Bassani Francesca, Fatichi Simone, Rinaldo Andrea, Bonetti Sara
Laboratory of Catchment Hydrology and Geomorphology, School of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne (EPFL), Sion 1951, Switzerland.
Department of Civil and Environmental Engineering, National University of Singapore, Singapore 117576, Singapore.
Proc Natl Acad Sci U S A. 2024 Oct 15;121(42):e2410736121. doi: 10.1073/pnas.2410736121. Epub 2024 Oct 9.
Allometric scaling relations are widely used to link biological processes to body size in nature. Several studies have shown that such scaling laws hold also for natural ecosystems, including individual trees and forests, riverine metabolism, and river network organization. However, the derivation of scaling laws for catchment-scale water and carbon fluxes has not been achieved so far. Here, we focus on scaling relations of catchment green metabolism, defined as the set of ecohydrological and biogeochemical processes through which vegetation assemblages in catchments maintain their structure and react to the surrounding environment. By revising existing plant size-density relationships and integrating them across large-scale domains, we show that the ecohydrological fluxes occurring at the catchment scale are invariant with respect to the above-ground vegetation biomass per unit area of the basin, while they scale linearly with catchment size. We thus demonstrate that the sublinear scaling of plant metabolism results in an isometric scaling at catchment and regional scales. Deviations from such predictions are further shown to collapse onto a common distribution, thus incorporating natural fluctuations due to resource limitations into a generalized scaling theory. Results from scaling arguments are supported by hyperresolution ecohydrological simulations and remote sensing observations.
异速生长比例关系在自然界中被广泛用于将生物过程与体型联系起来。多项研究表明,此类比例定律也适用于自然生态系统,包括单棵树木和森林、河流新陈代谢以及河网组织。然而,目前尚未得出流域尺度的水通量和碳通量的比例定律。在此,我们关注流域绿色新陈代谢的比例关系,其定义为流域内植被组合维持其结构并对周围环境做出反应的一系列生态水文和生物地球化学过程。通过修正现有的植物大小 - 密度关系并将其整合到大规模区域,我们表明,流域尺度上发生的生态水文通量相对于流域单位面积的地上植被生物量是不变的,而它们与流域面积呈线性比例关系。因此,我们证明了植物新陈代谢的亚线性比例关系导致了流域和区域尺度上的等比缩放。进一步表明,与这些预测的偏差会汇聚到一个共同的分布上,从而将由于资源限制引起的自然波动纳入广义比例理论。比例论证的结果得到了高分辨率生态水文模拟和遥感观测的支持。