Nitrous oxide (N2O) and methane (CH4) fluxes from tree stems in birch and black alder stands - a case study in forests with deep peat soils

A. Lazdiņš, A. Butlers, Ritvars Ancāns
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Abstract

The aim of the study is to evaluate greenhouse gas (GHG) fluxes from stems in black alder (Alnus glutinosa (L.) Gaertn.) and birch (Betula pendula Roth) stands with drained and naturally wet nutrient rich peat soils, as well as to evaluate correlation between the GHG fluxes, soil temperature and groundwater level. The study was implemented in 8 forest stands – three black alder stands with nutrient rich peat soil (stand types according to national classification – Dryopterioso-caricosa and Filipendulosa) and 5 birch stands with peat soil (stand type Oxalidosa turf. mel. and Dryopterioso-caricosa). Measurement of GHG fluxes was continued for 12 months using Gasmet DX4040 FTIR analyser and removable non-transparent chambers of fixed volume and area. GHG fluxes were measured at 0.5, 1.0 and 1.5 m height on 3 trees in every stand. According to the study results the average CH4 emissions from stem surface in birch stands are 6.9 ± 6.2 g CO2 eq m·yr and in black alder stands 1.0 ± 3.2 g CO2 eq m·yr. Groundwater level significantly effects CH4 emissions – if it remains above 15 cm during summer, the CH4 emissions from stem increases to 84.0 ± 25.2 g CO2 eq. m·yr. Tree stems in drained peat soils are not a source of CH4 emissions. According to the study results tree stems in peat soils are not producing N2O emissions.
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一氧化二氮(N2O)和甲烷(CH4)从桦树和黑桤木林的树干通量-一个案例研究的森林与深泥炭土
本研究的目的是评估黑桤木(Alnus glutinosa, L.)茎部温室气体(GHG)通量。(桦树)和桦树(Betula pendula Roth)生长在排水和自然湿润的富含营养的泥炭土壤中,以及评估温室气体通量、土壤温度和地下水位之间的相关性。研究对象为8个森林林分,分别为3个营养丰富的泥炭土黑桤木林分(林分类型按国家分类-白杨和黄杨)和5个泥炭土桦木林分(林分类型为草皮)。梅尔。和Dryopterioso-caricosa)。使用Gasmet DX4040 FTIR分析仪和固定体积和面积的可拆卸非透明腔持续测量温室气体通量12个月。在0.5、1.0和1.5 m高度测量了每个林分3棵树的温室气体通量。研究结果表明,桦木林分茎表面CH4平均排放量为6.9±6.2 g CO2 eq m·yr,黑桤木林分茎表面CH4平均排放量为1.0±3.2 g CO2 eq m·yr。地下水位对CH4排放有显著影响,夏季地下水位高于15 cm时,地表CH4排放量增加至84.0±25.2 g CO2当量m·年。排干的泥炭土中的树干不是CH4排放源。根据研究结果,泥炭土壤中的树干不会产生N2O排放。
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