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河岸农林业中植物功能性状和多样性在土壤碳动态中的作用。

The role of plant functional traits and diversity in soil carbon dynamics within riparian agroforests.

机构信息

Dep. of Physical and Environmental Sciences, Univ. of Toronto Scarborough, Toronto, ON, Canada.

School of Environmental Sciences, Univ. of Guelph, Guelph, ON, Canada.

出版信息

J Environ Qual. 2022 Jan;51(1):33-43. doi: 10.1002/jeq2.20303. Epub 2021 Dec 1.

Abstract

Restoration of agricultural riparian buffers with trees (agroforestry) provides an elegant solution to enhance carbon storage while also augmenting local biodiversity. Yet the scope and role of riparian plant community diversity in key soil dynamics remain unresolved. Operationalizing riparian age (young [<10 yr] and mature [>30 yr] since establishment] and forest stand type (coniferous and deciduous dominant) to capture the potential extent of plant diversity, we measured plant functional trait diversity and community weighted mean trait values, microbial composition, abiotic soil conditions, and rates of soil CO efflux (mg CO -C m h ). We used piecewise structural equation modeling (SEM) to further refine the role of biotic indices (leaf, root, and microbial characteristics), and abiotic factors (soil physio-chemical metrics) on soil C cycling processes in riparian systems. We found significantly lower rates of CO efflux (F = 8.47; p < .01) over one growing season and higher total soil C (F = 3.46; p = .03) in mature buffers compared with young buffers. Using SEM, we describe influences on soil C content (marginal r = 61) and soil CO efflux (marginal r = 53). Within young buffers, soil C content was significantly predicted by fungal/bacterial ratio and root length density, whereas in mature buffers, tree leaf characteristics were associated with soil C content. Soil CO efflux was predicted by soil moisture, soil carbon content, and herbaceous root characteristics. Evidently, leaf and root functional traits in combination with broad soil parameters significantly describe soil C dynamics in the field; however, significant pathways are not the same throughout the life cycle of a riparian agroforest.

摘要

利用树木(农林复合)恢复农业河岸缓冲带为增强碳储存和提高当地生物多样性提供了一种巧妙的解决方案。然而,河岸植物群落多样性在关键土壤动态中的范围和作用仍未得到解决。我们通过操作河岸年龄(<10 年的幼龄[young]和>30 年的成熟[mature])和林分类型(针叶树和落叶树为主)来捕获潜在的植物多样性范围,测量了植物功能性状多样性和群落加权平均性状值、微生物组成、非生物土壤条件和土壤 CO 排放速率(mg CO -C m h )。我们使用分段结构方程模型(SEM)来进一步细化生物指标(叶片、根系和微生物特征)和非生物因素(土壤理化指标)对河岸系统土壤碳循环过程的作用。我们发现,在一个生长季节内,成熟缓冲带的 CO 排放速率(F=8.47;p<.01)明显较低,总土壤 C 含量(F=3.46;p=.03)较高。通过 SEM,我们描述了对土壤 C 含量(边缘 r=61)和土壤 CO 排放(边缘 r=53)的影响。在幼龄缓冲带中,土壤 C 含量主要受真菌/细菌比和根长密度的影响,而在成熟缓冲带中,树的叶片特征与土壤 C 含量有关。土壤 CO 排放受土壤水分、土壤碳含量和草本根系特征的影响。显然,叶片和根系功能性状与广泛的土壤参数相结合可以很好地描述田间土壤 C 动态;然而,在河岸农林的整个生命周期中,重要途径并不相同。

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