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陆地生物圈模型中的根系结构和功能动态——评估与建议。

Root structural and functional dynamics in terrestrial biosphere models--evaluation and recommendations.

机构信息

Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory, PO Box 2008, Oak Ridge, TN, 37831-6301, USA.

出版信息

New Phytol. 2015 Jan;205(1):59-78. doi: 10.1111/nph.13034. Epub 2014 Sep 26.

Abstract

There is wide breadth of root function within ecosystems that should be considered when modeling the terrestrial biosphere. Root structure and function are closely associated with control of plant water and nutrient uptake from the soil, plant carbon (C) assimilation, partitioning and release to the soils, and control of biogeochemical cycles through interactions within the rhizosphere. Root function is extremely dynamic and dependent on internal plant signals, root traits and morphology, and the physical, chemical and biotic soil environment. While plant roots have significant structural and functional plasticity to changing environmental conditions, their dynamics are noticeably absent from the land component of process-based Earth system models used to simulate global biogeochemical cycling. Their dynamic representation in large-scale models should improve model veracity. Here, we describe current root inclusion in models across scales, ranging from mechanistic processes of single roots to parameterized root processes operating at the landscape scale. With this foundation we discuss how existing and future root functional knowledge, new data compilation efforts, and novel modeling platforms can be leveraged to enhance root functionality in large-scale terrestrial biosphere models by improving parameterization within models, and introducing new components such as dynamic root distribution and root functional traits linked to resource extraction.

摘要

在对陆地生物圈进行建模时,应该考虑到生态系统中根系功能的广泛多样性。根系结构和功能与植物从土壤中吸收水分和养分、植物碳(C)同化、分配和向土壤释放以及通过根际相互作用控制生物地球化学循环密切相关。根系功能极其动态,取决于内部植物信号、根系特性和形态以及物理、化学和生物土壤环境。虽然植物根系对环境变化具有显著的结构和功能可塑性,但它们的动态在用于模拟全球生物地球化学循环的基于过程的地球系统模型的陆地组成部分中明显缺失。在大规模模型中对其动态的表示应提高模型的准确性。在这里,我们描述了当前跨尺度模型中根系的包含情况,从单个根系的机械过程到在景观尺度上运行的参数化根系过程。在此基础上,我们讨论了如何利用现有的和未来的根系功能知识、新的数据编纂工作以及新的建模平台,通过改进模型内的参数化以及引入与资源提取相关的动态根系分布和根系功能特性等新组件,来增强大规模陆地生物圈模型中的根系功能。

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