中国亚热带毛竹林常绿阔叶林土壤碳氮比的恒等比例变化

IF 3.9 2区 农林科学 Q1 AGRONOMY
Ming Ouyang, Anwar Eziz, Wenjing Fang, Qiong Cai, Suhui Ma, Shuli Xiao, Jiangling Zhu, Qingpei Yang, Jinming Hu, Zhiyao Tang, Jingyun Fang
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引用次数: 0

摘要

背景和目的元素化学计量对生物地球化学循环的运作至关重要。然而,目前还不清楚毛竹(Phyllostachys edulis)入侵常绿阔叶林对土壤C和N的化学计量有何影响。方法我们在中国主要竹类分布区的30个地点,采用成对取样法采集了三种森林类型(竹林、竹阔叶混交林和常绿阔叶林)的90个入侵断面的1098个土壤样本。结果 竹子入侵明显降低了 0-20 厘米土层的表土碳含量和碳氮比,但增加了 30-70 厘米土层的底土碳和氮含量。在所有入侵阶段,所有土层的土壤碳含量与氮含量近似等比例(比例指数≈1)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Constant isometric scaling of soil carbon to nitrogen in Moso bamboo-invaded evergreen broadleaf forests in subtropical China

Constant isometric scaling of soil carbon to nitrogen in Moso bamboo-invaded evergreen broadleaf forests in subtropical China

Background and aims

Elemental stoichiometry is crucial for the functioning of biogeochemical cycles. However, it is unclear how the invasion of Moso bamboo (Phyllostachys edulis) into evergreen broadleaf forests influences soil C and N stoichiometry. In the present study, we aimed to investigate how bamboo invasion affects soil C and N content, C:N ratio, and their scaling relationship at a large scale.

Methods

We collected 1,098 soil samples from 90 invasive transects using pairwise sampling across three forest types (bamboo, mixed bamboo and broadleaf, and evergreen broadleaf forests) at 30 sites in China's major bamboo distribution areas.

Results

Bamboo invasion significantly decreased the topsoil C content and C:N ratio in the 0–20-cm layer but increased the subsoil C and N content at the 30–70-cm depth. Soil C content scaled approximately isometrically (scaling exponent ≈ 1) with N content in all soil layers across all invasion stages.

Conclusion

These findings highlight the general patterns of bamboo invasion-induced changes in soil stoichiometry and provide new insights into the events in forest ecosystems caused by bamboo invasion.

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来源期刊
Plant and Soil
Plant and Soil 农林科学-农艺学
CiteScore
8.20
自引率
8.20%
发文量
543
审稿时长
2.5 months
期刊介绍: Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manuscripts with a strong mechanistic component which develop and test hypotheses aimed at understanding underlying mechanisms of plant-soil interactions. Manuscripts can include both fundamental and applied aspects of mineral nutrition, plant water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics, as long as they are hypothesis-driven and enhance our mechanistic understanding. Articles including a major molecular or modelling component also fall within the scope of the journal. All contributions appear in the English language, with consistent spelling, using either American or British English.
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