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Chemical composition and diversity influence non-additive effects of litter mixtures on soil carbon and nitrogen cycling: Implications for plant species loss

机译:化学成分和多样性影响凋落物混合物对土壤碳和氮循环的非累加效应:对植物物种流失的影响

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Diverse plant litter mixtures frequently decompose differently than expected compared to the average of the component species decomposing alone, and it remains unclear why decomposition may respond non-additively to diversity. Here, we hypothesized that litter chemical composition and chemical diversity would be important determinants of the strength and direction (synergistic versus antagonistic) of non-additive soil carbon (C) and nitrogen (N) cycling responses to litter mixtures. To test this, we performed a soil incubation experiment using litter mixtures comprised of up to four plant species, and we measured three components of decomposition: respiration, net N mineralization, and microbial biomass N accumulation. We used nine chemical traits to calculate the chemical composition and diversity of the litter mixtures. First, we found that respiration responded as the average of the individual species in the mixture (i.e. additively), rather than non-additively as initially predicted. Second, litter mixtures stimulated significantly more net N immobilization than expected in 64% of cases, and non-additive responses were highly dependent on mixture chemical composition, and were influenced to a lesser degree by chemical diversity. Specifically, concentrations of tannins and certain low molecular weight phenolics in the mixtures were positively correlated with greater N immobilization than expected. Non-additive N mineralization responses were poorly correlated with traditional measures of litter chemistry like N concentration, C:N, lignin:N, and phenolic:N. Our results also show that non-additive N mineralization responses were affected by loss of some species significantly more than others, and the effects of species loss could depend on 1) whether a species contains compounds with strong effects on non-additive responses; and 2) whether those compounds are also found in other species. Finally, litter mixtures stimulated more microbial biomass N than expected in 45% of cases, but non-additive responses were only weakly dependent on the litter chemistry variables that we measured.
机译:与单独分解的组分物种的平均值相比,不同的植物凋落物混合物分解的频率通常比预期的要高,并且尚不清楚为什么分解可能对多样性产生非累加的响应。在这里,我们假设凋落物的化学成分和化学多样性将是决定非添加性土壤碳(C)和氮(N)对凋落物混合物循环响应的强度和方向(协同作用与拮抗作用)的重要决定因素。为了测试这一点,我们使用最多由四种植物组成的凋落物混合物进行了土壤培养实验,并测量了分解的三个成分:呼吸,净氮矿化和微生物生物量氮的积累。我们使用了9个化学特性来计算垃圾混合物的化学组成和多样性。首先,我们发现呼吸反应是混合物中单个物种的平均值(即加和),而不是最初预测的非加和。其次,在64%的情况下,混合杂物刺激的净氮固定量明显多于预期,并且非加性反应高度依赖于混合化学成分,并且受化学多样性的影响较小。具体而言,混合物中单宁酸和某些低分子量酚类化合物的浓度与固氮能力比预期的高呈正相关。非累加的氮矿化反应与传统的垫料化学指标(如氮浓度,C:N,木质素:N和酚醛:N)的相关性很低。我们的研究结果还表明,某些物种的损失对非加成氮矿化反应的影响远大于其他物种,物种丧失的影响可能取决于1)一个物种是否包含对非加成反应具有强烈影响的化合物; 2)这些化合物是否也存在于其他物种中。最后,在45%的情况下,垃圾混合物刺激的微生物生物量氮比预期的多,但非加性反应仅弱依赖于我们测得的垃圾化学变量。

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