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The relationships among microbial parameters and the rate of organic matter mineralization in forest soils, as influenced by forest type

机译:森林类型对微生物参数与森林土壤有机质矿化速率的关系

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Vegetation type influences the rate of accumulation and mineralization of organic matter in forest soil, mainly through its effect on soil microorganisms. We investigated the relationships among forest types and microbial biomass C (MBC), basal respiration (R-B), substrate-induced respiration (R-s), N mineralization (N-min), specific growth rate mu, microbial eco-physiology and activities of seven hydrolytic enzymes, in samples taken from 25 stands on acidic soils and one stand on limestone, covering typical types of coniferous and deciduous forests in Central Europe. Soils under deciduous trees were less acidic than soils of coniferous forests, which led to increased mineralizing activities R-B and N-min, and a higher proportion of active microbial biomass (R-s/MBC) in the Of horizon. This resulted in more extractable organic C (0.5 M K2SO4) in soils of deciduous forests and a higher accumulation of soil organic matter (SUM) in coniferous forest soil. No effect of forest type on the microbial properties was detected in the Oh horizon and in the 0-10 cm layer. The microbial quotient (MBC/C-org), reflecting the quality of organic matter used for microbial growth, was higher in deciduous forests in all three layers. The metabolic quotient qCO(2) (R-B/MBC) and the specific growth rate mu, estimated using respiration growth curves, did not differ in soils of both forest types. Our results showed that the quality of SOM in coniferous forests supported microorganisms with higher activities of beta-glucosidase, cellobiosidase and beta-xylosidase, which suggested the key importance of fungi in these soils. Processes mediated by bacteria were probably more important in deciduous forest soils with higher activities of arylsulphatase and urease. The results from the stand on limestone showed that pH had a positive effect on microbial biomass and SUM mineralization. (C) 2014 Elsevier GmbH. All rights reserved.
机译:植被类型主要通过其对土壤微生物的影响来影响森林土壤中有机质的积累和矿化速率。我们调查了森林类型与微生物生物量碳(MBC),基础呼吸(RB),底物诱导的呼吸(Rs),氮矿化(N-min),比生长率mu,微生物生态生理和7种活动之间的关系。水解酶是从酸性土壤中的25种林分和石灰石上的一种林分中采集的,样品覆盖了中欧典型的针叶和落叶林。落叶树下的土壤比针叶林的土壤酸性弱,这导致矿化活性R-B和N-min增加,并且Of地平线中活性微生物生物量(R-s / MBC)的比例更高。这导致了落叶林土壤中可提取的有机碳(0.5 M K2SO4)更多,而针叶林土壤中土壤有机质(SUM)的积累更高。在Oh地平线和0-10 cm层中未检测到森林类型对微生物特性的影响。反映所有微生物生长所用有机物质量的微生物商(MBC / C-org)在所有三层落叶林中均较高。使用呼吸生长曲线估算的代谢商qCO(2)(R-B / MBC)和比生长率μ在两种森林类型的土壤中都没有差异。我们的结果表明,针叶林中SOM的质量支持具有更高活性的β-葡萄糖苷酶,纤维二糖苷酶和β-木糖苷酶的微生物,这表明真菌在这些土壤中具有至关重要的作用。细菌介导的过程在落叶林土壤中可能更重要,而落叶林土壤中的芳基硫酸酯酶和脲酶活性较高。石灰石摊位的结果表明,pH值对微生物生物量和SUM矿化有积极影响。 (C)2014 Elsevier GmbH。版权所有。

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