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首页> 外文期刊>Soil Biology & Biochemistry >Labile carbon matters more than temperature for enzyme activity in paddy soil
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Labile carbon matters more than temperature for enzyme activity in paddy soil

机译:不稳定的碳在水稻土中的酶活性大于温度

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Global warming increases belowground carbon (C) input as plant litterfall, root biomass and rhizodeposition, which influences the stocks and dynamics of soil organic matter. To clarify the effects of labile C availability (biochemical factor) and temperature (environmental factor) on enzyme activities, we incubated typical paddy soil for 75 d at four temperatures (5, 15, 25, and 35 degrees C) under anaerobic conditions. Acetate was used as the source of labile C and methane. The potential activities of three hydrolases (beta-glucosidase, chitinase, and xylanase) were analysed on days 3, 15, and 75 after acetate addition. Activity of beta-glucosidase and chitinase in soil without acetate addition was 2.1-2.7 times higher than that with acetate. Xylanase activity increased with temperature and incubation period. The enzymes involved in the C cycle were sensitive to temperature, whereas chitinase (responsible for N cycle) activity became temperature sensitive only after acetate addition (Q(10)-V-max >= 1). Organic C mineralisation (CO2 release) was more sensitive at low temperature with Q(10) values 1.1-3.4 times higher at 5-15 degrees C than at 25- 35 degrees C. The Q(10) values for methane (CH4) emission were 2.8-13.5 times higher at 5-15 degrees C than at 25-35 degrees C. Organic matter decomposition in paddy soil was more sensitive to temperature (Q(10) of CO2 and CH4 emission >= 1) than enzyme activities. Comparison of abiotic (temperature) and biochemical (C availability) effects indicated that warming has limited effects on hydrolase activities in paddy soil. The increase in labile C remarkably stimulated microbial activity and soil organic matter turnover. We conclude that: i) enzyme activities are more sensitive to C addition than to temperature; ii) and SOM decomposition is accelerated by both C input and warming, especially at low temperatures.
机译:全球变暖的地下碳(c)输入作为植物凋落物,根生物量和无溶解沉积,影响土壤有机物的股票和动态。为了阐明不稳定的C可用性(生化因子)和温度(环境因素)对酶活性的影响,我们在厌氧条件下在四个温度(5,15,25和35℃)下孵育75d的典型水稻土。乙酸盐用作不稳定C和甲烷的来源。在乙酸盐添加后,分析了三天3,15和75天水解酶(β-葡糖苷酶,丁酶和木聚糖酶)的潜在活性。 β-葡萄糖苷酶的活性与醋酸盐的土壤中的葡萄糖苷酶和几丁质酶的活性比乙酸盐高2.1-2.7倍。木聚糖酶活性随温度和培养期增加。 C循环中涉及的酶对温度敏感,而几丁酶(负责N循环)活性仅在乙酸盐添加后变得温度敏感(Q(10)-V-MAX> = 1)。有机C矿化(CO2释放)在低温下更敏感,Q(10)值比在5-15℃下较高1.1-3.4倍,比在25-35℃下。甲烷(CH4)排放的Q(10)值在5-15℃下比在25-35℃下较高,水稻土中的有机物质分解比酶活性更敏感(CO 2和CH4发射> = 1)更敏感。非生物(温度)和生物化学(C可用性)效果的比较表明,温暖对水稻土壤中的水解酶活性有限。不稳定的C刺激性的微生物活性和土壤有机质转换增加。我们得出结论:i)酶活性比温度更敏感。 II)和SOM分解通过C输入和变暖,特别是在低温下加速。

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