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作 者:朱丽琴[1] 黄荣珍[1] 黄国敏[1] 黄诗华[1] 易志强[1] 张文锋[1] 贾龙[1] 王赫[1] 刘勇[1] ZHU Liqin;HUANG Rongzhen;HUANG Guomin;HUANG Shihua;YI Zhiqiang;ZHANG Wenfeng;JIA Long;WANG He;LIU Yong(Nanchang Institute of Technology,330099, Nanchang,China;Jiangxi Key Laboratory of Degraded Ecosystem Restoration and Watershed Eco-hydrology 330099, Nanchang,China)
机构地区:[1]南昌工程学院,江西省退化生态系统修复与流域生态水文重点实验室,南昌330099
出 处:《中国水土保持科学》2017年第5期58-66,共9页Science of Soil and Water Conservation
基 金:国家自然科学基金“生态恢复对红壤严重侵蚀地土壤水库重建的影响与机制”(31160179);江西省自然科学基金目“侵蚀红壤碳吸存对植被恢复的响应及其微生物学机制”(20151BAB204033);江西省高等学校“十二五”水土保持与荒漠化防治重点学科培育基金“红壤侵蚀地不同植被恢复模式对土壤团聚体有机碳的影响”
摘 要:研究土壤团聚体的组成及其有机碳的分布,有助于从微观角度理解土壤结构与功能的相互作用。采用干筛法和湿筛法,研究南方红壤退化地实施人工恢复30年后,马尾松与阔叶复层林(PB)、木荷+马尾松混交林(SP)和阔叶林(BF)3种典型林分在0~60 cm土层的团聚体组成及其有机碳分布特征,分析土壤团聚体有机碳与总有机碳相关关系。结果表明:各恢复林分土壤机械稳定性团聚体质量分数,以>2 mm粒径所占比例最大(均在60%以上),而在水稳性团聚体中,以<0.05 mm粒径占优势。不同林分土壤团聚体结构破坏率顺序依次为BF(53.38%~84.27%)>SP(52.22%~70.86%)>PB(22.70%~47.83%)。机械稳定性和水稳性团聚体有机碳质量分数均以PB最高,随着土层深度的增加,各林分土壤团聚体有机碳质量分数呈下降趋势。水稳性大团聚体(>0.25 mm粒径)有机碳质量分数总体高于相应土层的总有机碳质量分数,而微团聚体的(<0.25 mm粒径)则低于后者,说明有机碳对于大团聚体的形成和水稳性具有积极作用。土壤团聚体有机碳与总有机碳的相关关系分析表明,土壤团聚体有机碳的增加,对总有机碳的积累具有正面影响。保留密度大、灌木(草)层盖度高的马尾松与阔叶复层林土壤团聚体的数量和质量更高;因此,在红壤侵蚀退化地森林恢复初期,可通过适当密植、增加林下灌草覆盖等措施,增加有机碳的输入,促进团聚体的形成和稳定,从而加速了退化土地的土壤结构改善和功能恢复。该研究可为南方严重红壤退化地生态恢复中的林分类型选择和优化配置提供科学依据。[Background]Research on the composition of aggregates and the distribution of organic carbon in soil will be beneficial for understanding the interaction between soil structure and function at the molecular scale.[Methods]Three typical artificially restored forests after a30-year restoration in degraded red soil were selected in this study,which were Pinus massoniana-multiple layer broadleaf forest(P B),Schima superba-Pinus massoniana mixed forest(S P),and broadleaf forest(B F),respectively.Methods of dry sieve and wet sieve were applied to investigate the composition of aggregates and the distribution of organic carbon in different layers(0-60cm)of soil in each of the three forests,following which the correlations between soil aggregate organic carbon and soil total organic carbon were also determined.[Results]For all three forests,particles larger than2mm in diameter constituted more than60%of mechanical-stable aggregates in soil,while particles less than0.05mm in diameter made up the majority of water-stable aggregates in soil.
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