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基于Vaganov-Shashkin模型的太白红杉径向生长对气候要素的响应

陈兰 李书恒 侯丽 史阿荣 白红英

应用生态学报2017,Vol.28Issue(8):2470-2480,11.
应用生态学报2017,Vol.28Issue(8):2470-2480,11.DOI:10.13287/j.1001-9332.201708.038

基于Vaganov-Shashkin模型的太白红杉径向生长对气候要素的响应

Response of Larix chinensis radial growth to climatic factors based on the Vaganov-Shashkin model

陈兰 1李书恒 1侯丽 1史阿荣 1白红英1

作者信息

  • 1. 西北大学城市与环境学院,西安710127
  • 折叠

摘要

Abstract

Tree ring width chronologies were established by core samples of Larix chinensis collected from the Herb Temple in southern slope and the Shangban Temple in northern slope of Taibai Mountain,respectively.Based on the Vaganov-Shashkin model,this paper discussed the responses of Qinling Mountains L.chinensis' radial growth to various climatic factors.The research found that the temperatures of growing season (from April to August),the precipitation in initial stage of growth and in July to August were the main climatic factors limiting the growth of L.chinensis.The higher temperature was favorable.for the growth of trees,but precipitation in the early stage of growth inhibited it.L.chinensis from the southern and northern slope of Qinling Mountains showed different responses to precipitation in July to August,in which abundant precipitation promoted the growth of L.chinensis in the northern slope,while inhibiting the growth in the southern slope.Even in the same slope,sampling sites with different altitudes brought discrepant responses of trees' radial growth to climatic factors.The L.chinensis at higher altitude needed lower growth temperature than that at lower altitude,but the former demanded greater soil moisture than the latter.The start day of growth had a great influence on the radial growth of L.chinensis,however,the end day of growth only affected that on the southern slope.

关键词

Vaganov-Shashkin模型/树木年轮/气候要素/太白红杉

Key words

Vaganov-Shashkin model/tree-ring/climate factors/Larix chinensis

引用本文复制引用

陈兰,李书恒,侯丽,史阿荣,白红英..基于Vaganov-Shashkin模型的太白红杉径向生长对气候要素的响应[J].应用生态学报,2017,28(8):2470-2480,11.

基金项目

本文由国家林业公益性行业科研专项(201304309)、陕西省自然科学基金项目(2014JQ5172)和黄土与第四纪地质国家重点实验室开放基金项目(SKLLQG1611)资助 This work was supported by the National Forestry Public Welfare Industry Scientific Research Project (201304309),the Shaanxi Natural Science Foundation (2014JQ5172) and the State Key Laboratory of Loess and Quaternary Geology (SKLLQG1611). (201304309)

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