东北地区落叶松林碳固持能力及其影响因素OA
Carbon Sequestration Capacity of Larch Forests in Northeast China and Its Influencing Factors
为明确不同纬度梯度下落叶松林碳固持能力的差异及其影响因素,以东北地区大兴安岭、小兴安岭与长白山山脉9个不同纬度地区(桓仁、和龙、露水河、清河、带岭、五营、加格达奇、新林、漠河)的落叶松林为研究对象,采用清查法量化植被碳密度、土壤碳密度及年均固碳量,并结合林分结构和气候因子探究其对碳固持能力的影响.结果表明,落叶松植被碳密度和植被年均固碳量在9个纬度地区的波动范围分别为22.44~126.69 t/hm²和1.05~4.27 t C/(hm2·a),二者在不同纬度地区均存在显著差异(P<0.05),小兴安岭地区植被年均固碳量为最高.0~10、10~20、20~30、30~40、40~50 cm土壤层的有机碳质量分数在不同山系的波动范围分别为71.61~91.21、15.09~44.94、5.99~24.21、3.07~14.55、2.55~11.96 mg/g;土壤有机碳质量分数随深度增加显著降低,0~10 cm土壤有机碳质量分数在不同山系之间无显著差异,而在其他层次存在显著差异.土壤碳密度和总碳密度的波动范围分别为18.41~113.87 t/hm²和40.89~219.81 t/hm²,且在不同地区存在显著差异.植被碳密度和年均固碳量与纬度、年均气温和平均胸径等因子呈显著相关(P<0.05),但与年降水量无相关性(P>0.05).这表明,适宜的气候条件与稳定的林分结构有助于提升落叶松林碳积累能力.
To clarify the differences in carbon sequestration capacity of Larix gmelinii forests along different latitudinal gradients and their influencing factors,Larix gmelinii forests at nine sites with different latitudes across the Daxing'an-ling,Xiaoxing'anling,and Changbai Mountains in Northeast China(Huanren,Helong,Lushuihe,Qinghe,Dailing,Wuying,Jiagedaqi,Xinlin,and Mohe)were selected as study subjects.Using a forest inventory method,vegetation car-bon density,soil organic carbon density,and annual carbon sequestration rate were quantified,and the influence of stand structure and climatic factors on carbon sequenstration capacity was analyzed.The results showed that vegetation carbon density and annual vegetation carbon sequestration rate across the nine sites ranged from 22.44-126.69 t/hm2 and 1.05-4.27 t C/(hm2·a),respectively,both exhibiting significant regional differences(P<0.05),with the Lesser Khingan Mountains showing the highest annual sequestration rate.Soil organic carbon contents at depths of 0-10 cm,10-20,20-30,30-40,and 40-50 cm ranged from 71.61-91.21,15.09-44.94,5.99-24.21,3.07-14.55 mg/g,and 2.55-11.96 mg/g,respectively.Soil organic carbon content decreased significantly with increasing depth,showing no significant differences among regions at 0-10 cm but significant differences at deeper layers.Soil carbon density and total carbon density ranged from 18.41-113.87 t/hm² and 40.89-219.81 t/hm²,respectively,both differing signifi-cantly among regions.Vegetation carbon density and annual carbon sequestration rate were significantly correlated with latitude,mean annual temperature,and mean diameter at breast height(P<0.05),but showed no correlation with an-nual precipitation(P>0.05).These findings indicate that favorable climatic conditions and stable stand structure en-hance the carbon accumulation capacity of larch forests.
刘光明;王波;刘霁广;张全智
东北林业大学 生态学院,森林生态系统可持续经营教育部重点实验室,哈尔滨 150040黑龙江省自然资源权益调查监测院,哈尔滨 150030东北林业大学 生态学院,森林生态系统可持续经营教育部重点实验室,哈尔滨 150040东北林业大学 生态学院,森林生态系统可持续经营教育部重点实验室,哈尔滨 150040
农业科技
落叶松碳固持植被碳密度土壤碳密度纬度梯度气候因子林分结构森林生态系统
Larchcarbon sequestrationvegetation carbon densitysoil carbon densitylatitudinal gradientclimatic factorsstand structureforest ecosystem
《森林工程》 2026 (4)
659-668,10
国家重点研发计划项目(2021YFD2200401).
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