿化和生物土壤性质的影响

摘要

Four biochar types, produced by slow pyrolysis of poultry litter (PL) and pine chips (P) at 400 or 500°C, were added to two adjacent soils with contrasting soil organic matter (SOM) content (8.9 vs. 16.1 g C kg-1). The N mineralization rate was determined during 14-weeks incubations and assessments were made of the microbial biomass C, dehydrogenase activity and the microbial community structure (PLFA-extraction). The addition of PL biochars increased the net N mineralization (i.e. compared to the control treatment) in both soils while for treatments with P biochars net N immobilization was observed in both soils. Increasing the pyrolysis temperature of both feedstock types led to a decrease in net N mineralization. The ratio of Bacterial to Fungal PLFA biomarkers also increased with addition of biochars, and particularly in the case of the 500°C biochars. Next to feedstock type and pyrolysis temperature, SOM content clearly affected the assessed soil biological parameters, viz. net N mineralization or immobilization, MBC and dehydrogenase activity were all greater in the H soil. This might be explained by an increased chance of physical contact between the microbial community activated by SOM mineralization upon incubation and discrete biochar particles. However, when considering the H soil’s double C and N content, these responses were disproportionally small, which may be partly due to the L soil’s, somewhat more labile SOM. Nonetheless increasing SOM content and microbial biomass and activity generally appears to result in greater mineralization of biochar. Additionally, higher N mineralization after PL addition to the H soil with lower pH than the L soil can be due to the liming effect of the PL biochars.
机译:通过将家禽垫料(PL)和松木屑(P)在400或500°C下缓慢热解而产生的四种生物炭类型添加到两个相邻土壤中,土壤有机质(SOM)含量相反(8.9 vs. 16.1 g C kg -1)。在培养14周的过程中确定了氮矿化率,并对微生物生物量C,脱氢酶活性和微生物群落结构(PLFA提取)进行了评估。 PL生物炭的添加增加了两种土壤中的净氮矿化(即与对照处理相比),而P生物炭处理的两种土壤中均观察到了净氮固定化。两种原料的热解温度的升高导致净氮矿化的减少。细菌与真菌PLFA生物标志物的比例也随着生物炭的添加而增加,尤其是在500°C生物炭的情况下。除了原料类型和热解温度,SOM含量明显影响评估的土壤生物学参数,即。净氮矿化或固定化,MBC和脱氢酶活性在H土壤中均较高。可能是由于孵育后SOM矿化激活的微生物群落与离散的生物炭颗粒之间增加了物理接触的机会。但是,考虑到H土的C和N含量是其两倍时,这些响应会不成比例地减小,这可能部分是由于L土的SOM更不稳定。尽管如此,增加的SOM含量和微生物生物量及活性通常似乎导致生物炭矿化程度更高。另外,由于PL生物炭的石灰作用,PL添加到H土壤中比L土壤pH低的土壤中较高的N矿化作用。

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