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عنوان فارسی مقاله:

استوکیومتری منابع بواسطه از دست دادن C خاک و تحولات مواد مغذی در خاک جنگل


عنوان انگلیسی مقاله:

Resource stoichiometry mediates soil C loss and nutrient transformations in forest soils


سال انتشار : 2016



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مقدمه انگلیسی مقاله:

1. Introduction

The transfer of carbon (C)from tree roots to the surrounding soil (i.e., the rhizosphere) is increasingly being recognized as a critical driver of ecosystem processes (Hogberg et al., 2001; Cheng and Kuzyakov, 2005; Finzi et al., 2015), ecosystem sensitivity to global change (Phillips et al., 2011), and biospheric feedbacks to climate (Bardgett et al., 2008; Heimann and Reichstein, 2008). Plant roots release between 5 and 20% of total photosynthate C as root exudates, mostly as soluble sugars, amino acids, or organic acids (Grayston et al., 1996). By exuding compounds of varying chemical quality, roots regulate microbial physiology and extracellular enzyme production in ways that can both accelerate or decelerate SOM decomposition and increase or decrease nutrient availability (Cheng et al., 2014). Consequently, there is a need to develop a theoretical and predictive understanding of exudate impacts on soil biogeochemistry, in order to develop improved strategies that maximize ecosystem services while minimizing environmental degradation. In forests, most studies of the biogeochemical impacts of exudates have focused on quantifying exudation rates or rhizosphere C fluxes (Phillips and Fahey, 2005; Phillips et al., 2011; Brzostek et al., 2013; Yin et al., 2013; Cheng et al., 2014). Much less is known about variation in the chemical quality of exudates (among tree species or within the same species growing indifferent environmental conditions), and how such variation can influence microbial communities and ecosystem processes. Most exudates are organic compounds (Smith, 1976; Grayston et al., 1996) that have C:N ratios greater than those of the microbial biomass (Cleveland and Liptzin, 2007). This can create strong competition between roots and microbes for N in the rhizosphere, leading to N immobilization and exacerbated nutrient limitation for plants (Jackson et al., 2008; Frank and Groffman, 2009). Moreover, tree species can differ in their exudate stoichiometry (Smith, 1976), and such differences have the potential to alter bacterial (Eilers et al., 2010), fungal (Broeckling et al., 2008) or both bacteria and fungal (de Graaff et al., 2010) communities, and consequently SOM decomposition and nutrient cycling via priming effects (Landi et al., 2006; Drake et al., 2013).



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کلمات کلیدی:

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