藏东南小型泥石流沉积区植被群落演替特征

【目的】藏东南是青藏高原乃至全国泥石流集中频发的地域,泥石流是区域内最重要的生态环境问题之一,因此,本文探寻了藏东南中小型泥石流的生态恢复技术。【方法】以时空互代法对藏东南不同年限泥石流沉积区植被演替特征进行调查统计,并以重要值确定不同年限泥石流沉积区植被群落组成。【结果】在海拔2700~3000 m范围内泥石流沉积区植物群落演替进程植物群落演替进程为西南草莓、苔草群落—藏川杨+鸡骨柴+苔草—藏川杨+越桔忍冬+苔草—藏川杨+高丛珍珠梅+苔草,乔木先锋种主要是藏川杨、灌木先锋种为鸡骨柴和高丛珍珠梅,草本植物为苔草;海拔3300~3600 m范围内泥石流沉积区植物群落演替进程为云南沙棘+云南锦鸡儿...

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Published in西南农业学报 Vol. 30; no. 6; pp. 1450 - 1457
Main Author 梁博 聂晓刚 万丹 喻武 杨东升 汪书丽
Format Journal Article
LanguageChinese
Published 西藏农牧学院高寒水土保持研究中心,西藏林芝860000%西藏农牧学院高原生态研究所,西藏林芝,860000 2017
西藏农牧学院资源与环境学院,西藏林芝860000
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ISSN1001-4829
DOI10.16213/j.cnki.scjas.2017.6.036

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Summary:【目的】藏东南是青藏高原乃至全国泥石流集中频发的地域,泥石流是区域内最重要的生态环境问题之一,因此,本文探寻了藏东南中小型泥石流的生态恢复技术。【方法】以时空互代法对藏东南不同年限泥石流沉积区植被演替特征进行调查统计,并以重要值确定不同年限泥石流沉积区植被群落组成。【结果】在海拔2700~3000 m范围内泥石流沉积区植物群落演替进程植物群落演替进程为西南草莓、苔草群落—藏川杨+鸡骨柴+苔草—藏川杨+越桔忍冬+苔草—藏川杨+高丛珍珠梅+苔草,乔木先锋种主要是藏川杨、灌木先锋种为鸡骨柴和高丛珍珠梅,草本植物为苔草;海拔3300~3600 m范围内泥石流沉积区植物群落演替进程为云南沙棘+云南锦鸡儿+蕨麻萎陵菜—糙皮桦+高丛珍珠梅+西南草莓—糙皮桦+云南锦鸡儿+西南草莓乔木先锋种主要是糙皮桦、灌木先锋种为云南锦鸡儿和高丛珍珠梅,草本植物为西南草莓。【结论】藏东南泥石流沉积区植被随着演替的进行,群落差异性逐渐增大。泥石流沉积区植被的恢复,在遵循一般的演替规律下,更应做到因地制宜。
Bibliography:51-1213/S
Southeast Tibet; Debris flow; Community succes-sion; Important value
LIANG Bo1 ,2, NIE Xiao-gang1,2, WAN Dan1,2 , YU Wu1,2, YANG Dong-sheng1.2, WANG Shu-li3 ( 1. College of Resources and Environment, Tibet College of Agrieuhure and Animal Husbandry, Tibet Linzhi 860000, China; 2. Research Center of Alpine and Cold Soil and Water Conservation, Tibet Aeademy of Agriculture and Animal Husbandry, Tibet Linzhi 860000, China; 3. Institute of Plateau Eeology of Tibet Institute of Agrieulture and Animal Husbandry, Tibet Linzhi 860000, China)
[ Objective] Debris flow is concentrated in the southeast of Tibetan in Tibetan Plateau and even the national. Debris flow is one of the most severe ecological environment problems in the region. Therefore, the ecological restoration technology of small and medium sized debris flow in Southeast Tibet was explored in this paper. [ Method]The characteristics of vegetation succession in the debris flow gully in the southeast of Tibetan by time-space mutual substitution method
ISSN:1001-4829
DOI:10.16213/j.cnki.scjas.2017.6.036