喀斯特山原红壤退化过程中土壤表层团聚体变化规律
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  • 英文篇名:The Variation of Surface Soil Aggregates in the Degradation Process of the Mountain Red Earth Zone Karst
  • 作者:张磊 ; 王嘉学 ; 刘保强 ; 肖梦景 ; 程艳芳 ; 许路艳
  • 英文作者:ZHANG Lei;WANG Jiaxue;LIU Baoqiang;XIAO Mengjing;CHENG Yanfang;XU Luyan;School of Tourism and Geographical Science,Yunnan Normal University;
  • 关键词:喀斯特 ; 山原红壤 ; 团聚体 ; 影响因素
  • 英文关键词:karst;;mountain red earth;;aggregate characteristics;;factors
  • 中文刊名:SDYA
  • 英文刊名:Mountain Research
  • 机构:云南师范大学旅游与地理科学学院;
  • 出版日期:2015-01-15
  • 出版单位:山地学报
  • 年:2015
  • 期:v.33
  • 基金:国家自然科学基金(41061021);; 云南省科技计划(2012CA024)~~
  • 语种:中文;
  • 页:SDYA201501002
  • 页数:8
  • CN:01
  • ISSN:51-1516/P
  • 分类号:10-17
摘要
山原红壤是古气候影响下残存于高原面的古红土,近年来退化严重。为认识山原红壤的退化机理及效应,以滇东喀斯特典型山原红壤发育地带为研究对象,分析了4种不同覆被条件下0~20 cm土壤表层团聚体的特征。结果表明:从草地→灌丛→松林→红裸土,土壤>0.25 mm水稳性团聚体含量(WSAC)和平均重量直径(MWD)逐渐减少,分形维数(FD)显著增大;团聚体破坏率(PAD0.25)则表现为松林<草地<灌丛<红裸土。山原红壤从有植被到无植被(红裸土)退化过程中,表层土壤的团聚体稳定性和其他物理性质劣化,抗水蚀能力变弱,有机质含量减少;草地、灌丛、松林之间的土壤团聚体特征变化不明显,尚不能准确反映植被间的退化过程。研究还表明水稳性团聚体的稳定性指标(WSAC、MWD)与容重呈显著负相关,与土壤密度呈极显著负相关,与孔隙度、通气度呈极显著正相关;有机质对水稳性团聚体的稳定性和其他物理性质具有促进作用,植被的保育是改善山原红壤结构状况的关键。
        Mountain red earth is the foe-hn Paleosol influenced by the ancient climate and has been degenerated seriously in recent years. In order to understand the mechanism of degradation and the effects of mountain red earth,and the typical development zone of the mountain red earth in Karst eastern Yunnan of China is chosen to analyze the characteristics of the 0 ~ 20 cm soil surface aggregates under the four different covers in red earth zone. The results indicate that > 0. 25 mm water stable aggregate content( WSAC) and mean weight diameter( MWD) are gradually reduced,but the fractal dimension( FD) increased significantly in process of grassland→shrub lands→pine wood → red bare soil. The percentage aggregate destruction( PAD) demonstrated: the law of pine wood
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