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Effects of amendment of different biochars on soil carbon mineralisation and sequestration

机译:不同生物炭的改良对土壤碳矿化和固存的影响

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The aim of this study was to determine the impact of addition of different biochars on soil carbon mineralisation and sequestration. Different biochars were produced from two types of feedstock, fresh dairy manure and pine tree woodchip, each of which was pyrolysed at 300, 500, and 700 degrees C. Each biochar was mixed at 5% (w/w) with a forest loamy soil and the mixture was incubated at 25 degrees C for 180 days, during which soil physicochemical properties and soil carbon mineralisation were measured. Results showed that the biochar addition increased soil carbon mineralisation at the early stage (within the first 15 days) because biochar brought available organic carbon to the soil and changed associated soil properties, such increasing soil pH and microbial activity. The largest increase in soil carbon mineralisation at the beginning of incubation was induced by the dairy manure biochar pyrolysed at 300 degrees C. Soil carbon mineralisation was enhanced more significantly by the dairy manure biochars than by the woodchip biochars, and the enhancement effect decreased with increasing pyrolysis temperature. Although the biochar addition induced increased soil carbon mineralisation at the beginning of the incubation, soil carbon mineralisation rates decreased sharply within a short time (within 15 days) and then remained very low afterwards. Carbon mineralisation kinetic modelling indicated that the stable organic matter in biochars could be sequestrated in soil for a long time and resulted in high levels of carbon sequestration, especially for the woodchip biochars pyrolysed from higher temperatures.
机译:这项研究的目的是确定添加不同生物炭对土壤碳矿化和固存的影响。由两种类型的原料生产不同的生物炭,分别是新鲜的奶牛粪便和松树木屑,它们分别在300、500和700摄氏度下热解。每种生物炭均以5%(w / w)的比例混合于森林沃土将混合物在25℃下孵育180天,在此期间测量土壤理化性质和土壤碳矿化。结果表明,生物炭的添加会在早期(前15天之内)增加土壤碳的矿化作用,因为生物炭将有效的有机碳带入土壤并改变了相关的土壤特性,例如增加了土壤的pH值和微生物活性。在孵化开始时,土壤碳矿化的最大增加是由300℃下热解的乳牛粪生物炭引起的。与木屑生物炭相比,乳牛粪生物炭对土壤碳矿化的增强作用更大,增强作用随木炭生物炭的增加而降低。热解温度。尽管在培养开始时添加生物炭会导致土壤碳矿化增加,但土壤碳矿化率在短时间内(15天之内)急剧下降,然后保持很低水平。碳矿化动力学模型表明,生物炭中的稳定有机物可以在土壤中长时间螯合,并导致高水平的碳螯合,尤其是高温下热解的木屑生物炭。

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