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首页> 外文期刊>Soil & Tillage Research >Soil compaction and forest litter amendment affect carbon and net nitrogen mineralization in a boreal forest soil.
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Soil compaction and forest litter amendment affect carbon and net nitrogen mineralization in a boreal forest soil.

机译:土壤压实和森林凋落物改良会影响北方森林土壤中的碳和净氮矿化。

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摘要

Mechanical site preparation in forests often results in soil compaction, mixing of forest litter with mineral soil, and/or displacement of surface organic material in forest ecosystems. We used a 9-month laboratory incubation experiment to examine the effects of soil compaction and forest litter amendment on microbial biomass C (MBC) and N (MBN), soluble organic C and N, and C and net N mineralization rates in a boreal forest soil with a silt loam texture. Four treatments: forest litter unamended and noncompacted (OM0C0, bulk density at 1.1 Mg m-3), forest litter unamended and compacted (OM0C1, 1.5 Mg m-3), forest litter amended and noncompacted (OM1C0), and forest litter amended and compacted (OM1C1) were applied to the soil. Soil compaction reduced MBC, MBN, soluble organic C and N on several sampling dates. Carbon mineralization and net nitrification rates were reduced by soil compaction whether forest litter was amended or not. The total amount of C mineralized from OM0C0, OM0C1, OM1C0, and OM1C1 in 9-month was 1.8, 1.6, 2.6 and 1.7 mg C g-1 soil, respectively. Forest litter amendment alone increased MBC in the early stage of the incubation and soluble organic C and N on every sampling date except the initial one. Forest litter amendment had a positive priming effect on C and net N mineralization and nitrification rates. The total amount of N mineralized from OM0C0, OM0C1, OM1C0, and OM1C1 was 40, 39, 61, and 59 mg N kg-1 soil, respectively. We conclude that soil compaction and forest litter amendment influenced microbial properties and processes in this boreal forest soil under controlled conditions. Our results imply that forest management practices that alter soil porosity (through compaction) and organic matter distribution in the soil profile can dramatically change soil C and N dynamics that may result in the eventual change in soil C and N concentrations or availability..
机译:在森林中进行机械现场准备通常会导致土壤压实,森林凋落物与矿物土壤的混合和/或森林生态系统中表面有机物质的置换。我们使用了一个为期9个月的实验室孵化实验,研究了土壤压实和森林凋落物改良对北方森林中微生物生物量碳(MBC)和氮(MBN),可溶性有机碳和氮以及碳和净氮矿化率的影响淤泥质壤土的土壤。四种处理方法:未改性和未压实的森林凋落物(OM0C0,密实度为1.1 Mg m-3),未改性和压实的森林凋落物(OM0C1,1.5 Mg m-3),未改性和未压缩的森林凋落物(OM1C0)以及已改性和未压缩的森林凋落物压实(OM1C1)应用于土壤。在几个采样日期,土壤压实降低了MBC,MBN,可溶性有机碳和氮。无论是否对森林凋落物进行修正,土壤压实都会降低碳矿化和净硝化率。在9个月中,从OM0C0,OM0C1,OM1C0和OM1C1矿化的C总量分别为1.8、1.6、2.6和1.7 mg C g-1土壤。在孵化初期,仅森林凋落物改良剂就增加了MBC,除最初的采样日期外,每个采样日均增加了可溶性有机碳和氮。森林凋落物改良剂对碳和净氮矿化和硝化速率具有积极的启动作用。从OM0C0,OM0C1,OM1C0和OM1C1矿化的N总量分别为40、39、61和59 mg N kg-1土壤。我们得出结论,在受控条件下,土壤压实和森林凋落物改良会影响这种北方森林土壤的微生物特性和过程。我们的结果表明,森林管理实践会改变土壤孔隙度(通过压实)和土壤剖面中有机物的分布,从而极大地改变土壤碳和氮的动态,从而最终改变土壤碳和氮的浓度或可用性。

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