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High throughput method for measuring urease activity in soil

机译:测量土壤中脲酶活性的高通量方法

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Extracellular enzymes break down soil organic matter into smaller compounds and their measurement has proved to be a powerful tool to evaluate the functionality of soils. Urease is the enzyme that degrades urea and is widely considered to be a good proxy of nitrogen (N) mineralisation. But the methods available to measure this enzyme are time consuming; as such, urease is not commonly included in standard enzyme profiling of soils. We developed a fast, high throughput and reproducible colorimetric microplate technique to evaluate urease activity in soil. The method involves the incubation of soil slurries in 96-deepwell blocks with urea solutions and the measurement, by colorimetric reaction, of ammonium produced. We compared the new method with existing methods, yielding comparable results, and evaluated optimal conditions for urease analysis (soil slurry concentration, substrate concentration, incubation times and extractant salt concentration) in different grassland soils. The method proved to be a faster, higher throughput, and more precise alternative to existing methods for evaluating this important N-related enzyme.
机译:细胞外酶将土壤有机质分解成较小的化合物,其测量已被证明是评估土壤功能的强大工具。脲酶是降解尿素的酶,并且被广泛认为是氮气(n)矿化的良好代理。但可用于测量此酶的方法是耗时的;因此,脲酶通常不包含在土壤的标准酶谱中。我们开发了一种快速,高通量和可重复的比色微电子技术,可评估土壤中的脲酶活性。该方法涉及用尿素溶液孵育96- Deplwell块中的土壤浆料,并通过测量法,测量结果产生铵。我们将新方法与现有方法进行比较,产生可比的结果,并评估不同草地土壤中的释放释放量(土壤浆料浓度,底物浓度,孵化时间和萃取剂盐浓度和萃取剂盐浓度)的最佳条件。该方法被证明是一种更快,更高的产量,更精确的替代方法,用于评估该重要的N相关酶的现有方法。

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