首页> 外文期刊>Fresenius environmental bulletin >VARIATION OF SOIL ENZYME ACTIVITIES IN WETLANDS FROM PERMAFROST TO SEASONALLY FROZEN SOIL REGION IN NORTHEAST CHINA
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VARIATION OF SOIL ENZYME ACTIVITIES IN WETLANDS FROM PERMAFROST TO SEASONALLY FROZEN SOIL REGION IN NORTHEAST CHINA

机译:东北地区从多年冻土到季冻冻土地区土壤酶活性的变化

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Soil enzyme activities are sensitive indicators of soil organic matter (SOM) dynamics brought about by climate change. The distribution of soil enzyme activities in wetlands from different types of frozen region in Northeast China was evaluated in this paper. The results showed that the specific enzyme activities of P-glucosidase, invertase, dehydrogenase, urease, and acid phosphatase showed the highest values in seasonally frozen ground indicating faster turnover rate of SOM. Specific activities of invertase and acid phosphatase were higher in discontinuous permafrost than in continuous permafrost. The temperature, SOM and vegetation species regulated soil enzyme activities. Soil dehydrogenase and urease activities increased with soil MBC (microbial biomass carbon) concentrations. P-Glucosidase and acid phosphatase activities were significantly related to DOC (dissolved organic carbon) concentrations suggesting that these two enzymes drive the release of labile components from the SOM. This study helps better understanding relations between soil enzyme and soil labile carbon fractions, and further facilitates the understanding of the stability of soil carbon pool in permafrost wetland of Northeast China.
机译:土壤酶活性是气候变化带来的土壤有机质(SOM)动态的敏感指标。评价了东北地区不同类型冰冻地区湿地土壤酶活性的分布。结果表明,P-葡萄糖苷酶,转化酶,脱氢酶,脲酶和酸性磷酸酶的特定酶活性在季节性冻土中显示出最高的值,表明SOM的周转速度更快。不连续多年冻土中转化酶和酸性磷酸酶的比活高于连续多年冻土。温度,SOM和植被种类调节土壤酶的活性。土壤脱氢酶和脲酶活性随土壤MBC(微生物生物量碳)浓度的增加而增加。 P-葡萄糖苷酶和酸性磷酸酶活性与DOC(溶解的有机碳)浓度显着相关,表明这两种酶驱动SOM中不稳定组分的释放。这项研究有助于更好地了解土壤酶与土壤不稳定碳组分之间的关​​系,并进一步有助于了解中国东北多年冻土湿地中土壤碳库的稳定性。

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