[1]王世杰,张信宝,白晓永.南方喀斯特石漠化分区的名称商榷与环境特点[J].山地学报,2013,(01):18.
　WANG Shijie,ZHANG Xinbao,BAI Xiaoyong.Discussion on Nomenclature of the Karst Desertification Regions and Illustration for Their Environment Characteristics in Southwest China[J].Mountain Research,2013,(01):18.
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南方喀斯特石漠化分区的名称商榷与环境特点()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2013年01期
页码:
18
栏目:
山地环境
出版日期:
2013-01-01

文章信息/Info

Title:
Discussion on Nomenclature of the Karst Desertification Regions and Illustration for Their Environment Characteristics in Southwest China
作者:
王世杰;  张信宝; 白晓永
1. 中国科学院地球化学研究所环境地球化学国家重点实验室，贵州 贵阳 550002；
2. 中国科学院水利部 成都山地灾害与环境研究所，四川 成都 610041；
3. 中国科学院普定喀斯特生态系统观测研究站，贵州 普定 562100
Author(s):
WANG Shijie;  ZHANG Xinbao; BAI Xiaoyong
1. State Key Laboratory of Environmental Geochemistry，Institute of Geochemistry，Chinese Academy of Sciences，Guiyang 550002，China； 　　
2. Institute of Mountain Hazards and Environment，Chinese Academy of Sciences，Chengdu 610041，China； 　　3. Karst Ecosystem Observation Research Station in Puding，Chinese Academy of Sciences，Puding 562100，Guizhou, China
关键词:
喀斯特; 地貌; 区域分异; 石漠化
Keywords:
karst; geomorphology; regional variation ; karst land desertification
分类号:
P642.22
文献标志码:
A
摘要:
阐明了锥、塔峰等热带喀斯特地貌发育的适宜的气候和地质地貌条件，论述了我国南方喀斯特地区喀斯特地貌空间分布与气候和地质地貌条件的关系。针对现行《石漠化分区》命名存在的科学系统性问题，对石漠化分区的命名系统提出了修改意见：将我国南方喀斯特地区分为锥、塔峰喀斯特地貌区和非锥、塔峰喀斯特地貌区2个区。锥、塔峰喀斯特地貌区，根据喀斯特地貌类型分为浅碟型峰丛洼地，漏斗型峰丛洼地和峰林平原等3个亚区，分别对应原《石漠化分区》的岩溶高原区，峰丛洼地区和峰林平原区。非锥、塔峰喀斯特地貌区，根据区域地貌类型分为高原盆谷，高原峡谷，高原和中低山槽谷，中高山和中低山等5个亚区，分别对应原石漠化分区的岩溶断陷盆地区，岩溶峡谷区，岩溶槽谷区，中高山区和溶丘洼地（槽谷）区。鉴于热带喀斯特地貌区裸露性喀斯特坡地分布广，石漠化严重，特别是漏斗型峰丛洼地亚区裸露性喀斯特坡地面积比例高，是南方喀斯特地区石漠化最为严重的地区，也是集中连片的国家级贫困区，建议南方石漠化治理向黔桂滇接壤的漏斗型峰丛洼地亚区倾斜。
Abstract:
Suitable climatic，geological and geomorphologic conditions for tropical karst landforms，such as cone and tower karst hills，are illustrated and the relationship of spatial distribution of cone and tower karst hills with those conditions in the karst areas of Southwest China. Aiming at the problem of scientific systems on the standing nomenclature of “karst desertification division”，some modification suggestions for the nomenclature are putted forward: the karst areas in southwest China are divided into two regions: the cone and tower karst region and the noncone and tower karst region. According to the karst morphology，the cone and tower karst region is further divided into three subregions: the Peak-Cluster Depression region of shallow dish type ；the Peak-Cluster Depression region of funnel type；and the peak forest plain region. Those subregions are correspondent to the karst plateau region，the Peak-Cluster Depression region and the peak forest plain region，respectively. According to the regional landforms，the noncone and tower karst region is further divided into five subregions: the plateau basin valley region；plateau gorge valley region；the plateau and midlow mountain trough valley region；the highmid plateau region；and the midlow mountain region，respectively.

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备注/Memo

备注/Memo:
收稿日期(Received date)：2012-12-20；改回日期(Accepted) :2012-12-30。
基金项目（Foundation item）:国家973项目(2013CB956702)，中国科学院战略性先导科技专项重大课题（XDA05070400），国家自然科学
基金项目(41001162)，贵州省科技计划(黔科合重大专项字﹝2012﹞6015号)。[ Financially supported by 973 Program (Grant Nos. 2013CB956702), the Strategic Priority Research Program — Climate Change：Carbon Budget and Related Issues of the Chinese Academy of Sciences (Grant No. XDA05070400), the National Natural Science Foundation of China (Grant No. 41001162), andMajor special plan of science and technology and Social Development Scientific Research Programs of Guizhou (Grant No 2011-3076).]
作者简介（Biography）：王世杰(1966-),男,研究员,博士生导师,主要从事喀斯特生态环境研究 [Wang Shijie(1966-)，male，professor，doctoral supervisor，specialized in karst environment.] E-mail：wangshijie@vip.skleg.cn]
更新日期/Last Update: 1900-01-01