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

大兴安岭北部多年冻土区植被对活动层厚度变化的响应
引用本文:温理想,郭蒙,黄书博,于方冰,钟超,周粉粉.大兴安岭北部多年冻土区植被对活动层厚度变化的响应[J].冰川冻土,2021,43(5):1531-1541.
作者姓名:温理想  郭蒙  黄书博  于方冰  钟超  周粉粉
作者单位:东北师范大学地理科学学院 长白山地理过程与生态安全教育部重点实验室,吉林 长春 130024
基金项目:国家自然科学基金项目(41871103);吉林省教育厅“十三五”科学技术项目(JJKH20201172KJ)
摘    要:植被与多年冻土共同维系着大兴安岭地区的冷湿环境。随着全球气候变暖,大兴安岭多年冻土已发生严重退化,植被的生长也受到影响。在大兴安岭北部多年冻土区设置55个采样点,每个采样点采集多年冻土活动层厚度、林下灌木生物量和落叶松胸径树龄等指标,同时借助增强型植被指数(EVI)在区域尺度比较大片多年冻土区和岛状融区多年冻土区的植被生长状况。结果表明:黑龙江呼中国家级自然保护区(简称呼中保护区)活动层厚度的平均值为(0.47±0.14) m,保护区周边为(0.83±0.38) m,呼中保护区周边的活动层厚度大于保护区内。大片多年冻土区的活动层厚度平均值为(1.04±0.47) m,小于岛状融区多年冻土区的(1.40±0.41) m。呼中保护区和周边灌木生物量的平均值分别为(201.75±71.70) g·m-2和(259.10±111.14) g·m-2,胸径与树龄比值的平均值分别为(0.20±0.08)和(0.26±0.14)。大片多年冻土区和岛状融区多年冻土区林下灌木生物量的平均值分别为(128.31±63.33) g·m-2和(199.04±66.13) g·m-2,胸径树龄比的平均值分别为(0.30±0.13)和(0.59±0.21)。活动层厚度大的区域,灌木的生物量以及落叶松胸径树龄比都大于活动层厚度小的区域,表明活动层厚度增加对灌木和乔木的生长有一定的促进作用。EVI的结果显示岛状融区多年冻土区植被的生长状况以及植被覆盖情况好于大片多年冻土区,从区域尺度证明了多年冻土对植被生长存在限制作用。研究结果对于深入理解多年冻土变化及其环境效应具有重要意义。

关 键 词:多年冻土退化  活动层厚度  增强型植被指数(EVI)  大兴安岭  黑龙江呼中国家级自然保护区  
收稿时间:2021-07-09
修稿时间:2021-09-26

The response of vegetation to the change of active layer thickness in permafrost region of the north Greater Khingan Mountains
WEN Lixiang,GUO Meng,HUANG Shubo,YU Fangbing,ZHONG Chao,ZHOU Fenfen.The response of vegetation to the change of active layer thickness in permafrost region of the north Greater Khingan Mountains[J].Journal of Glaciology and Geocryology,2021,43(5):1531-1541.
Authors:WEN Lixiang  GUO Meng  HUANG Shubo  YU Fangbing  ZHONG Chao  ZHOU Fenfen
Institution:Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains,Ministry of Education,School of Geographical Sciences,Northeast Normal University,Changchun 130024,China
Abstract:Vegetation and permafrost jointly maintain the cold and humid environment in the Greater Khingan Mountains. With global warming, the permafrost in the Greater Khingan Mountains has been severely degraded, and the growth of vegetation has also been affected. In order to further explore the relationship between vegetation and permafrost in the Greater Khingan Mountains, this study set up 55 sampling points in the permafrost regions of the North Greater Khingan Mountains, and at each sampling point we collected indicators such as the active layer thickness (ALT), the biomass of understory shrubs, and the diameter of larch trees at breast height. Then we used the enhanced vegetation index (EVI) to compare the vegetation growth status of predominantly continuous permafrost and permafrost with isolated taliks at a regional scale. The results show that: (1) The average of ALT in Heilongjiang Huzhong National Nature Reserve is (0.47±0.14) m, and the ALT around the reserve is (0.83±0.38) m. The ALT around Heilongjiang Huzhong National Nature Reserve is greater than that in the reserve. The ALT in predominantly continuous permafrost is (1.04±0.47) m, which is less than (1.40±0.41) m in permafrost with isolated taliks. (2) The average biomass of Heilongjiang Huzhong National Nature Reserve and surrounding shrubs are (201.75±71.70) g·m-2 and (259.10±111.14) g·m-2, respectively, and the average ratios of diameter at breast height to tree age are (0.20±0.08) and (0.26±0.14), respectively. The average biomass of understory shrubs in predominantly continuous permafrost and permafrost with isolated taliks regions are (128.31±63.33) g·m-2 and (199.04±66.13) g·m-2, respectively, and the ratio of diameter at breast height to tree age was (0.30±0.13) and (0.59±0.21), respectively. In areas where the ALT is large, the biomass of shrubs and larch diameter at breast height are greater than those in the areas where the ALT is smaller, indicating that the increase in the ALT can promote the growth of shrubs and trees to a certain extent. (3) The results of EVI show that vegetation growth and vegetation coverage in permafrost with isolated taliks are better than those in predominantly continuous permafrost region. The study proves that at the regional scale permafrost has a restrictive effect on vegetation growth. The results of this study are of great significance for in-depth understanding of the relationship between permafrost changes and its environmental effects.
Keywords:permafrost degradation  active layer thickness (ALT)  Greater Khingan Mountains  enhanced vegetation index (EVI)  Heilongjiang Huzhong National Nature Reserve  
本文献已被 万方数据 等数据库收录!
点击此处可从《冰川冻土》浏览原始摘要信息
点击此处可从《冰川冻土》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