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机构地区:[1]竹类病虫防控与资源开发四川省重点实验室,四川乐山614004 [2]乐山师范学院生命科学学院,四川乐山614004
出 处:《暨南大学学报(自然科学与医学版)》2017年第5期462-466,共5页Journal of Jinan University(Natural Science & Medicine Edition)
基 金:国家自然科学基金资助项目(31500346);竹类病虫防控与资源开发四川省重点实验室项目(17ZZ004;17ZZ005)
摘 要:目的:全面了解冬季高山土壤循环过程,为全球气候变化下生物种群和分布的变化提供技术支持.方法:采用室内模拟冻融的方法,研究了不同冻融处理(-2℃,-2~2℃,-20~2℃)对土壤微生物数量和活性的影响.结果:研究发现,持续的冻结(-2℃)降低了土壤细菌数量、微生物总数量和微生物生物量碳氮含量.剧烈的冻融(-20~2℃)降低了蔗糖酶活性,而温和的冻融(-2~2℃)则增加了细菌数量、微生物总数量和纤维素酶、过氧化氢酶活性.结论:适当的冻融可以通过改善土壤微生物数量和群落结构,从而对土壤营养物质的转化和植物群落的构建产生实质性的影响.Aim: In order to understand the alpine soil ecology process,to provide technical support for the change of biological population and distribution under the global climate change. Methods: The effects of different freezing-thawing treatments(-2 ℃,-2 ~ 2 ℃,-20 ~ 2 ℃) on the number of soil microorganism and activity were studied by simulated freeze-thaw in lab. Results: The results showed that the continuous frozen state reduced the number of bacteria, the number of total microbe, and microbial biomass carbon and nitrogen contents. The severe freeze-thaw decreased the activity of invertase, while moderate freeze-thaw increased the number of bacteria, the total number of microorganisms and the activity of cellulose and catalase. Conclusion: The results suggest that the appropriate freeze-thaw can improve the number of soil microbial and community structure,and thus have a substantial impact on the transformation of soil nutrients and the construction of plant communities.
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