Carbon dioxide (CO2) emissions from naturally wet and drained nutrient-rich organic forests soils

A. Butlers, G. Spalva, Ieva Līcīte, Dana Purviņa
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Abstract

Implementation of climate change mitigation measures in forestry has a key role to successfully fulfil the climate change policy goals of Land use, land use change and forest sector set by the Paris Agreement to fully offset total GHG emissions in the country by CO2 removals in 2050. GHG emissions from organic soils in forest land have significant impact on total emissions of Latvia, however, high emissions also indicate the potential of climate change mitigation measures. This study aims to evaluate CO2 emissions from drained and naturally wet nutrient-rich forest soils to improve knowledge of forest management practice impact on GHG emissions. The study is conducted in 21 drained (Myrtillosa turf.mel. and Oxalidosa turf. mel.) and 10 naturally wet (Dryopterioso–caricosa and Filipendulosa) forest sites with nutrient-rich organic soils for 12 consecutive months. Soil total CO2 emissions were measured by closed manual non-transparent chamber method. The groundwater level, soil and air temperature were measured to evaluate factors affecting CO2 emission. Empirical data collected within the scope of the study showed high correlation (r = 0.85) between CO2 emissions and temperature, however, the groundwater level depth had no considerable impact on emissions. Total soil CO2 emissions from drained nutrient-rich organic soils ranged from 5.44 t ± 0.1 tC·ha·yr in black alder stands to 9.76 ± 2.47 tC·ha·yr in clearcut areas (average 7.35 ± 0.89 tC·ha·yr), while CO2 emissions from forest sites with naturally wet soil ranged from 5.73 ± 2.23 tC·ha·yr in spruce stands to 10.41 ± 4.33 tC·ha·yr in clearcut areas (average 7.02 ± 0.96 tC·ha·yr). The study results demonstrate that drainage does not have significant effect on CO2 emissions.
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自然湿润和排水的营养丰富的有机森林土壤的二氧化碳排放
在林业领域实施气候变化缓解措施,对于成功实现《巴黎协定》规定的土地利用、土地利用变化和森林部门的气候变化政策目标,即到2050年通过二氧化碳清除量完全抵消该国的温室气体排放总量,具有关键作用。林地有机土壤的温室气体排放对拉脱维亚的总排放量有重大影响,然而,高排放量也表明减缓气候变化措施的潜力。本研究旨在评估排水和自然湿润的富含营养的森林土壤的二氧化碳排放,以提高对森林管理实践对温室气体排放影响的认识。本研究在21个排水的紫金娘草皮上进行。和草皮草皮。在连续12个月的时间里,对10个有机土壤营养丰富的自然湿润森林(毛蕨和菲律宾)进行了研究。采用闭式人工非透明室法测定土壤总CO2排放量。通过测量地下水位、土壤温度和空气温度来评价影响CO2排放的因素。研究范围内的经验数据表明,CO2排放量与温度之间存在较高的相关关系(r = 0.85),而地下水位深度对CO2排放量的影响并不大。排干的富营养有机土壤的总土壤CO2排放量从黑桤木林分的5.44±0.1 tC·ha·yr到砍伐迹地的9.76±2.47 tC·ha·yr(平均7.35±0.89 tC·ha·yr)不等,而自然湿润土壤林分的CO2排放量从云杉林分的5.73±2.23 tC·ha·yr到砍伐迹地的10.41±4.33 tC·ha·yr不等(平均7.02±0.96 tC·ha·yr)。研究结果表明,排水对CO2排放影响不显著。
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