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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Interactive effects of nitrogen forms and temperature on soil organic carbon decomposition in the coastal wetland of the Yellow River Delta, China
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Interactive effects of nitrogen forms and temperature on soil organic carbon decomposition in the coastal wetland of the Yellow River Delta, China

机译:氮形态与温度对中国黄河三角洲沿海湿地土壤有机碳分解的互动效应

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Nitrogen (N) is a limiting nutrient in many terrestrial ecosystems. Many studies concentrated on the relation. ships between the amount of N deposition and soil organic carbon (SOC) dynamics. However, few studies are dedicated to differentiate the influence of inorganic and organic N deposition on SOC decomposition. In addition, the interactive effect of different forms of N and temperature on SOC decomposition is still unknown. A short-term incubation experiment was conducted to determine the interactive of N addition (nitrate, ammonium and organic N) and temperature on SOC decomposition in the coastal wetland of the Yellow River Delta, China. The results showed that increased temperature had a positive effect on SOC decomposition (P & 0.05). Both ammonium and organic N additions accelerated SOC decomposition at the initial phase of incubation (P & 0.05), while organic N produced larger and positive effects on SOC decomposition than ammonium at high level of N addition in the initial stage of incubation (P & 0.05). Furthermore, the interactive effect of N additions (i.e. two level of nitrate and organic N additions and a high level of ammonium addition) and temperature on SOC decomposition was mainly an additive effect due to the neutral effect of such N additions on the Q(10) value of SOC decomposition. However, a low level of ammonium addition and temperature produced an antagonistic effect on SOC decomposition. This may be attributed to the decreased Q(10) value of SOC decomposition at a low level of ammonium addition (P & 0.05). This indicates that short-term SOC decomposition under simultaneous influence of temperature and a low level of ammonium addition may be overestimated based on their single effects. Our results also highlight the importance of differentiating the effects of organic and inorganic N additions on SOC decomposition.
机译:氮气(n)是许多陆地生态系统中的限制营养素。许多研究集中在关系中。 n沉积和土壤有机碳(SoC)动态的船舶之间的船舶。然而,很少有研究旨在区分无机和有机N沉积对SoC分解的影响。此外,不同形式的N和SoC分解的温度的交互式效果仍然未知。进行了短期培养实验,以确定黄河三角洲沿海湿地的N添加(硝酸铵,铵和有机N)和温度对SoC分解的互动。结果表明,升高的温度对SOC分解具有阳性作用(P& 0.05)。铵和有机N在孵育(P& 0.05)的初始阶段添加加速SOC分解,而有机氮在孵育初始阶段的高水平N添加时对SoC分解产生的较大和积极影响( P& 0.05)。此外,N添加的交互式效果(即两级硝酸盐和有机N添加和高水平的铵添加)和对SoC分解的温度主要是由于Q上的N个添加的中性效果导致的添加效果(10 )SoC分解的价值。然而,低水平的铵加成和温度产生对SOC分解的拮抗作用。这可能归因于SoC分解的降低的Q(10)值在低水平的铵添加(P& 0.05)。这表明可以基于它们的单一效果高估了在同时对温度和低水平的铵添加的影响下的短期SOC分解。我们的结果还突出了区分有机和无机N添加对SOC分解的影响的重要性。

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