[1]姜伏伟,郭福生*,杨安林.丹霞地貌岩体差异胀缩特征及其成景作用[J].山地学报,2018,(04):501-508.[doi:10.16089/j.cnki.1008-2786.000346]
　JIANG Fuwei,GUO Fusheng*,YANG Anlin.Differential Expansion and Contraction Characteristics of Danxia Landform Rock Mass and Its Geomorphological Effect[J].Mountain Research,2018,(04):501-508.[doi:10.16089/j.cnki.1008-2786.000346]
点击复制

丹霞地貌岩体差异胀缩特征及其成景作用()
分享到：

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2018年04期
页码:
501-508
栏目:
山地环境
出版日期:
2018-07-30

文章信息/Info

Title:
Differential Expansion and Contraction Characteristics of Danxia Landform Rock Mass and Its Geomorphological Effect
文章编号:
1008-2786-(2018)4-501-08
作者:
姜伏伟1;  郭福生2*; 杨安林1
1.贵州理工学院 资源与环境工程学院,贵阳55003; 2.东华理工大学 地球科学学院,南昌330013
Author(s):
JIANG Fuwei1;  GUO Fusheng2*;  YANG Anlin1
1.School of Resources and Environmental Engineering, Guizhou Institute of Technology, Guiyang 550003, China; 2.School of Earth Sciences, East China University of Technology, Nanchang 330013, China
关键词:
丹霞地貌;  膨胀试验;  胀缩过程;  成景作用
Keywords:
Danxia landform;  expansion test;  expansion and contraction process;  formation of landscapes
分类号:
P931
DOI:
10.16089/j.cnki.1008-2786.000346
文献标志码:
A
摘要:
丹霞地貌的研究主要以地质构造、地层岩性、外动力条件等宏观方面为主,但这些因素是地质景观形成的普遍性因素,未能较好解释丹霞地貌景观个体特征差异性原因。龙虎山丹霞地貌区岩性物质成分复杂,种类较多。本文从微观的角度,分析其岩体差异胀缩在丹霞地貌景观成因中的作用。选取研究区主要的6类物质成分岩块,在热、水、热-水三种条件下进行膨胀性试验,得出热膨胀率最大相差2.58倍,水膨胀率相差3.54倍,热-水膨胀率相差3.88倍。由于物质成分的差异性,当外界环境条件变化时,岩体内物质发生差异性胀缩。这种差异性胀缩引起岩体表面细粒物、砾石脱落,形成凹凸形态,构成了丹霞地貌成景的基础元素。研究区胀缩引起的凹凸形态,主要形成“脸型”“头型”和“身型”三类丹霞地貌景观。
Abstract:
The research on Danxia landform is mainly based on macroscopic aspects such as geological structure, stratum lithology and external dynamic conditions, but these factors are the universal factors for the formation of geological landscape, which fails to explain the differences in individual characteristics of Danxia landscapes.The lithologic composition of the Danxia landform area in Longhushan at Yingtang country, Jiangxi province, China is complex and has many types.From the microscopic point of view, this paper analyzed the role of the differential expansion and contraction of rock mass in the genesis of Danxia landform.The main six types of rock masses in the study area were selected, and expansion tests were carried out under the conditions of heating, water soaking and hydrothermal treatments.The maximum thermal volumetric expansion rate was 2.58 times.The water volumetric expansion rate was 3.54 times, and similarly the thermal-water volumetric expansion rate was obtained.The difference in expansion rate between water condition and heat condition was 3.88 times.Due to the differences in material composition, when the external environmental conditions changed, the material in the rock body underwent differential expansion and contraction, causing the fine particles and gravel on the surface of rock mass to fall off and then to form a concave and convex shape, which constituted the basic element of the Danxia landform in Longhushan.In the study area there are mainly three types of Danxia landforms, “face shape”, “head shape” and “body shape”.This paper provides a perspective from the volumetric expansion coefficient of sediments in red beds to study micro-geomorphology of Danxia landforms.

参考文献/References:

[1] 潘志新,彭华,任舫,等.美国Zion国家公园红层地貌发育研究[J].地球学报,2016,37(1):116-126.[PAN Zhixin, PENG Hua, REN Fang, et al.A study of the development of red bed landforms in Zion national park, the United States [J].Acta Geoscientica Sinica,2016,37(1):116-126]
[2] 丁宏伟,王世宇,尹政,等.张掖丹霞暨彩色丘陵地质成因及与南方丹霞地貌之对比[J].干旱区地理,2014,37(3):419-428.[DING Hongwei, WANG Shiyu, YIN Zheng, et al.Geologic origins of Danxia and colorful hills of Zhangye and comparison with Danxia landform in southern china[J].Arid Land Geography,2014,37(3):419-428]
[3] 程驰,周爱国,周建伟.广西桂平白石山丹霞地貌景观特色与成因过程[J].地球科学(中国地质大学学报),2013,38(3):641-648.[CHENG Chi, ZHOU Aiguo, ZHOU Jianwei.Landscape characteristics and cause process of Danxia landforms in Baishishan of Guiping city, Guangxi province[J].Earth Science-Journal of China University of Geoscience,2013, 38(3):641-648]
[4] 彭花明,刘林清,郭福生.浙江江郎山丹霞地貌地质成因分析及景观保护[J].火山地质与矿产,2001,22(2):143-149.[PENG Huaming, LIU Linqing, GUO Fusheng.On geological genesis of the Danxia landform in Zhejiang province[J].Volcanology Mineral Resources,2001,22(2):143-149]
[5] 吕文,朱诚,彭华,等.浙江江山市江郎山岩石岩性特征及其对丹霞地貌形成的影响[J].矿物岩石地球化学通报,2009,28(4):349-355.[LYU Wen, ZHU Cheng, PENG Hua, et al.The contribution of lithological characteristics to Danxia landform genesis in Jianglang mountain, Zhejiang province [J].Bulletin of Mineralogy, Petrology and Geochemistry,2009,28(4):349-355]
[6] 张广胜,朱诚,俞锦标,等.浙江江郎山丹霞地貌区岩性特征[J].山地学报,2010,28(3):301-312.[ZHANG Guangsheng, ZHU Cheng, YU Jinbiao, et al.Experimental study on lithological characteristic with Danxia landform, Jianglang mountain, Zhejiang province[J].Mountain Research,2010,28(3):301-312]
[7] 陈姝,朱诚,彭华,等.广东丹霞山洞穴景观岩体稳定性的抗压实验研究[J].安徽师范大学学报(自然科学版),2010,33(2):170-174.[CHEN Shu, ZHU Cheng, PENG Hua, et al.Anti-pressure experimental study on rocks in level cave of Jinshiyan of Danxiashan in Guangdong province[J].Journal of Anhui Normal University(Natural Science), 2010,33(2):170-174]
[8] 欧阳杰,朱诚,彭华,等.湖南崀山丹霞地貌岩体抗酸侵蚀脆弱性的实验研究[J].地球科学进展,2011,26(9):965-970.[OU Yangjie, ZHU Cheng, PENG Hua, et al.Experimental research on vulnerability of Danxia rocks to resistance against acid erosion in Langshan, Hunan province[J].Advances in Earth Science,2011, 26(9):965-970]
[9] 郭福生,朱志军,黄宝华,等.江西信江盆地白垩系沉积体系及其与丹霞地貌的关系[J].沉积学报,2013,31(6):954-964.[GUO Fusheng, ZHU Zhijun, HUANG Baohua, et al.Cretaceous sedimentary system and their relationship with Danxia Landform in Xinjiang basin, Jiangxi[J].Acta Sedimentologica Sinica,2013,31(6):954-964]
[10] 朱志军,黄宝华,郭福生,等.江西龙虎山世界地质公园白垩系辫状河相沉积及其丹霞地貌发育特征[J].地球学报,2012,33(3):379-387.[ZHU Zhijun, HUANG Baohua, GUO Fusheng, et al.Cretaceous braided river facies sediments and Danxia landform development characteristics in Longhushan world geopark, Jiangxi [J].Acta Geoscientica Sinica,2012,33(3):379-387]
[11] 黄进,陈致均,齐德利.中国丹霞地貌分布(下)[J].山地学报,2015,33(6):649-673.[HUANG Jin, CHEN Zhijun, QI Deli.Distribution of Danxia landform in China(Last)[J].Mountain Research,2015,33(6):649-673]
[12] 张荷生,崔振卿.甘肃省张掖丹霞与彩色丘陵地貌的形成与景观特征[J].中国沙漠,2007,27(6):942-945,1095.[ZHANG Hesheng, CUI Zhenqing.Landscape character and forming of Danxia Landform and color hill in Zhangye of Gansu Province[J].Journal of Desert Research,2007,27(6):942-945,1095]
[13] 田毓仁,刘成东,严兆彬,等.浙江省江山市江郎山地质遗迹资源特征及成景机制探讨[J].地球学报,2010,31(4):585-592.[TIAN Yuren, LIU Chengdong, YAN Zhaobin, et al.Characteristics and genetic mechanism of Jianglang mountain geological heritage resources in Jiangshan City, Zhejiang Province[J].Acta Geoscientica Sinica,2010,31(4):585-592]
[14] 高善坤,竺国强,董传万,等.丹霞地貌的坡地形态演化-以浙江新昌丹霞地貌为例[J].热带地理,2004,24(2):131-135.[GAO Shankun, ZHU Guoqiang, DONG Chuanwan, et al.The morphological development of Danxia hill slope: a case study of Xinchang Danxia landform[J].Tropical Geography,2004,24(2):131-135]
[15] 杨洪玉,杨艳华,白光顺.云南黎明高山丹霞地貌成因及其演化模式[J].云南地质,2011,30(3):370-372.[YANG Hongyu, YANG Yanhua, BAI Guangshun.The genesis and evolution model of high MT Danxia Geomorphology in liming,Yunnan[J].Yunnan Geology,2011,30(3):370-372]
[16] 郭福生,姜勇彪,胡中华,等.龙虎山世界地质公园丹霞地貌成景系统特征及其演化[J].山地学报,2011,29(2):195-201.[GUO Fusheng, JIANG Yongbiao, HU Zhonghua, et al.Evolution and genesis system features of Danxia landform in Longhushan world geopark[J].Mountain Research,2011,29(2):195-201]
[17] 姜勇彪,郭福生,刘林清,等.江西信江盆地丹霞地貌形成机制分析[J].热带地理,2011,31(2):146-152.[JIANG Yongbiao, GUO Fusheng, LIU Linqing, et al.A study on genesis of Danxia landforms in the Xinjiang Basin, Jiangxi [J].Tropical Geography,2011,31(2):146-152]
[18] 姜勇彪,郭福生,胡中华,等.龙虎山世界地质公园丹霞地貌特征及与国内其他丹霞地貌的对比[J].山地学报,2009,27(3):353-360.[JIANG Yongbiao, GUO Fusheng, HU Zhonghua, et al.Mountain Research,2009,27(3):353-360]
[19] 郭国林,郭福生,刘晓东,等.丹霞地貌砂岩的微观化学风化作用电子探针研究[J].中国岩溶,2006,25(2):172-176.[GUO Guolin, GUO Fuheng, LIU Xiaodong, et al.Study by EPMA on microcosmic chemical weathering to sandstone in Danxia landform[J].Carsologica Sinica,2006,25(2):172-176]
[20] 姜伏伟,郭福生,姜勇彪,等.龙虎山丹霞地貌危岩景观成因及保护[J].山地学报,2011,29(2):202-209.[JIANG Fuwei, GUO Fusheng, JIANG Yongbiao, et al.Causes of formation and protection for Landscape-rock fall of Danxia landform in Longhushan[J].Mountain Research,2011,29(2):202-209]
[21] 彭华.中国丹霞地貌研究进展[J].地理科学,2000,20(3):203-211.[PENG Hua.A Survey of the Danxia Land form Research in China[J].Scientia Geographica Sinica,2000,20(3):203-211]
[22] 姜勇彪,郭福生,孙传敏,等.江西弋阳县龟峰丹霞地貌景观特征与形成机制[J].山地学报,2008,26(1):124-130.[JIANG Yongbiao, GUO Fusheng, SUN Chuanmin, et al.The Features and Origin of the Danxia Landform in Guifeng Scenic Park in Yiyang County, Jiangxi[J].Mountain Research,2008,26(1):124-130]
[23] 朱诚,彭华,李世成,等.安徽齐云山丹霞地貌成因[J].地理学报,2005,60(3):445-455.[ZHU Cheng, PENG Hua, LI Shicheng, et al.Danxia Landform Genesis on Qiyun Mountain, Anhui Province[J].Acta Geographica Sinica,2005,60(3):445-455]

相似文献/References:

[1]姜勇彪,郭福生,陈珊珊,等.江西信江盆地丹霞地貌空间分布及其成因[J].山地学报,2013,(06):731.
　JIANG Yongbiao,GUO Fusheng,CHEN Shanshan.Spatial Distribution and Its Genesis of the Danxia Landforms in Xinjiang Basin, Jiangxi[J].Mountain Research,2013,(04):731.
[2]郭福生,姜伏伟,胡中华,等.丹霞地貌危岩景观分类及可持续开发对策——以龙虎山景区为例[J].山地学报,2012,(01):99.
　GUO Fusheng,JIANG Fuwei,HU Zhonghua,et al.Danxia Landscape Rockfalllandscape Types and Protection Measures—— A Case Study of Mt. Longhushan in Jiangxi, China[J].Mountain Research,2012,(04):99.
[3]郭福生,姜勇彪,胡中华,等.龙虎山世界地质公园丹霞地貌成景系统特征及其演化[J].山地学报,2011,(02):195.
　GUO Fusheng,JIANG Yongbiao,HU Zhonghua,et al.Evolution and Genesis System Features of Danxia Lanform in Longhushan World Geopark[J].Mountain Research,2011,(04):195.
[4]周学军.中国丹霞地貌的南北差异及其旅游价值[J].山地学报,2003,(02):180.
[5]姜勇彪,郭福生,孙传敏,等.江西弋阳县龟峰丹霞地貌景观特征与形成机制[J].山地学报,2008,(01):120.
[6]姜勇彪,郭福生,胡中华,等.龙虎山世界地质公园丹霞地貌特征及与国内其他丹霞地貌的对比[J].山地学报,2009,(03):353.
[7]张广胜,朱诚,俞锦标,等.浙江江郎山丹霞地貌区岩性特征[J].山地学报,2010,(03):301.
[8]黄宝华,郭福生,姜勇彪,等.广丰盆地丹霞地貌遥感影像特征[J].山地学报,2010,(04):500.
[9]姜勇彪,郭福生,胡中华,等.信江盆地丹霞地貌特征及其景观类型[J].山地学报,2010,(04):505.
[10]嘉益.封面照片:丹霞山[J].山地学报,2015,(03):293.

备注/Memo

备注/Memo:
收稿日期(Received date):2017-06-27; 改回日期(Accepted date):2018-01-17
基金项目(Foundation item):国家自然科学基金项目(No.41772197)。[National Nature Science Foundation of China(No.41772197).]
作者简介(Biography):姜伏伟(1987-),男,江西抚州人,博士,研究方向为丹霞地貌成因。[JIANG Fuwei,(1987-), male, born in Fuzhou, Jiangxi province, Ph.D., research on Danxia Landform.]E-mail: jfwei_666@126.com.
*通讯作者(Corresponding author):郭福生(1962-), 男,博士,教授,研究方向为区域地质与地貌景观。[GUO Fusheng,(1962-), male, Ph.D., professor, research on regional geology and geomorphologic landscape.]E-mail:fshguo@ecit.cn.
更新日期/Last Update: 2018-07-30