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首页> 外文期刊>Acta Agriculturae Scandinavica. Section B, Soil and Plant Science >Seasonal dynamics of soil microbial biomass C shows close correlation with environmental factors in natural Fagus crenata forests
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Seasonal dynamics of soil microbial biomass C shows close correlation with environmental factors in natural Fagus crenata forests

机译:天然云杉林土壤微生物生物量碳的季节动态与环境因素密切相关

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Soil microbial biomass (C-mic) is an important factor regulating a number of ecosystem processes. In this study, we investigated seasonal variations in soil microbial biomass in natural climax beech (Fagus crenata) forests in a typical cold-temperate mountain region of Japan. Four permanent tower sites along an altitudinal gradient were selected and soil samples were collected once every month during the growing season of 2007. Soil microbial biomass (by fumigation-extraction method) and soil properties were later measured in the laboratory, while environmental factors (soil temperature, soil moisture) were continuously recorded in the field. Our results indicated large seasonal variations (130.4 similar to 5558.0 mu g g(-1)) in soil microbial biomass in beech forests - a range that is much larger than previously reported. Statistically significant correlations are noted between soil properties with C-mic, but largely due to spatial linkages. On the other hand, the environmental factors of soil temperature and especially soil moisture largely control seasonal variations in C-mic. Furthermore, pH could be an important factor influencing seasonal change in C-mic at the 20-30 cm deep soil layer. The study suggests no direct correlation between plant eco-physiology and soil microbial biomass in seasonal courses of the forests.
机译:土壤微生物生物量(C-mic)是调节许多生态系统过程的重要因素。在这项研究中,我们调查了日本典型冷温山区自然高潮山毛榉(Fagus crenata)森林土壤微生物生物量的季节性变化。在2007年的生长季节中,沿着高度梯度选择了四个永久性塔位,并每月收集一次土壤样品。后来在实验室中测量了土壤微生物量(通过熏蒸-萃取法)和土壤性质,而环境因素(土壤温度,土壤湿度)在田间连续记录。我们的结果表明,山毛榉森林中土壤微生物生物量的季节变化较大(130.4与5558.0μg(-1)相似),该范围比以前报道的要大得多。在土壤性质与C-mic之间存在统计学上的显着相关性,但主要是由于空间联系。另一方面,土壤温度尤其是土壤湿度的环境因素在很大程度上控制了C-mic的季节性变化。此外,pH可能是影响20-30 cm深土壤层C-mic季节变化的重要因素。研究表明,森林的季节性变化过程中植物生态生理学与土壤微生物生物量之间没有直接关系。

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