首页 | 本学科首页   官方微博 | 高级检索  
   检索      

浑善达克沙地沙地榆种子雨的扩散规律
引用本文:谷伟,岳永杰,李钢铁,潘文杰,哈丽雅.浑善达克沙地沙地榆种子雨的扩散规律[J].生态学报,2012,32(11):3440-3448.
作者姓名:谷伟  岳永杰  李钢铁  潘文杰  哈丽雅
作者单位:内蒙古农业大学,呼和浩特,010019
基金项目:内蒙古自然科学基金项目(2009BS0507);教育部博士点基金项目(20091515120009)
摘    要:于2010年采用定点连续观测的方法,研究了浑善达克沙地不同树龄(23年生、40年生、56年生)沙地榆孤立木种子雨的数量、组成及散布过程,分析沙地榆种子雨的扩散规律及其与外界环境干扰因子的关系。结果表明:(1)孤立木种子雨的总量随其年龄增长而增加,其中56年生孤立木>40年生孤立木>23年生孤立木,其种子雨的总量分别为(7744±16.26)粒/m2、(5236±18.87)粒/m2、(2456±12.67)粒/m2;(2)40年生孤立木的种子质量较好,成熟种子的比例最高,未成熟、空粒和虫害种子的比例较低,56年生孤立木次之,23年生孤立木质量最差,56年生沙地榆和40年生沙地榆是自然更新种子的主要来源;(3)榆树种子于当年5月下旬开始成熟并于6月初开始脱落,6月中旬达到降落高峰期,落种持续到6月下旬结束,落种期持续近1个月;(4)种子雨的前扩散过程中种子集中降落在主风向的下风向50 m和树冠周围20 m的范围内;(5)在种子的后扩散过程中,种子沿下风向继续运动,散落在下风向50 m范围或更远处,后扩散对前扩散表现为"削锋"作用。

关 键 词:浑善达克沙地  沙地榆  种子雨  扩散规律
收稿时间:5/4/2011 10:11:32 PM
修稿时间:2011/10/31 0:00:00

Diffusion of elm seed rain in Otindag Sand Land
GU Wei,YUE Yongjie,LI Gangtie,PAN Wenjie and HA Liya.Diffusion of elm seed rain in Otindag Sand Land[J].Acta Ecologica Sinica,2012,32(11):3440-3448.
Authors:GU Wei  YUE Yongjie  LI Gangtie  PAN Wenjie and HA Liya
Institution:Inner Mongolia Agricultural Uniersity,Inner Mongolia Agricultural Uniersity,Inner Mongolia Agricultural Uniersity,,
Abstract:Seed dispersal is an important stage in life style of plant population, the diffusion Pattern of seed directly affect the seedling colonization, distribution and the main resource of propagule. The production of seed is mainly controlled by the seed yield characteristic of tree species, but the seed dispersal not only connected with the tree species, but also with the various environmental disturbance factors. There are difference of seed dispersal pattern among species even, even within population.The characteristic of seed rain directly affect the size, quality, pattern and the reproductive of young seedling. Elm woodland-steppe is spread in the typical temperate steppe zone. Sand elm is the top community which adapt well to the semiarid and sub-humid sandy. Sand elm in Otindag Sand Land can protect the local environment effectively. But with the decrease of population of Sand elm recently, the stability and sustainable development will be hindered. Therefore, there has an imperative require for the population renewal strategies and vegetation restoration when considering the seed rain spatial and temporal distribution features. Through observing the seed rain's quantity, composition and dissemination process for different age isolation elm wood in Otindag Sand Land, we try to illuminate the diffusion rule of seed rain and the relationship between the diffusion of seed rain and the external environment by continuous observation in original position. By selected the different ages of sand elm wood (23 years, 40 years and 56 years) located in Otindag Sandy Land, the seed rain's quantity, composition, distribution process and the relationship between the disperse rule of seed rain and the environmental factors. The study area is located in the middle of Otindag Sandy Land in Sang Genda town attached to Zhenglan Banner(N42°41'-43°43',E115°57'-115°59'). The experiment was conduced continuously from 18th May to the end of 2th July 2010. We selected three kind of wood isolated with different ages (23 years, 40 years, 56 years) which in the uniform habitat such as elevation, slope, aspect and other conditions. At the same time, no sand elm was found around 100 m in the upper direction and around 50 m in the other three direction of isolated wood. The Seed rain collector was laid as the local main direction, surrounded with the isolate wood and separated for 5 meters from one collector to another. 120 collectors were distributed in 10 sub-direction. The Seed rain was collected every 2 day from the seed rain began to drop, until the seed falling completed. The collected sand elm seeds (with Samara) were divided into 5 levels according the intact and mature degree of seed. The level 1 of seed means the intact Samara and mature seeds, the level 2 means the winged Samara and the incomplete mature seeds, the level 3 means mature seed without Samar, the level 4 means seeds rotted or destroyed by insects and the level 5 means immature or empty seeds. One way AVOVA (SPSS 13.0, SPSS Inc. Chicago, Illinois, USA) was used to assess the significance of the treatment impacts, the least significant difference (LSD) and correlation analysis of different data sets, compare the difference between. The results showed that: (1) the quantities of seed rain increase with the age of elm, the order is old elm > medium age elm > small age elm, the quantities of seed rain for the 56, 40, 23 years old elm is(7744±16.3), (5236±18.9) and (2456±12.7) per square meter; respectively. (2)The quality of middle age Isolation seeds is better than that for the young trees and old trees which shows in the lower proportion of immature, empty grain and seed pests. The quality of 23 years old isolation seeds is worst. The seeds of old trees and the middle age trees are the main sources of natural regeneration seed. (3) Elm seed begins to mature in late May 2010, begins to fall in early June, reaches the peak of fall in mid-June and complete until late June. (4) Elm seeds diffuse within 50m of the main wind direction along the downwind and the range of 20m around crown in the course of the pre-dispersal, then scattered to the 50m of the downwind areas or more distant areas in the course of the. (5) The process of post-dispersal shows the "cut peak" effect to the pre-dispersal of seed rain.
Keywords:Otindag Sand Land  Ulmus pumila var  sabulosa  seed rain  Diffusion rule
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《生态学报》浏览原始摘要信息
点击此处可从《生态学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号