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Effects of elevated CO2, increased nitrogen deposition, and plant diversity on aboveground litter and root decomposition

机译: CO 2 升高,氮沉降增加和植物多样性对地上凋落物和根系分解的影响

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Global change‐induced litter decomposition strongly affects the carbon (C) and nitrogen (N) dynamics in grassland ecosystems. However, few studies show the interactive effects of global change factors on litter and root decomposition. We conducted a four‐year grassland field experiment to examine the quality and decomposition of litter and root in a three‐factorial experiment with elevated CO _(2), increased N deposition, and plant species richness. We found that elevated CO _(2) decreased the litter N content and root lignin content. N addition increased the root N content and decreased the litter lignin content. Increasing plant richness decreased the N and lignin contents in litter and root. In contrast to the quality changes, elevated CO _(2) had no effect on decomposition of litter and root. N addition increased the C loss of the litter by 4.8%, but did not affect C and N loss in root. Increasing plant richness affected the C and N loss in litter and root. ANCOVA s showed that tissue quality and root biomass affected the C and N loss in litter and root, and soil C and N affected the N loss of litter and root. However, changes in tissue quality, biomass, and soil as covariates did not significantly change the effects of CO _(2), N, and plant richness on decomposition. The structural equation?model showed that elevated CO _(2) indirectly decreased litter N loss and increased root N loss, while N addition indirectly increased the C and N loss in litter and root, via their effects on tissue quality. Increasing plant richness increased litter C and N loss, but indirectly decreased root C and N loss. N deposition can accelerate litter and root decomposition, thus modifying the limitation of elevated CO _(2) on soil N availability. Biodiversity loss greatly alters litter and root decomposition, potentially driving any changes in C and N cycling. Our study clearly demonstrates a relative certainty of a predicted increase in the C loss and N release in litter and root decomposition with increased N deposition, whereas the effects of elevated CO _(2) and plant diversity changes on decomposition strongly differ between litter and root in grassland ecosystems.
机译:全球变化引起的凋落物分解强烈影响草地生态系统中的碳(C)和氮(N)动态。但是,很少有研究表明全局变化因子对凋落物和根分解的交互作用。我们进行了一项为期四年的草地田间试验,以三因素试验(CO _(2)升高,氮沉降增加和植物物种丰富度)检查凋落物和根的质量和分解。我们发现升高的CO _(2)减少了凋落物N含量和根木质素含量。氮的添加增加了根系氮的含量,降低了凋落物中木质素的含量。增加植物丰富度会降低凋落物和根中的氮和木质素含量。与质量变化相反,CO _(2)升高对凋落物和根的分解没有影响。氮的添加使凋落物的碳损失增加了4.8%,但不影响根系的碳和氮损失。植物丰富度的增加影响了凋落物和根中碳氮的流失。 ANCOVA s表明,组织质量和根系生物量影响凋落物和根系的碳和氮损失,土壤碳和氮影响凋落物和根系的氮损失。但是,组织质量,生物量和土壤作为协变量的变化并没有显着改变CO_(2),N和植物丰富度对分解的影响。结构方程模型表明,升高的CO _(2)通过降低凋落物和根系对组织质量的影响,间接降低了凋落物N的损失并增加了根系N的损失,而添加氮间接增加了凋落物和根系中的C和N损失。增加植物丰富度会增加凋落物C和N的损失,但间接减少根系C和N的损失。氮的沉积可以加速凋落物和根系的分解,从而改变升高的CO _(2)对土壤氮有效性的限制。生物多样性的丧失极大地改变了凋落物和根的分解,可能导致碳和氮循环的任何变化。我们的研究清楚地表明,凋落物和根系分解过程中碳流失和氮素释放随氮沉降增加而预测增加的相对确定性,而升高的CO _(2)和植物多样性变化对分解的影响在凋落物和根系之间差异很大。在草地生态系统中

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