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应用生态学报 ›› 2018, Vol. 29 ›› Issue (2): 483-491.doi: 10.13287/j.1001-9332.201802.012

• 研究报告 • 上一篇    下一篇

锡林浩特草原小叶锦鸡儿灌丛的阻雪能力及其对积雪形态的影响

闫敏1, 左合君1*, 董智2, 刘宝河1, 王嫣娇1, 魏翔鸿1, 李钢铁1   

  1. 1内蒙古农业大学沙漠治理学院/内蒙古风沙物理与防沙治沙工程重点实验室, 呼和浩特 010011;
    2 山东农业大学林学院, 山东泰安 271018
  • 收稿日期:2017-06-28 出版日期:2018-02-18 发布日期:2018-02-18
  • 通讯作者: E-mail: zuohj@126.com
  • 作者简介:闫 敏, 男, 1992年生, 博士研究生. 主要从事荒漠化防治研究. E-mail: ym5233@126.com
  • 基金资助:

    本文由国家自然科学基金项目(41361012)资助

Capacity of Caragana microphylla shrub on counteracting snow movement and its influence on snow morphology in the Xilinhot Steppe, China.

YAN Min1, ZUO He-jun1*, DONG Zhi2, LIU Bao-he1, WANG Yan-jiao1, WEI Xiang-hong1, LI Gang-tie1   

  1. 1College of Desert Control Science and Engineering, Inner Mongolia Agricultural University/Inner Mongolia Key Laboratory of Aeolian Physics and Desertification Control Engineering, Hohhot 010011, China;
    2 College of Forestry, Shandong Agricultural University, Tai’an 271018, Shandong, China
  • Received:2017-06-28 Online:2018-02-18 Published:2018-02-18
  • Contact: E-mail: zuohj@126.com
  • Supported by:

    This work was supported by the National Natural Science Foundation of China (41361012).

摘要: 通过对典型草原区小叶锦鸡儿灌丛积雪体的调查,研究了灌丛特征(灌丛高度、灌丛迎风侧宽度、灌丛顺风侧长度)对积雪形态(积雪高度、积雪宽度、雪辫长度)的影响.结果表明:小叶锦鸡儿灌丛高度与积雪形态参数呈显著二次多项式函数关系,灌丛迎风侧宽度、灌丛顺风侧长度与积雪形态参数呈显著幂函数关系(指数<1).灌丛积雪形态和发育特征是灌丛特征参数共同影响和作用的结果,其中,灌丛高度对积雪高度影响最大,灌丛迎风侧宽度对积雪宽度和雪辫长度影响最大.灌丛较小时积雪形态发育较快,随后逐渐趋于稳定.灌丛二维滞雪范围模型直接反映灌丛对风力的干扰范围和积雪的潜在范围,间接反映灌丛的滞雪能力;灌丛三维阻雪体积模型直接反映一定雪源、风况条件下灌丛的阻雪能力.本文建立的灌丛滞雪范围和灌丛阻雪体积模型可为典型草原风吹雪区积雪资源估算和雪害防治提供理论依据.

Abstract: The aim of this study was to examine the impacts of characteristics of the shrub (shrub height, shrub width on the windward side, shrub length on the downwind side) on the snow morphology (snow height, snow width, and snow tail length) in the typical steppe of Xilinhot, China. The relationship between shrub height and parameters of snow morphology showed significant quadratic polynomial regression. The relationship between shrub width on the windward side, length on the downwind side and parameters of snow morphology showed significant power function (exponent was less than 1). The morphology and development characteristics of shrub snow were affected by the shrub characteristic parameters. Shrub height had the greatest influence on snow height. Shrub width at the windward side had the greatest influence on snow width and snow tail length. The snow morphology developed faster when the shrub was small, and then tended to be stable. The two-dimensional snow retention range model of shrub directly reflected the disturbance range of shrub to wind and the potential range of snow, indirectly reflected the capacity of shrub to retard snow movement. The three-dimensional snow blocking volume model of shrub snow directly reflected the snow resistance capacity of shrub under certain snow sources and wind conditions. Both models established here would provide a theoretical basis for estimating snow resources and preventing snow disaster in the wind blown snow area of typical steppe.