芬兰温室气体清单中估算排干泥炭地森林土壤二氧化碳排放量的新方法

IF 3.9 2区 地球科学 Q1 ECOLOGY Biogeosciences Pub Date : 2023-09-21 DOI:10.5194/bg-20-3827-2023
Jukka Alm, Antti Wall, Jukka-Pekka Myllykangas, Paavo Ojanen, Juha Heikkinen, Helena M. Henttonen, Raija Laiho, Kari Minkkinen, Tarja Tuomainen, Juha Mikola
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引用次数: 2

摘要

摘要在排干用于林业的泥炭地,土壤碳(C)或二氧化碳(CO2)平衡受到以下两方面的影响:(i)更快分解的土壤有机质(SOM)释放的异养型CO2-C含量更高,以及(ii)生长更旺盛的森林输入的凋落物C含量更高。国家温室气体清单每年向《联合国气候变化公约》报告这种平衡以及管理土地上的其他温室气体汇和源。在本文中,我们提出了一种修订的,完全动态的方法来报告芬兰排水泥炭地森林土壤的二氧化碳平衡。该方法基于排水泥炭地森林SOM分解和凋落物输入的经验回归模型,可以跟踪树木生物量生长、采伐和气候参数的时间变化。包括地面植被以及活树和自然死亡的树木输入的地上和地下凋落物的所有主要成分,并辅以木本植物细根的新获得周转率。每年从采伐剩余物中输入的凋落物是使用国家伐木和树木能源使用统计数据来计算的。浸出,也从排干的泥炭地输出溶解的碳,不包括在内。按照温室气体清单的做法,将结果报告为1990-2021年的时间序列。我们修正后的方法得出芬兰1990 - 2021年期间年排放量从0.2 t CO2 ha - 1年增加到2.1 t CO2 ha - 1年的趋势(相当于整个4.3 Mha排水泥炭地森林的年排放量从1.4 m CO2 ha - 1增加到790 m CO2 yr - 1的趋势),在1990年和2021年之间存在统计学上的显著差异。在1990-2021年期间,在较温暖的芬兰南部,年平均排放量为1.5 t CO2 ha - 1年- 1 (2.2 Mha面积为340万吨CO2年- 1),在较冷的芬兰北部,年平均排放量为- 0.14 t CO2 ha - 1年- 1 (2.1 Mha面积为- 30万吨CO2年- 1)。结合树木生长产生的二氧化碳汇数据,在2021年,芬兰南部的排水泥炭地森林生态系统为1.0 t CO2 ha - 1 - 1(230万吨CO2年- 1),芬兰北部为1.2 t CO2 ha - 1 - 1(250万吨CO2年- 1)。我们将这些结果与之前在芬兰温室气体清单中使用的半动态方法产生的结果进行了比较,并讨论了与更静态的排放因子相比,新修订方法的优势和弱点。
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A new method for estimating carbon dioxide emissions from drained peatland forest soils for the greenhouse gas inventory of Finland
Abstract. In peatlands drained for forestry, the soil carbon (C) or carbon dioxide (CO2) balance is affected by both (i) higher heterotrophic CO2-C release from faster decomposing soil organic matter (SOM) and (ii) higher plant litter C input from more vigorously growing forests. This balance and other greenhouse gas (GHG) sinks and sources in managed lands are annually reported by national GHG inventories to the United Nations Climate Change Convention. In this paper, we present a revised, fully dynamic method for reporting the CO2 balance of drained peatland forest soils in Finland. Our method can follow temporal changes in tree biomass growth, tree harvesting and climatic parameters, and it is built on empirical regression models of SOM decomposition and litter input in drained peatland forests. All major components of aboveground and belowground litter input from ground vegetation as well as live trees and trees that died naturally are included, supplemented by newly acquired turnover rates of woody plant fine roots. Annual litter input from harvesting residues is calculated using national statistics of logging and energy use of trees. Leaching, which also exports dissolved C from drained peatlands, is not included. The results are reported as time series from 1990–2021 following the practice in the GHG inventory. Our revised method produces an increasing trend of annual emissions from 0.2 to 2.1 t CO2 ha−1 yr−1 for the period 1990–2021 in Finland (equal to a trend from 1.4 to 7.9 Mt CO2 yr−1 for the entire 4.3 Mha of drained peatland forests), with a statistically significant difference between the years 1990 and 2021. Across the period 1990–2021, annual emissions are on average 1.5 t CO2 ha−1 yr−1 (3.4 Mt CO2 yr−1 for 2.2 Mha area) in warmer southern Finland and −0.14 t CO2 ha−1 yr−1 (−0.3 Mt CO2 yr−1 for 2.1 Mha area) in cooler northern Finland. When combined with data on the CO2 sink created by the growing tree stock, in 2021 the drained peatland forest ecosystems were a source of 1.0 t CO2 ha−1 yr−1 (2.3 Mt CO2 yr−1) in southern Finland and a sink of 1.2 t CO2 ha−1 yr−1 (2.5 Mt CO2 yr−1) in northern Finland. We compare these results to those produced by the semi-dynamic method used earlier in the Finnish GHG inventory and discuss the strengths and vulnerabilities of the new revised method in comparison to more static emission factors.
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来源期刊
Biogeosciences
Biogeosciences 环境科学-地球科学综合
CiteScore
8.60
自引率
8.20%
发文量
258
审稿时长
4.2 months
期刊介绍: Biogeosciences (BG) is an international scientific journal dedicated to the publication and discussion of research articles, short communications and review papers on all aspects of the interactions between the biological, chemical and physical processes in terrestrial or extraterrestrial life with the geosphere, hydrosphere and atmosphere. The objective of the journal is to cut across the boundaries of established sciences and achieve an interdisciplinary view of these interactions. Experimental, conceptual and modelling approaches are welcome.
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