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The CO2 dependence of photosynthesis, plant growth responses to elevated CO2 concentrations and their interaction with soil nutrient status, II. Temperate and boreal forest productivity and the combined effects of increasing CO2 concentrations and in

机译:光合作用的CO2依赖性,植物生长对升高的CO2浓度的响应及其与土壤养分状况的相互作用,II。温带和寒带森林生产力以及二氧化碳浓度和

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摘要

Appropriate rates of carbon acquisition by temperate and boreal forests were re-evaluated. Based on continental-scale forestry data it was suggested that the productivity of temperate and boreal forests had been previously overestimated. Using thesevalues, a model of the integrated response of ecosystems to carbon dioxide concentration and soil nitrogen availability is presented. The model did not assume constant C:N ratios in plant or soil and considered the effect of increases in atmospheric CO2concentrations and nitrogen deposition separately or together. For temperate-zone forests a co-occurrence of a CO2 increase and N deposition doubled the increase in net primary productivity and carbon sequestration. Considered separately, the effect ofthe atmospheric CO2 increase was less than even moderate rates of anthropogenic N deposition for temperate or boreal forests. By contrast, for tropical forests, the atmospheric CO2 increase was sufficient to induce large rates of carbon accumulation in plants and soil. Application of the model at the global scale suggests large localized sinks for CO2 in either tropical rain forests or in forested or grassland areas of Europe and North America where appreciable N deposition occurs. Overall, the model suggests a terrestrial sink owing to CO2 fertilization and N deposition of about 0.2 Pmol C per year. Approximately half of this was in the mid-latitudes of the northern hemisphere and half in the tropics.
机译:重新评估了温带和北方森林的适当碳吸收率。根据大陆范围的林业数据,建议温带和北方森林的生产力以前被高估了。利用这些值,提出了生态系统对二氧化碳浓度和土壤氮素有效性的综合响应模型。该模型未假定植物或土壤中的C:N比率恒定,而是单独或一起考虑了大气CO2浓度和氮沉降增加的影响。对于温带地区的森林,同时出现二氧化碳增加和氮沉降使净初级生产力和碳固存增加一倍。单独考虑,对于温带或北方森林,大气CO2增加的影响甚至不到中等程度的人为氮沉积速率。相反,对于热带森林,大气中二氧化碳的增加足以引起植物和土壤中大量的碳积累。该模型在全球范围内的应用表明,热带雨林或欧洲和北美洲的森林或草原地区会出现大量的N沉积,因此会产生较大的局部CO2汇。总体而言,该模型表明,由于二氧化碳的施肥和每年约0.2 Pmol C的氮沉积,导致了一个地面下沉。其中大约一半在北半球的中纬度地区,而另一半在热带地区。

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