生态与农村环境学报 ›› 2012, Vol. 28 ›› Issue (2): 128-132.doi:

• 区域环境与发展 • 上一篇    下一篇

退耕还湖安庆沿江湿地土壤颗粒分形特征

张平究, 赵永强   

  1. 安徽师范大学国土资源与旅游学院
  • 收稿日期:2011-10-24 修回日期:2011-11-25 出版日期:2012-03-25 发布日期:2012-03-27
  • 通讯作者: 张平究 安徽师范大学国土资源与旅游学院 E-mail:changpj2006@yahoo.com.cn
  • 作者简介:张平究(1975-),男,江西玉山人,副教授,博士,主要从事土壤环境质量及其微生物学指示研究。E-mail:changpj2006@yahoo.com.cn
  • 基金资助:

    安徽省高校省级自然科学研究项目(KJ2008B264)

Fractal Features of Soil Particles of Riverain Wetlands Recovered From Farmlands in Anqing, Anhui Province

ZHANG  Ping-Jiu, ZHAO  Yong-Qiang   

  1. College of Territorial Resource and Tourism,Anhui Normal University
  • Received:2011-10-24 Revised:2011-11-25 Online:2012-03-25 Published:2012-03-27
  • Contact: ZHANG Ping-Jiu College of Territorial Resource and Tourism,Anhui Normal University E-mail:changpj2006@yahoo.com.cn

摘要: 以安庆沿江不同退耕还湖方式(白荡湖区,低坝高网式养鱼;菜子湖区,自然恢复湿地)和不同历史利用方式(水耕和旱耕)的湿地土壤为研究对象,分析退耕还湖后湿地土壤的颗粒分形特征变化。结果表明,退耕还湖后白荡湖区湿地土壤颗粒分形维数和<0.01 mm粒径颗粒含量降低,而历史水耕湿地土壤颗粒分形维数降幅小于历史旱耕湿地;菜子湖区湿地土壤颗粒分形维数和<0.01 mm粒径颗粒含量升高,而历史水耕湿地土壤颗粒分形维数增幅大于历史旱耕湿地。2个湖区土壤颗粒分形维数与土壤细黏粒、粗黏粒和细粉粒含量呈显著正相关(P<0.01),,与粗粉粒、细砂粒和粗砂粒含量呈显著负相关(P<0.01),与土壤有机质、全磷和有效氮含量呈显著正相关(P<0.01),土壤颗粒分形维数和土壤养分含量的聚类分析结果总体相似。土壤颗粒分形维数可作为评价退耕还湖后湿地生态恢复过程中土壤演变状况的重要参考指标。

关键词: 退耕还湖, 湿地土壤, 分形维数, 安庆

Abstract: Soils of recovered wetlands different in land use history(paddy and upland farming)and in mode(low dam and high net aquaculture in Baidang Lake and naturally recovered wetland in Caizi Lake)in Anqing were sampled for study of changes in fractal feature of soil particles after returning farmland to lake(RFL).Results show that in Baidang Lake area the fractal dimension of soil particles and the content of <0.01 mm particles decreased after RFL,and the change of the former was less significant in welands that used to be paddy fields than in wetlands that used to be upland fields,while in Caizi Lake area,the fractal dimension of soil particles and the content of <0.01 mm particles in creased after RFL,and the changes of the formaer was more significant in welands that used to be paddy fields than in wetlands that used to be upland fields.The fractal dimension of soil particles of the wetlands in these two areas were significantly and positively related to the contents of fine clay,coarse clay,and fine sit (P<0.01)and to the contens of soil organic matter,total P and available N(P<0.05),but negatively to the contents of coarse silt,fine sand and coarse sand (P<0.01).On the whole,the fractal dimension of soil particales of the wetlands is quite similar to the result of clustering analysis of soil nutrient contents.It is,therefore,suggested that fractal dimension of soil particles be used as a comprehensively quantitative index to evaluate changes in soil of the wetlands after RFL.

Key words: returning farmland to lake, wetland soil, fractal dimension of soil particle, Anqing

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