首页|海南岛热带原始林地不同海拔梯度森林土壤易氧化有机碳分布规律及其影响因素

海南岛热带原始林地不同海拔梯度森林土壤易氧化有机碳分布规律及其影响因素

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[目的]研究热带海岛原始雨林不同海拔梯度土壤易氧化有机碳的分布格局及影响因子,以期为海南热带雨林土壤碳库合理评测及科学管理提供理论依据.[方法]以海南岛东南部典型热带原始雨林区的森林土壤为研究对象,测定土壤易氧化有机碳含量和土壤理化性质,分析不同海拔梯度森林土壤不同土层易氧化有机碳分布规律和影响因素.[结果]海南岛东南部典型原始热带雨林区0~60 cm土壤易氧化有机碳含量均值为4.22 g/kg,变化范围为2.31~8.11 g/kg;研究区各海拔梯度森林土壤剖面中,研究区土壤易氧化有机碳含量在0~20 cm土层中占比最高,七仙岭为44.81%,五指山为42.97%,吊罗山为47.89%.在不同海拔梯度同一土层内,五指山和吊罗山自然保护区土壤易氧化有机碳含量随海拔的升高呈现出先减少再增加的趋势;七仙岭国家森林公园土壤易氧化有机碳含量随海拔的升高呈现出先增加再减少再增加的变化趋势.研究区土壤易氧化有机碳含量与海拔梯度呈极显著正相关关系,相关系数为0.608,与土壤pH呈极显著负相关关系,相关系数为-0.366,而与土壤颗粒组成均未达到显著相关(P<0.01).[结论]研究区土壤易氧化有机碳含量呈现出明显的"表聚现象",研究区不同样点森林土壤易氧化有机碳含量随海拔的升高呈现出不同变化趋势;海拔和pH是影响研究区森林土壤易氧化有机碳分布格局的重要因素.
Distribution and influencing factors of the readily-oxidizable organic carbon in tropical virgin forest soils at different altitude gradients on Hainan Island
[Objective]This study investigated the distribution patterns and influencing factors of readily-oxidable organic carbon in soils across different altitude gradients within tropical island virgin rain-forests,aimed at establishing a theoretical foundation for the rational assessment and scientific management of soil carbon pools in the tropical rainforests of Hainan.[Method]Forest soils from a typical tropical prime-val rainforest area in southeastern Hainan Island were selected as the research object.The study measured the content of readily oxidizable organic carbon in the soil,along with analyzing the soil's physical and chemi-cal properties.The distribution patterns and influencing factors of this carbon component were examined in different soil layers across varied altitude gradients.[Result]The results indicated that the average content of readily oxidizable organic carbon in the 0~60 cm soil layer of the typical primitive tropical rainforest area in southeastern Hainan Island was 4.22 g/kg,with a range of variation from 2.31 to 8.11 g/kg.Notably,in the forest soil profiles at different altitude gradients,the content of readily oxidizable organic carbon was highest in the 0~20 cm soil layer,accounting for 44.81%in Qixianling,42.97%in Wuzhishan,and 47.89%in Diaoluoshan.Furthermore,within the same soil layer across different altitude gradients,the con-tent of readily oxidizable organic carbon in Wuzhishan and Diaoluoshan Nature Reserves exhibited a pattern of initially decreasing and then increasing with altitude.Conversely,in Qixianling National Forest Park,the content displayed a pattern of initially increasing,then decreasing,and finally increasing with altitude.More-over,a significant positive correlation was observed between the content of readily oxidizable organic carbon and altitude(P<0.01),with a correlation coefficient of 0.608,while an equally significant negative correla-tion was found with soil pH(P<0.01),yielding a correlation coefficient of-0.366.There was no significant correlation with soil particle composition.[Conclusion]The content of readily oxidizable organic carbon in the soil exhibited a notable"surface aggregation"phenomenon in the study area.Additionally,different changing trends were observed in the content of readily oxidized organic carbon in forest soils at various points in the study area with increasing altitude,highlighting altitude and pH as key influencing factors in the distribution pattern of this carbon component in the forest soils of the area.

soil readily oxidizable organic carbonaltitude gradientPearson correlation analysisregres-sion model constructionHainan Island

王军广、吴丹、赵志忠、王鹏、吴雯、吴慧、董鹏

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海南师范大学地理与环境科学学院,海南 海口 571158

陕西师范大学地理科学与旅游学院,陕西 西安 570119

海南省地质调查院,海南 海口 570206

土壤易氧化有机碳 海拔梯度 Pearson相关分析 回归模型构建 海南岛

2024

甘肃农业大学学报
甘肃农业大学

甘肃农业大学学报

CSTPCD北大核心
影响因子:0.612
ISSN:1003-4315
年,卷(期):2024.59(6)