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Soil carbon and nitrogen pools and microbial properties in a 6-year-old slash pine plantation of subtropical Australia: impacts of harvest residue management.

机译:亚热带澳大利亚6年生阔叶松人工林的土壤碳和氮库及微生物特性:收获物残留管理的影响。

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摘要

Harvest residue management can affect the dynamics of soil carbon (C) and nutrient pools and associated soil microbial processes. A field experiment was conducted to investigate the impacts of harvest residue management practices on soil C and nitrogen (N) pools in a slash pine plantation grown on a sandy soil of subtropical Australia. Results showed that harvest residue retention significantly enhanced accumulation of soil total C and N compared with residue removal. The NH4+-N was the predominant form of soil mineral N, and there were no significant impacts of residue management practices on concentrations of soil NH4+-N measured at the time of sampling. Concentrations of water-soluble and hot water extractable organic C and total N tended to be higher in soil with residue retention compared with residue removal, but this trend was only significant for hot water extractable organic C (HWEOC) in surface soil (0-10 cm). Residue retention also tended to increase soil microbial biomass C and N, but did not significantly affect soil respiration and metabolic quotient (qCO2). Direct C and N inputs into soil from the residue layer and moderation of the variation of soil moisture and temperature over the seasons by harvest residue cover might have contributed to the accumulation of soil C and N and microbial biomass with the residue retention treatments. The lack of statistically significant differences in some of soil microbial properties (e.g. microbial biomass C, respiration, etc.) might have been related to a large spatial variability among replicate plots at the experimental site.
机译:收获残余物管理会影响土壤碳(C)和养分池的动态以及相关的土壤微生物过程。进行了野外试验,以研究收获物残留管理措施对在亚热带澳大利亚沙质土壤上生长的阔叶松人工林中土壤碳和氮(N)库的影响。结果表明,与去除残留物相比,收获物残留物的保留显着提高了土壤总碳和氮的积累。 NH4 + -N是土壤矿质N的主要形式,残留管理措施对采样时测得的土壤NH4 + -N浓度没有显着影响。与残留物去除相比,具有残留物保留的土壤中水溶性和热水可提取有机碳的浓度及总氮含量往往较高,但这种趋势仅对表层土壤中的热水可提取有机碳(HWEOC)有意义(0-10厘米)。残留物保留也倾向于增加土壤微生物生物量碳和氮,但并未显着影响土壤呼吸和代谢商(qCO2)。碳和氮从残渣层直接输入土壤,并通过收获残渣覆盖减轻季节内土壤水分和温度的变化,可能通过残渣保留处理促进了土壤碳,氮和微生物生物量的积累。在某些土壤微生物特性(例如微生物生物量C,呼吸作用等)方面缺乏统计学上显着的差异可能与实验地点的重复样地之间较大的空间变异性有关。

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