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首页> 外文期刊>The Open Ecology Journal >The Role of Litter Quality Feedbacks in Terrestrial Nitrogen andPhosphorus Cycling
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The Role of Litter Quality Feedbacks in Terrestrial Nitrogen andPhosphorus Cycling

机译:凋落物质量反馈在陆地氮和磷循环中的作用

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Many studies in ecosystem ecology argue for strong control of litter quality over nitrogen (N) cycling. Wedeveloped a model for temperate grasslands to test the importance of litter quality in decomposition for N and phosphorus(P) cycling based on the following premises. First, terrestrial N and P cycling differ fundamentally because N is astructural component of the soil organic matter (SOM), whereas P is not. Secondly, SOM has a much lower C:N ratio thanlitter inputs. Thirdly, litter decomposition follows an exponential decay with 20% of the original litter mass turning intoSOM. Fourth, litter N concentration shows an exponential increase during decomposition, whereas P does not change andis released proportionally to the litter mass. Based on these premises we constructed a model which shows that 0.75% N isa critical initial litter concentration at which concentration all N is immobilized and no N is released from the litter. Thusat 0.75% N of the litter all net N mineralization is through SOM decomposition and not through litter decomposition.Phosphorus, in contrast, is primarily released in the early stages of litter decomposition. Empirical tests of these modelpredictions support the applicability of the model to temperate grassland ecosystems. This model predicts that Nmineralization from SOM is much more important than mineralization from litter and that plant litter quality differencesalone cannot explain ecosystem N cycling patterns. Phosphorus, in contrast, does cycle largely through litterdecomposition, and plant litter quality differences are the dominant factor in determining ecosystem P cycling feedbacks.
机译:生态系统生态学上的许多研究都主张对氮(N)循环更好地控制垃圾质量。我们基于以下前提开发了温带草原的模型,以测试凋落质量对氮和磷(P)循环分解的重要性。首先,由于氮是土壤有机质(SOM)的结构组成部分,而陆地磷和磷循环则根本不同,因此陆地氮和磷的循环存在根本差异。其次,SOM的C:N比要比小输入低得多。第三,凋落物分解遵循指数衰减,原始凋落物质量的20%转化为SOM。第四,凋落物N的浓度在分解过程中呈指数增长,而P不变,并与凋落物质量成比例地释放。基于这些前提,我们构建了一个模型,该模型表明0.75%的N是临界的初始垫料浓度,在该浓度下,所有N均被固定,垫料中没有N释放出来。因此,在凋落物氮的0.75%处,所有净氮矿化是通过SOM分解而不是通过凋落物分解。相反,磷主要在凋落物分解的早期释放。这些模型预测的实证检验支持了该模型对草地生态系统的适应性。该模型预测,SOM的矿化作用比凋落物的矿化作用更为重要,而且植物凋落物的质量差异无法解释生态系统的N循环模式。相反,磷的确通过凋落物分解而大量循环,而植物凋落物质量的差异是决定生态系统磷循环反馈的主要因素。

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