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应用生态学报 ›› 2017, Vol. 28 ›› Issue (5): 1431-1440.doi: 10.13287/j.1001-9332.201705.038

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浙西南毛竹林覆盖对土壤渗透性及生物特征的影响

王意锟1, 金爱武1*, 方升佐2   

  1. 1丽水学院, 浙江丽水 323000;
    2南京林业大学, 南京 210037
  • 收稿日期:2016-08-18 修回日期:2017-03-14 发布日期:2017-05-18
  • 通讯作者: *E-mail: kinaw@zafu.edu.cn
  • 作者简介:王意锟, 男, 1984年生, 讲师, 博士研究生. 主要从事竹林生态栽培和土壤环境修复研究. E-mail: wykknjfu@163.com
  • 基金资助:
    本文由国家重点基础研究发展计划项目(2012CB416904)资助

Effects of mulching management of Phyllostachys heterocycla forests on the characteristics of soil infiltration and biometrics in southwest Zhejiang Province, China

WANG Yi-kun1, JIN Ai-wu1*, FANG Sheng-zuo2   

  1. 1Lishui College, Lishui 323000, Zhejiang, China;
    2Nanjing Forestry University, Nanjing 210037, China
  • Received:2016-08-18 Revised:2017-03-14 Published:2017-05-18
  • Contact: *E-mail: kinaw@zafu.edu.cn
  • Supported by:
    This work was supported by the National Basic Research Program of China (2012CB416904)

摘要: 对浙西南山区4种不同覆盖年限下毛竹林地的土壤入渗、土壤理化性质、土壤根系和土壤动物特征进行了研究.结果表明:不同覆盖年限林地及同一林地不同土壤层次下土壤渗透性能存在较大差异,随着土层加深各林地土壤渗透性能均降低.渗透性能表现为覆盖1次林地>未覆盖林地>覆盖2次和3次后的林地.Kostiakov模型适合该研究区域的土壤水分入渗过程模拟.随着林地覆盖年限的增加(4~6年),林地土壤总孔隙度、非毛管孔隙度、pH值显著降低,而土壤容重、有机质和全N含量则显著提高.土壤初渗率、稳渗率、平均渗透率和渗透总量等均随根长密度减少而变小,土壤入渗能力的变化与直径0.5~5.0 mm的根长密度有关.不同覆盖年限毛竹林地土壤动物的平均密度差异显著,覆盖1次的林地最高,而覆盖3次的林地最低.综合纲、唇足纲、倍足纲、膜翅目、伪蝎目等大中型节肢动物,蜱螨目甲螨亚目、中气门亚目,以及弹尾目棘跳科、长角跳科、疣跳科、驼跳科等小型节肢动物数量的减少不利于土壤水分入渗.毛竹林长期覆盖会使土壤理化性状劣变,减弱土壤入渗性能,限制土壤动物活动,进而导致毛竹林退化.

Abstract: Soil infiltration, soil physical and chemical properties, root length density and soil fauna diversity were studied in Phyllostachys heterocycla forests with different mulching times in southwest Zhejiang Province, China. Significant differences of soil infiltration capability were found among the forests with different mulching times and among soil layers. Soil infiltration capability generally declined in the deeper soil layers. With mulching management, soil infiltration capability increased under the first mulching, and then declined with the increase of mulching times. The Kostiakov model was suitable for simulating soil infiltration process. With the extending of mulching times (4 to 6 years), soil pH and total/non-capillary porosity decreased, while soil bulk density, soil orga-nic matter and total nitrogen contents increased significantly. Soil initial, steady, and average infiltration rates as well as the cumulative infiltration amount correlated closely with the length density of roots with diameter from 0.5 mm to 5.0 mm, showing a decreasing tendency with the decrease in root length density. Soil fauna density was highest in the forest under the first mulching, and was lowest after third mulching. The decreased numbers of large and meso-arthropods, including Symphyla, Chilopoda, Diplopoda, Hymenoptera and pseudoscorpions, and the micro-arthropods, including Oribatida, Mesostigmata, Onychiuridae, Neanuridae, Cyphoderidae, and Entomobryidae, showed negative effects on soil infiltration. In conclusion, long-term mulching changed soil physical and chemical properties, decreased soil infiltration capability, and suppressed the development of soil fauna, which might cause the decline ofP. heterocycla forests.