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应用生态学报 ›› 2005, Vol. 16 ›› Issue (8): 1417-1421.

• 研究论文 • 上一篇    下一篇

不同林地清理方式对杉木林土壤肥力的影响

薛立1,2,3, 向文静2, 何跃君2, 李燕2, 吴敏2, 徐燕2, 屈明2   

  1. 1. 中国科学院沈阳应用生态研究所, 沈阳 110016;
    2. 中国科学院会同森林生态试验站, 会同 418307;
    3. 华南农业大学林学院, 广州 510642
  • 收稿日期:2004-05-10 修回日期:2004-07-02 出版日期:2005-08-15 发布日期:2005-08-15
  • 通讯作者: 薛立,男,1958年生,博士,副教授.主要从事林分密度和自然稀疏及林木养分研究,发表论文50多篇,其中7篇被SCI收录.Tel:020-85283259;E-mail:forxue@scau.edu.cn
  • 基金资助:
    中国科学院知识创新工程重要方向项目(KZCX3-SW-418)、国家自然科学基金项目(30270268)和广东省林业局生态公益林中心资助项目(4400-F02084).

Effects of different ground clearance on soil fertility of Chinese fir stands

XUE Li1,2,3, XIANG Wenjing2, HE Yuejun2, LI Yan2, WU Min2, XU Yan2, QU Ming 2   

  1. 1. Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;
    2. Huitong Experimental Station of Forest Ecology, Chinese Academy of Sciences, Huitong 418307, China;
    3. College of Forestry, South China Agricultural University, Guangzhou 510642, China
  • Received:2004-05-10 Revised:2004-07-02 Online:2005-08-15 Published:2005-08-15

摘要: 研究了杉木林采伐迹地及采伐后的炼山迹地的土壤物理性质、养分含量、微生物数量和酶活性.结果表明,采伐迹地的非毛管孔隙比杉木林地增加23%,自然含水量和毛管持水量则下降2%;炼山迹地土壤容重比杉木林地增加10%,非毛管孔隙、自然含水量和毛管持水量分别下降61%、48%和26%.采伐迹地有机质、全N、全P和全K含量分别比杉木林地下降14%、14%、3%和22%,炼山迹地分别下降37%、37%、47%和7%.采伐迹地碱解N和有效K含量分别比杉木林地增加24%和31%,有效P含量比杉木林地下降1%;炼山迹地的碱解N、有效P和有效K含量分别比杉木林地下降2%、43%和40%.采伐迹地的细菌、真菌和放线菌数量比杉木林地增加1.4、11.3和0.8倍;炼山迹地细菌数量比杉木林地减少24%,真菌和放线菌数量增加了.0和0.倍.采伐迹地脲酶、过氧化氢酶和纤维素分解酶活性分别为杉木林地1.9、1.6和2.1倍,而炼山迹地分别为后者的3.4%、90%和106%.湿润土壤有机质、全N和全P含量高,疏松多孔的土壤有利于碱解N、速效P、速效K积累和脲酶活性的增加.真菌数量随毛管孔隙的增加而减少.通气良好有利于提高土壤过氧化氢酶活性.

关键词: 杉木林, 采伐迹地, 炼山迹地, 土壤肥力

Abstract: The study on the soil physical properties,nutrient contents,microbial amounts and enzyme activities of clear cutting and controlled burning Chinese fir stands showed that in comparing with the control,soil non-capillary porosity of clear cutting stand increased by 23%,whereas soil natural water capacity and capillary moisture capacity decreased by 25%.In controlled burning stand,soil bul穔 density increased by 10%,while soil non-capillary porosity,natural water capacity and capillary moisture capacity decreased by 61%,48% and 26%,respectively.The contents of soil organic matter,total N,total P and total K in clear cutting stand decreased by 14%,14%,35% and 22%,and in controlled burning stand,they decreased by 37%,37%,47% and 7%,respectively.Soil al穔alized N and available K in clear cutting stand increased by 24% and 31%,respectively,but soil available P decreased by 15%.The contents of soil al穔alized N,available P and available K in controlled burning stand decreased by 25%,43% and 40%,respectively.In clear cutting stand,the amounts of soil bacteria,fungi and actinomyces increased by 1.4,11.3 and 0.8 times,respectively,but in controlled burning stand,the amounts of soil bacteria decreased by 24%,while those of soil fungi and actinomyces increased by 5.0 and 0.5 times,respectively.The activities of soil urease,catalase and cellulase in clear cutting stand increased by 1.9,1.6 and 2.1 times,and in controlled burning land,they were 35%,90% and 106% of the control,respectively.Damp soil had higher contents of organic matter,total N and total P,whereas porous soil was favorable for the accumulation of al穔alized N,available P and available K and for the increase of soil urease activity.The amount of soil fungi decreased with increasing soil capillary porosity.Aerated soil was favorable for the increase of soil catalase activity.

Key words: Chinese fir stand, Clear cutting land, Control burning land, Soil fertility

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