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Effects of Seasonal Freeze-Thaw Cycles on Quantity of Soil Microbes in Subalpine Fir Forest

机译:季节冻融循环对亚高山杉木林土壤微生物量的影响

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Fir(Abies faxoniana) distributes widely in the alpine and subalpine region of western Sichuan.To understand effects of freeze-thaw events on soil microbial community,microbial number was investigated monthly in a fir forest,employing the method of lab freeze/thaw cycles in combination with field soil sampling.Bacterial and actinomycete number in soil decreased and fungal count increased after a seasonal freeze-thaw season cycle.Bacterial and fungal counts increased with the decreased altitude,while actinomycete count decreased with the decreased altitude.Different microbes had various change patterns with altitude in humus layer(AL), illuvial layer(BL) and parent material layer(CL). Compared with the 3 582 m altitude,bacterial count in the AL and CL at the 3 298 m altitude increased 4.2%and 7.0%,respectively,but that in the BL decreased 0.6%.Meanwhile,bacterial count increased 11.5%,3.5%and 2.1%in the AL,BL and CL at the 3 023 m altitude in comparison with the 3 298 m altitude,respectively.Fungi count in the AL,BL and CL increased by 10.5%,10.3%and 16.4%at the 3 298 m altitude in comparison with 3 582 m altitude,respectively,while it increased by 2.4%,1.7%and 3.5%at the 3 023 m altitude in comparison with 3 298 m altitude,respectively. Actinomycete count in the AL at the 3 298 m altitude increased by 0.7%than that at the 3 582 m altitude, but decreased 5.9%and 13.9%in the BL and CL.In the AL and BL,it increased 5.2%and 5.2% respectively at the 3 023 m altitude than that at the 3 298 m altitude,while in the CL it decreased 12.4%.These results were in agreement with the simulation freeze/thaw cycle experiment in lab.The results also revealed that the seasonal freeze-thaw cycle increased the ratio of soil fungi to bacteria. These results demonstrated that different microbial groups responded differentially to the seasonal freeze-thaw cycle,which may be an important ecological mechanism for maintaining the seasonal frozen ecosystem.
机译:FIR(ABIES FAXONIANA)在四川西部的高山和亚马尔彭地区广泛分销。要了解冻融事件对土壤微生物群落的影响,每月在杉木森林中调查微生物数量,采用实验室冷冻/解冻周期的方法与现场土壤采样组合。在季节性冻融季节周期后土壤中的细菌和放射性菌数减少,真菌计数增加。受海拔高度下降的细菌和真菌计数增加,而Altinomycete计数随着海拔的降低而降低。不同的微生物有各种变化腐殖质层(Al),光明层(BL)和母体材料层(CL)的图案。与3582米的高度相比,Al和Cl中的细菌计数分别增加4.2%和7.0%,但在BL中的增加0.6%,细菌计数增加11.5%,3.5%与3023米高度的3023米高度,在Al,Bl和Cl中的3298米高度相比,在Al,Bl和Cl中的2.1%,在3 298米处增加了10.5%,10.3%和16.4%与3 298米高度相比,海拔高度分别与3 582米的高度分别增加了2.4%,1.7%和3.5%。 Al在398米的Altinomycete计数比398米高度增加0.7%,但在Al和Bl中,BL和Cl.In的5.9%和13.9%下降,它增加了5.2%和5.2%分别在3 023米高度的3 298米高度,而在CL中,它降低了12.4%。这些结果与实验室的仿真冻结/解冻循环实验一致。结果也透露了季节性冻结 - 解冻循环增加了土壤真菌与细菌的比例。这些结果表明,不同的微生物基团差异地对季节性冻融循环差异,这可能是维持季节性冷冻生态系统的重要生态机制。

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