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川南坡地不同退耕模式对土壤团粒结构分形特征的影响
引用本文:王景燕,胡庭兴,龚伟,宫渊波,罗承德.川南坡地不同退耕模式对土壤团粒结构分形特征的影响[J].应用生态学报,2010,21(6):1410-1416.
作者姓名:王景燕  胡庭兴  龚伟  宫渊波  罗承德
作者单位:四川农业大学林业生态工程省级重点实验室,四川雅安 625014
基金项目:国家"十五"科技攻关计划项目,国家"十一五"科技支撑计划项目,四川省教育厅项目,四川农业大学"211工程"创新团队项目资助
摘    要:运用分形模型,研究了川南坡地及其退耕成慈竹林、杂交竹林、桤木+慈竹混交林和弃耕地5年后土壤团粒结构分形维数,探讨了分形维数与土壤理化性质之间的关系.结果表明:退耕后,不同退耕模式样地>0.25 mm的土壤团聚体和水稳性团聚体含量均显著增加,团粒结构分形维数介于1.377~2.826,为慈竹林<杂交竹林<桤木+慈竹混交林<弃耕地<农耕地,并随>0.25 mm的土壤团聚体及水稳性团聚体含量的增加而降低;土壤自然含水量、毛管孔隙、有机质、全氮、碱解氮、全磷和全钾含量增加,而土壤容重、非毛管孔隙和通气度降低.退耕后的慈竹林、杂交竹林、桤木+慈竹混交林和弃耕地的土壤团粒结构分形维数与土壤理化性质相关性较好.农耕地退耕对增加>0.25 mm的土壤团聚体及水稳性团聚体含量和提高土壤结构稳定性具有较好的作用;土壤团粒结构分形维数可以作为坡地退耕后土壤肥力变化的理想指标,在研究区坡地退耕种植慈竹具有较好的培肥改土效益.

关 键 词:关键词  退耕模式  植被恢复  团粒结构  分形维数  宝天曼暖温带森林    土壤微生物群落结构    16S  rRNA    Illumina  Miseq  

Fractal features of soil aggregate structure in slope farmland with different de-farming patterns in south Sichuan Province of China
WANG Jing-yan,HU Ting-xing,GONG Wei,GONG Yuan-bo,LUO Cheng-de.Fractal features of soil aggregate structure in slope farmland with different de-farming patterns in south Sichuan Province of China[J].Chinese Journal of Applied Ecology,2010,21(6):1410-1416.
Authors:WANG Jing-yan  HU Ting-xing  GONG Wei  GONG Yuan-bo  LUO Cheng-de
Institution:Sichuan Provincial Key Laboratory of Ecological Forestry Engineering, Sichuan Agricultural University,Ya’an 625014,Sichuan, China
Abstract:By using fractal model, this paper studied the fractal dimension of soil aggregate structure (D) in the slope farmland (CK), its 5-year de-farmed Neosinocalamus affinis plantation (NAP), Bambusa pervariabilis×Dendrocalamopsis oldhami plantation (BDP), Alnus crenastogyne +Neosinocalamus affinis plantation (ANP), and abandoned farmland (AFL) in south Sichuan Province ofChina, and analyzed the relationships between the Dand soil physical and chemical properties. In the de-farmed plantations and abandoned farmland, the contents of >0.25 mm soil aggregates and water stable aggregates were increased significantly, compared with those in the slope farmland. The D was 1.377-2.826, being in the order of NAP<BDP<ANP<AFL<CK, and decreased with the increasing contents of >0.25 mm soil aggregates and water-stable aggregates. Comparing with CK, de-farming increased the soil natural water content, capillary porosity, and contents of soil organic matter, total N, alkali-hydrolysable N, total P,and total K, and decreased soil bulk density, non-capillary porosity, and aeration porosity. There were close relationships between the fractal dimension of soil aggregate structure and the soil physical and chemical properties. All the results suggested that the de-farming of slope farmland was beneficial to the increase of the contents of >0.25 mm soil aggregates and water-stable aggregates, and the enhancement of soil structure stability. The D could be used as an ideal index to evaluate soil fertility, and planting Neosinocalamus affinis onthe de-farming slope farmland was a good measure for the improvement of soil fertility in the research area.
Keywords:de-farming pattern  vegetation restoration  aggregate structure  fractal dimension  Baotianman warm temperate forest  soil bacterial community  16S rRNA  Illumina Miseq    
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