Winter soil freeze-thaw cycles lead to reductions in soil microbial biomass and activity not compensated for by soil warming

环境科学 矿化(土壤科学) 生长季节 融雪 土壤呼吸 土壤水分 农学 氮气循环 生物量(生态学) 高山气候 微生物种群生物学 土壤碳 生态系统 自行车 生态学 化学 生物 土壤科学 地表径流 氮气 林业 物理 气象学 有机化学 遗传学 地理 细菌
作者
Patrick O. Sorensen,Adrien C. Finzi,Marc‐André Giasson,Andrew B. Reinmann,Rebecca Sanders‐DeMott,Pamela H. Templer
出处
期刊:Soil Biology & Biochemistry [Elsevier]
卷期号:116: 39-47 被引量:111
标识
DOI:10.1016/j.soilbio.2017.09.026
摘要

Air temperatures are rising and the winter snowpack is getting thinner in many high-latitude and high-elevation ecosystems around the globe. Past studies show that soil warming accelerates microbial metabolism and stimulates soil carbon (C) and nitrogen (N) cycling. Conversely, winter snow removal to simulate loss of snow cover leads to increased soil freezing and reductions in soil microbial biomass, exoenzyme activity, and N cycling. The Climate Change Across Seasons Experiment (CCASE), located at Hubbard Brook Experimental Forest, NH (USA) is designed to evaluate the combined effects of growing season soil warming and an increased frequency of winter soil freeze-thaw cycles on a northern forest ecosystem. Soils were collected from CCASE over two years (2014 and 2015) and extractable C and N pool sizes, as well as microbial biomass, exoenzymes, and potential net N mineralization and microbial respiration were measured. Soil warming alone did not stimulate microbial activity at any sampling time. Extractable amino acid N and organic C, proteolytic and acid phosphatase activity, and microbial respiration were reduced by the combination of warming in the growing season and winter soil freeze-thaw cycles during the period following snowmelt through tree leaf out in spring. The declines in microbial activity also coincided with an 85% decline in microbial biomass N at that time. Growing season warming and winter soil freeze-thaw cycles also resulted in a two-fold reduction in phenol oxidase activity and a 20% reduction in peroxidase activity and these declines persisted throughout the snow-free time of the year. The results from this study suggest that positive feedbacks between warming and rates of soil C and N cycling over the next 100 years will be partially mitigated by an increased frequency of winter soil freeze-thaw cycles, which decrease microbial biomass and rates of soil microbial activity.
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