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亚热带退化森林不同恢复方式对土壤团聚体胶结物质及稳定性的影响
引用本文:蔡琳,杨予静,种玉洁,袁义平,曾翔宇,姚和风,陈初明,李中强,魏立飞,余海燕.亚热带退化森林不同恢复方式对土壤团聚体胶结物质及稳定性的影响[J].生态学报,2023,43(9):3689-3698.
作者姓名:蔡琳  杨予静  种玉洁  袁义平  曾翔宇  姚和风  陈初明  李中强  魏立飞  余海燕
作者单位:湖北大学, 资源环境学院, 区域开发与环境响应湖北省重点实验室, 武汉 430062;湖北省黄冈市罗田县大别山薄刀峰国有林场, 黄冈 438600
基金项目:国家自然科学基金(32001298); 湖北省教育厅重点项目(D20201001); 大学生创新训练项目(S202110512085)
摘    要:退化森林的恢复一直是林业和生态学研究的热点。良好的森林土壤结构有助于林木生长发育,作为土壤最基本的结构单元,土壤团聚体组成和稳定性是衡量土壤肥力和质量的重要指标,其团聚结构的形成依靠土壤胶结物质。然而,土壤胶结物质与团聚体稳定性之间的关系尚不确定。为探明亚热带退化森林的不同恢复方式对团聚体稳定性的影响及其潜在机制,以自然恢复的次生林为对照(CK),选取了亚热带三种常见的人工林:一代杉木林(P1)、二代杉木林(P2)和黄山松林(P3),测定土壤团聚体稳定性及其胶结物质的含量,并分析了各胶结物质对团聚体稳定性的影响。研究发现:不同森林恢复方式显著影响了土壤pH值、碳氮比、速效磷含量、团聚体的组成和稳定性。所有森林类型中,三种人工林的团聚体稳定性显著高于CK,P2的大团聚体所占比例最大,团聚体稳定性最高。恢复方式显著影响了土壤游离氧化铁含量、菌根密度和易提取球囊霉素相关土壤蛋白(EEG)含量。团聚体稳定性与游离氧化铁含量、菌根密度呈正相关,但与EEG含量呈负相关。研究结果表明,亚热带退化森林的人工恢复比自然恢复更有助于增强土壤团聚体稳定性,土壤游离氧化铁、菌根密度和EEG是显著影响团聚体稳定...

关 键 词:土壤团聚体稳定性  土壤游离氧化铁、铝  球囊霉素相关土壤蛋白  森林恢复方式  亚热带森林
收稿时间:2022/4/21 0:00:00
修稿时间:2022/10/11 0:00:00

Effects of different restoration approaches of subtropical degraded forests on bonding materials and stability of soil aggregate
CAI Lin,YANG Yujing,CHONG Yujie,YUAN Yiping,ZENG Xiangyu,YAO Hefeng,CHEN Chuming,LI Zhongqiang,WEI Lifei,YU Haiyan.Effects of different restoration approaches of subtropical degraded forests on bonding materials and stability of soil aggregate[J].Acta Ecologica Sinica,2023,43(9):3689-3698.
Authors:CAI Lin  YANG Yujing  CHONG Yujie  YUAN Yiping  ZENG Xiangyu  YAO Hefeng  CHEN Chuming  LI Zhongqiang  WEI Lifei  YU Haiyan
Institution:Hubei Key Laboratory of Regional Development and Environmental Response, Faculty of Resources and Environmental Sciences, Hubei University, Wuhan 430062, China;Bodaofeng Forest Farm, Luotian County, Huanggang 438600, China
Abstract:The restoration of degraded forest has been a hot topic in forestry and ecology. As a basic structural unit of soil, soil aggregate composition and stability are important indicators of soil fertility and quality, and the formation of soil aggregate relies on aggregate bonding materials. However, the relationship between aggregate bonding materials and aggregate stability is uncertain. To explore the effects of different restoration approaches of degraded subtropical forests on aggregate stability and its underlying mechanisms, we compared the secondary forest (natural restoration) as a control (CK), with three different common subtropical plantations which were: (1) first-generation Cunninghamia lanceolata (P1), (2) second-generation C. lanceolata (P2), and a Pinus. taiwanensis plantation (P3). We measured the aggregate stability and the contents of different aggregate bonding materials, and then analyzed the influence of these materials on soil aggregate stability. Results showed that forest restoration approach significantly affected soil pH, C/N, available phosphorus, as well as the composition and stability of aggregate. Among all the forests, the aggregate stability was significantly lower in CK than in the other three plantations, and P2 had the greatest proportion of large aggregates and the highest aggregate stability. The forest restoration approach also significantly affected soil free Fe oxide content, mycorrhizal density, and easily extractable glomalin-related soil protein (EEG). Aggregate stability was positively correlated with free Fe oxide content and mycorrhizal density, but negatively correlated with EEG. For subtropical degraded forests, the results indicated that artificial restoration was better than natural restoration to enhance soil aggregate stability, with soil free Fe oxide, mycorrhizal density and EEG being the main bonding materials that significantly affected the aggregate stability.
Keywords:soil aggregate stability|soil free Fe and Al oxides|glomalin-related soil protein|forest restoration|subtropical forests
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