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Effects of elemental sulfur and soil compaction on microbial biomass carbon and soil enzyme activities

机译:元素硫和土壤压实对微生物生物量碳和土壤酶活性的影响

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The soil enzymes and microbial biomass play a key role in nutrient cycling and sensitivity to management and environmental change compared to most physical and chemical properties. Thus these parameters have been monitored as essential indicators of soil q uality. The aim of this study was to investigate the effects of sulfur and soil compaction on microbial biomass and enzyme activities. Therefore a greenhouse experiment was designed at four levels of sulfur (0, 500, 1000 and 2000kgha - 1 ) and three levels of compaction (C 0 , C 1 , C 2 ). Microbial biomass carbon, urease and arylsulphatase activities were determined. The results showed that application of different levels of sulfure dicreased microbial biomass carbon but urease and arylsulphatase activities dicreas ed at the highest levels of sulfur. Microbial biomass carbon and arylsulphatase activitiy were not influenced by soil compaction but the highest of soil compaction dicreased urease activity.
机译:与大多数物理和化学性质相比,土壤酶和微生物生物量在养分循环以及对管理和环境变化的敏感性方面起着关键作用。因此,这些参数已被监测为土壤质量的重要指标。这项研究的目的是调查硫和土壤压实对微生物生物量和酶活性的影响。因此,设计了一个温室实验,其硫含量为四个级别(0、500、1000和2000kgha-1),压实级别为三个级别(C 0,C 1,C 2)。测定了微生物生物量碳,脲酶和芳基硫酸酯酶的活性。结果表明,施用不同水平的硫会降低微生物的生物量碳,而脲酶和芳基硫酸酯酶的活性会降低最高的硫水平。微生物生物量碳和芳基硫酸酯酶的活性不受土壤压实的影响,但最高的土壤压实会降低脲酶的活性。

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