东北黑土土壤呼吸活化能特征及其影响因素分析
首发时间:2022-11-28
摘要:土壤呼吸是全球碳循环重要组成部分,其排放的CO2对全球气候变化具有重要影响。在全球气候变暖日益严峻的今天,土壤呼吸已经引起了国内外学者的广泛重视。目前尚未系统研究呼吸活化能及其与地理位置、采样深度、土地利用与树木种类的关系。本研究采集了东北松嫩平原7个地点农田-杨树防护林和8种林分类型0-100cm的土壤,室内培养实验测定土壤呼吸速率,结合阿伦尼乌斯方程计算土壤呼吸活化能(Ea)。结果表明:(1) 东北地区土壤呼吸活化能的分布范围是0.7-122.3 kJ mol-1,平均值为60.3 kJ mol-1,95% 置信区间为58.7-61.8 kJ mol-1。相比于其他研究,我国黑土Ea的分布区间较大。(2) 林型对Ea有较大影响:落叶松林土壤Ea值最高(64.3-88.5 kJ mol-1),蒙古栎林最低(57.67-73.7 kJ mol-1),落叶松林显著高于其他7种林型。这种种间差异可能与植物功能组有关:外生菌根林型高于丛枝菌根林型,但未达到统计学显著;针叶林显著高于阔叶林6%。(3)森林土壤Ea随土壤深度显著增加,而农田和防护林的有中间层变低的趋势。 (4) 土地利用类型对Ea影响较大,农田显著高于防护林15.4%。综上,与传统单一化学反应具有较稳定的活化能不同,微生物呼吸驱动的土壤呼吸活化能具有较大的分布范围。 我们从化学角度分析了东北地区土壤碳库的稳定性,研究结果服务于"双碳战略",为其提供基础数据支撑。
关键词: 生态学 阿伦尼乌斯方程 土壤呼吸 活化能 林型 土地利用类型
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Characteristics of respiration activation energy in black soil and its influence by plant species and soil collection location in Northeast China
Abstract:Soil respiration is an important part of the earth\'s carbon cycle, and the influence of soil on global climate is caused by CO2 emission from soil respiration. To date, limited data are available on the activation energy of soil respiration, and its association of sampling location and depths, land uses and tree species. This study collected 0-100cm soil from farmland shelterbelt (6 different locations) and Harbin Experimental Forest (8 stands) of Northeast China black soil area. The soil respiration activation energy (Ea) was calculated by the Arrhenius equation model on the basis of the soil respiration rate measured by incubation experiment. (1)The range of soil respiration activation energy in Northeast China is large, from 0.7 to 122.3 kJ mol-1, with an average value is 60.3 kJ mol-1, and the range of 95% confidence interval was from 58.7 to 61.8 kJ mol-1. Compared with other studies, Ea of black soil had a larger distribution range in China. (2) Forest types had marked different Ea. Larch forest\'s Ea ranged from 64.3-88.5 kJ mol-1, and lowest at oak forests (57.67-73.7 kJ mol-1). Larch forest\'s Ea was significantly higher than all other 7 forest types. This forest type\'s differences possibly related to functional groups of plants, i.e., the Ea of ECM type was higher than AM type but not up to statistical significance (P> 0.05); the Ea of coniferous forests was significantly higher than that in broadleaf forest by 6% (P < 0.05). (3) Ea of pooled 8 forest soils linearly increased with soil depths, however, poplar shelterbelts and farmland had a middle-depth lower Ea than the surface and deep soils. (4) Different land use types had a significant impact on Ea, and the Ea in farmland was significantly higher than that in poplar shelterbelt by 15.4%. In summary, unlike traditional simple chemical reactions with conservative and constant Ea, the Ea of soil respiration driven by microorganisms has a rather large range. Our data highlighted the importance of respiration Ea in understanding the stability of the soil carbon pool in northeast China from a chemical point of view, and the results could favor the "double-carbon strategy" via black soil carbon management.
Keywords: botany Arrhenius equation soil respiration activation energy forest type land use type
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