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Regulation of extracellular protease activity in soil in response to different sources and concentrations of nitrogen and carbon

机译:响应不同来源和氮,碳浓度,调节土壤中细胞外蛋白酶的活性

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A large proportion of the nitrogen (N) in soil is in the form of proteinaceous material. Its breakdown requires the activity of extracellular proteases and other decomposing enzymes. The goal of our study was to better understand how carbon (C) and N availability affect soil protease activity. Several aerobic incubations were carried out with ammonium (NH sub(4) super(+)) and proteins as N sources and cellulose as the main C source. A strong increase in protease activity was observed when proteins were added, the increase depending on the amount of protein added and its solubility. Protease synthesis was clearly substrate induced, as NH sub(4) super(+) had no effect. During this substrate induced phase, the addition of glucose but not NH sub(4) super(+) resulted in protease repression, indicating that the level of protease synthesis was determined by the need for C rather than N. After 1 month of incubation, protease activity remained relatively constant over time and was closely related to microbial biomass N. Different concentrations of mineral N in soil solution had no direct effect on protease activity. However, during this stationary phase, protease activity could be repressed by glucose and NH sub(4) super(+) in a treatment with low mineral N content while in treatments with a higher N availability no repression was observed. We hypothesize that the need for N determined protease activity in the treatment with limited N availability. The addition of NH sub(4) super(+) allowed for reallocation of C and N away from protease synthesis, leading to the observed decrease in protease activity. The repression by glucose may be attributed to shifts in the pathway of microbial NH sub(4) super(+) assimilation. The results emphasize the close links between the microbially mediated cycles of organic C and N.
机译:土壤中很大一部分的氮(N)以蛋白质形式存在。其分解需要细胞外蛋白酶和其他分解酶的活性。我们研究的目的是更好地了解碳(C)和氮的有效性如何影响土壤蛋白酶的活性。以铵盐(NH sub(4)super(+))和蛋白质为氮源,以纤维素为主要C源进行了好氧培养。当添加蛋白质时,观察到蛋白酶活性的强烈增加,该增加取决于蛋白质添加量及其溶解度。蛋白酶合成显然是受底物诱导的,因为NH sub(4)super(+)没有作用。在此底物诱导阶段,葡萄糖的添加而不是NH sub(4)super(+)的添加导致蛋白酶的抑制,表明蛋白酶的合成水平是由对C而不是N的需求决定的。孵育1个月后,蛋白酶活性随时间保持相对恒定,并与微生物生物量氮密切相关。土壤溶液中不同浓度的矿物质氮对蛋白酶活性没有直接影响。但是,在此固定相期间,在矿物质氮含量低的处理中,葡萄糖和NH sub(4)super(+)可能抑制蛋白酶的活性,而在氮利用率较高的处理中,未观察到抑制作用。我们假设在有限的氮利用率下,对氮的需求决定了蛋白酶的活性。 NH sub(4)super(+)的添加允许C和N的重新分配远离蛋白酶合成,导致观察到的蛋白酶活性降低。葡萄糖的抑制作用可能归因于微生物NH sub(4)super(+)同化途径的转变。结果强调了微生物介导的有机碳和氮循环之间的紧密联系。

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