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大型真菌子实体分解导致的氨形成和土壤pH值升高。

Ammonia formation and soil pH increase caused by decomposing fruitbodies of macrofungi.

作者信息

Ingelög T, Nohrstedt H-Ö

机构信息

Department of Ecology and Environmental Research, Swedish University of Agricultural Sciences, S-750 07, Uppsala, Sweden.

The Forestry Research Institute of Sweden, P.O. Box 7007, S-750 07, Uppsala, Sweden.

出版信息

Oecologia. 1993 Mar;93(3):449-451. doi: 10.1007/BF00317891.

Abstract

The formation of gaseous compounds from decomposing fruibodies of three common macrofungi was qualitatively analysed. It was shown that significant production of ammonia took place. When the fruitbodies were decomposing on the surface of a podzolic forest floor more than 90% of the ammonia produced was absorbed by the soil, causing soil pH to increase.

摘要

对三种常见大型真菌子实体分解过程中气态化合物的形成进行了定性分析。结果表明,有大量氨气产生。当子实体在灰化森林土壤表面分解时,产生的氨气90%以上被土壤吸收,导致土壤pH值升高。

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