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大气湿度升高塑造了银桦林生态系统的碳循环:一项 FAHM 研究。

Elevated atmospheric humidity shapes the carbon cycle of a silver birch forest ecosystem: A FAHM study.

机构信息

Institute of Ecology and Earth Sciences, University of Tartu, Lai 40, Tartu 51005, Estonia.

Institute of Ecology and Earth Sciences, University of Tartu, Lai 40, Tartu 51005, Estonia.

出版信息

Sci Total Environ. 2019 Apr 15;661:441-448. doi: 10.1016/j.scitotenv.2019.01.160. Epub 2019 Jan 15.

Abstract

Processes determining the carbon (C) balance of a forest ecosystem are influenced by a number of climatic and environmental factors. In Northern Europe, a rise in atmospheric humidity and precipitation is predicted. The study aims to ascertain the effect of elevated atmospheric humidity on the components of the C budget and on the C-sequestration capacity of a young birch forest. Biomass production, soil respiration, and other C fluxes were measured in young silver birch (Betula pendula Roth) stands growing on the Free Air Humidity Manipulation (FAHM) experimental site, located in South-East Estonia. The C input fluxes: C sequestration in trees and understory, litter input into soil, and methane oxidation, as well as C output fluxes: soil heterotrophic respiration and C leaching were estimated. Humidified birch stands stored C from the atmosphere, but control stands can be considered as C neutral. Two years of elevated air humidity increased C sequestration in the understory but decreased it in trees. Humidification treatment increased remarkably the C input to the soil. The main reason for such an increase was the higher root litter input into the soil, brought about by the more than two-fold increase of belowground biomass production of the understory in the humidification treatment. Elevated atmospheric humidity increased C sequestration in young silver birch stands, mitigating increasing CO concentration in the atmosphere. However, the effect of elevated atmospheric humidity is expected to decrease over time, as plants and soil organisms acclimate, and new communities emerge.

摘要

影响森林生态系统碳(C)平衡的过程受许多气候和环境因素的影响。在北欧,预计大气湿度和降水将会增加。本研究旨在确定大气湿度升高对 C 预算组成部分和年轻桦木林 C 固存能力的影响。在位于爱沙尼亚东南部的自由空气湿度操纵(FAHM)实验场,对生长在年轻银桦(Betula pendula Roth)林分中的生物量生产、土壤呼吸和其他 C 通量进行了测量。C 输入通量:树木和林下的 C 固存、凋落物输入到土壤中以及甲烷氧化,以及 C 输出通量:土壤异养呼吸和 C 淋溶都进行了估算。加湿桦林分从大气中储存 C,但对照林分可以被认为是 C 中性的。两年的空气湿度升高增加了林下的 C 固存,但减少了树木的 C 固存。加湿处理显著增加了土壤中的 C 输入。这种增加的主要原因是林下地下生物量生产增加了一倍多,导致根凋落物输入到土壤中的量增加。大气湿度升高增加了年轻银桦林分的 C 固存,缓解了大气中 CO 浓度的增加。然而,随着植物和土壤生物的适应以及新群落的出现,预计大气湿度升高的影响将随着时间的推移而减弱。

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