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Distribution pattern of amidohydrolase activities among soil aggregates: Effect of soil aggregates isolation methods

机译:土壤聚集体中酰胺水解酶活性的分布模式:土壤聚集体分离方法的影响

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The effect of aggregate isolation methods on distribution patterns of N-cycling enzymes within soil aggregate is not well understood. In this study, the effects of wet and dry sieving methods on organic C (OC) content and amidohydrolase activities (Urease, L-glutaminase and L-asparaginase) were determined for six aggregate sizes (4-2, 2-1, 1-0.5, 0.5-0.25, 0.25-0.05 and & 0.05 mm) isolated from five grassland soils. The distribution of wet-sieved aggregates was skewed toward microaggregates (0.25-0.05 mm) and silt and clay fractions (& 0.05 mm), while the contrary was found with dry sieving. Wet-sieved macroaggregates (& 0.25 mm) had higher OC content and potential amidohydrolase activities than other aggregate sizes but not a specific size of macroaggregates was consistently higher in all soils studied. No significant differences in OC and amidohydrolase activity were also observed between dry-sieved macroaggregates. Although dry-sieved 0.25-0.05 mm fraction had generally higher amidohydrolase activities than the other aggregate sizes, the distribution pattern of urease (URE) activity within dry-sieved aggregates was different among soils studied. Unlike the dry sieving method, microaggregates and silt and clay fractions separated by wet sieving had a major contribution to the total OC content and amidohydrolase activities in all soils. Both sieving methods altered the amidohydrolase activities, causing either losses or even increases depending on the soil and the enzyme studied. The significant difference between grassland soils in terms of OC content and enzyme activity was observed in wet-and dry-sieved aggregates, although it was more pronounced in wet-sieved large macroaggregates. Overall, sieving methods resulted in different OC content and amidohydrolase activities in soil aggregates, however, wet sieving showed greater ability to reveal significant differences in terms of aggregate potential enzyme activity compared to dry sieving. Wet sieving was also most capable to examine long-term changes in organic matter and enzyme activity between soil types.
机译:聚集体分离方法对土壤聚集体内N-循环酶分布模式的影响还不太了解。在该研究中,测定六骨料尺寸(4-2,2-1,1- 0.5,0.5-0.25,0.25-0.05和& 0.05 mm)从五个草地土壤中分离。将湿筛分的聚集体的分布朝向微烧结(0.25-0.05mm)和淤泥和粘土馏分(& 0.05 mm)偏置,而相反的是用干筛分发现。湿式筛分的大草凝结(& 0.25mm)具有更高的OC含量和潜在的氨基水解酶活性,而不是其他骨料尺寸,但在所研究的所有土壤中始终如一的大小大小的大小。在干筛分的大草原之间也没有观察到OC和酰胺水解酶活性的显着差异。虽然干燥筛分的0.25-0.05mm级分具有比其他聚集体尺寸更高的酰胺水解酶活性,但是在研究的土壤中,干筛分聚集体内的脲酶(Ure)活性的分布模式不同。与干筛分方法不同,通过湿筛分分离的微烧结和淤泥和粘土馏分对所有土壤中的OC含量和酰胺水解酶活性不同。筛分方法都改变了氨基水解酶活性,导致损失或甚至根据土壤和所研究的酶增加而增加。在湿和干燥的聚集体中观察到OC含量和酶活性方面的草地土壤的显着差异,尽管在湿筛分的大型大甲骨中更加明显。总的来说,筛分方法导致不同的OC含量和土壤聚集体中的酰胺水溶生酶活性,然而,与干筛分相比,湿筛分显示出更大的揭示聚集势酶活性的显着差异。湿筛分也最能够检查土壤类型之间有机质和酶活性的长期变化。

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