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Effects of precipitation change on fine root morphology and dynamics at a global scale: a meta-analysis

机译:降水变化对全球范围内细根形态和动态的影响:META分析

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摘要

We compiled data from 495 observations and 103 papers and carried out a meta-analysis of the responses of fine root biomass, production, decomposition, and morphology to precipitation increases and decreases. In addition, we evaluated the effects of plant life form, soil depth, and experiment duration on the responses of fine roots to precipitation changes. Our results confirmed that decreased precipitation limited fine root diameter and accelerated turnover. Increased precipitation stimulated fine root elongation and enhanced the fine root accumulation. The responses of fine roots to precipitation changes varied among plants of different life forms. Tree fine root production and decomposition and non-tree fine root diameter varied most strongly under decreased precipitation. Specific root length of non-tree fine roots was much higher than that of tree fine roots under increased precipitation. Decreased precipitation limited the growth of fine roots in 20-40 cm deep soil, whereas increased precipitation promoted the growth of fine roots in both shallow and deep soil layers. The responses of fine roots to decreased precipitation were affected by experiment duration. Results filled the gap of evaluation data on the effect of precipitation change on fine root morphology and dynamics, which are useful for better predicting the C cycle under precipitation change.
机译:我们从495个观察和103篇论文编制数据,并对细根生物量,生产,分解和形态的响应进行了荟萃分析,以降水增加和降低。此外,我们还评估了植物寿命形式,土壤深度和实验持续时间对沉淀变化的响应的影响。我们的结果证实,降水量有限细根直径和加速趋势。提高降水刺激细根伸长率,增强细根积累。细根对沉淀变化的反应在不同生活形式的植物中变化。树细根生产和分解和非树细根直径在降水下降下最强烈变化。非树细根的特异性根长得多高于降水下树细根的细根。降低降低限制了20-40厘米的深层土壤中细根的生长,而降水量促进浅层和深层土壤层中细根的生长。通过实验持续时间影响细根对降水降低的反应。结果填补了评价数据对沉淀变化对细根形态和动力学影响的影响,这对于更好地预测降水变化的C循环是有用的。

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