首页> 外文会议>The 5th China-Japan-Korea Grassland Conference: Knowledge Innovation of Grassland Science and Sustainalbe Development of Grassland Agriculture >Effects of nitrogen addition and increased precipitation on soil hydrolytic enzyme activities in a temperate meadow steppe
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Effects of nitrogen addition and increased precipitation on soil hydrolytic enzyme activities in a temperate meadow steppe

机译:氮素增加和降水增加对温带草原草原土壤水解酶活性的影响

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Soil extracellular enzymes are the proximal drivers of organic matter decomposition via mineralizing organic matter and releasing carbon and nutrients in forms that can be assimilated.This process can be greatly affected by the change of temperature, precipitation, and other environmental factors.However, few experiments have been conducted to study the responses of hydrolase activities to the interaction of nitrogen (N) deposition and precipitation.The main purpose of this study was to investigate the change of soil hydrolytic enzyme activities in a Stipa baicalensis meadow steppe with a complete randomized block factorial experimental design with the N addition, the increased precipitation and a combination of N and precipitation increase in northeastern China.These hydrolases included carbon-acquisition enzymes (α-glucosidase, αG;β-glucosidase, βG;β-xylosidase, βX;Cellobiohydrolase, CBH), nitrogen-acquisition enzymes (N-acetylglucosaminidase, NAG;Leucine aminopeptidase, LAP), and phosphorus-acquisition enzymes (acid phosphatases, aP).The results showed that N addition just significantly increased the activity of NAG and increased precipitation had no significant effect on all hydrolase activities, N addition and increased precipitation had significantly interactive effects on the activity of βX and CBH.However, single N addition resulted in an increase in the activity of NAG, βG, βX and CBH, as well as the content of soil organic carbon (SOC), soil total N (TN), soil available N (AN) and soil moisture (SM).But, all the significant effects disappeared when precipitation synchronously increased.On the other side, single increased precipitation led to the obvious increase of SOC, TN and AN, and the change of precipitation had no significant effects on hydrolytic enzyme activities in all plots.Correlation analysis demonstrated that soil properties enormously influenced NAG but had relatively weak effects on the activity of other enzymes.Redundancy analysis indicated that the patterns of hydrolase activities were mainly driven by soil pH, SOC and TN.Overall, our results suggested that the variation of carbon-acquisition and nitrogen-acquisition hydrolase activities caused by N addition was offset by the effects of increased precipitation.Furthermore, the differential responses of hydrolases to N addition and increased precipitation may have important implications for carbon and nutrient cycling under the conditions of global change in the future.
机译:土壤细胞外酶是有机物通过矿化有机物并以可被吸收的形式释放碳和养分而分解的近端驱动力,这一过程受温度,降水和其他环境因素的变化影响很大,但是很少有实验进行了研究水解酶活性对氮(N)沉积和降水相互作用的响应。本研究的主要目的是利用完全随机分组因子分析黄针草原草甸草原土壤水解酶活性的变化。在东北地区添加氮,增加降水,增加氮和降水的组合的实验设计。这些水解酶包括碳捕获酶(α-葡萄糖苷酶,αG;β-葡萄糖苷酶,βG;β-木糖苷酶,βX;纤维素酶, CBH),氮捕获酶(N-乙酰氨基葡萄糖苷酶,NAG;亮氨酸氨基肽酶,LAP)和ph结果表明,氮的添加仅显着增加了NAG的活性,沉淀的增加对所有水解酶的活性均无显着影响,氮的添加和增加的沉淀对βX的活性具有显着的交互作用。然而,单次添加氮会增加NAG,βG,βX和CBH的活性,以及​​土壤有机碳(SOC),土壤总氮(TN),土壤有效氮(AN)的含量但是,当降水量同步增加时,所有显着的影响都消失了;另一方面,单次增加的降水导致了SOC,TN和AN的明显增加,并且降水的变化对水解没有显着影响。相关性分析表明,土壤性质对NAG的影响很大,但对其他酶的活性影响相对较弱。总的来说,我们的研究结果表明,氮的添加引起的碳吸收和氮吸收水解酶活性的变化被降水增加的影响所抵消。在未来全球变化的条件下,水解酶对氮添加和降水增加的不同响应可能对碳和养分循环产生重要影响。

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