干旱区生态环境知识资源中心(Arid): 基于高分辨率地形数据的冲洪积扇特征提取与演化模式讨论以海原断裂带老虎山地区冲洪积扇为例

Arid

	基于高分辨率地形数据的冲洪积扇特征提取与演化模式讨论以海原断裂带老虎山地区冲洪积扇为例
其他题名	EXTRACTING FEATURES OF ALLUVIAL FAN AND DISCUSSING LANDFORMS EVOLUTION BASED ON HIGH-RESOLUTION TOPOGRAPHY DATA: TAKING ALLUVIAL FAN OF LAOHUSHAN ALONG HAIYUAN FAULT ZONE AS AN INSTANCE
	韩龙飞; 刘静; 袁兆德; 邵延秀; 王伟; 姚文倩; 王鹏; 梁欧博; 徐心悦
来源期刊	地震地质
ISSN	0253-4967
出版年	2019
卷号	41 期号:2 页码:251-265
中文摘要	干旱半干旱地区第四纪冲洪积扇蕴含着丰富的气候与构造信息,划分并描述不同时期的冲洪积扇单元及其地貌特征是开展第四纪冲洪积扇研究的重要步骤。野外考察等传统方法是对冲洪积扇进行描述与填图的最重要的途径之一,但在此之前对冲洪积扇进行大范围的自动化地貌初步分级则可为地貌填图提供指导,从而提高后续的野外工作效率。文中借助航空影像生成的0.2m分辨率数字高程模型提取老虎山地区各冲洪积扇单元的起伏度与粗糙度,实现对各冲洪积扇单元的分类与差异探讨。研究表明,随着提取窗口尺寸的增大,粗糙度迅速增大,而当提取窗口增大到一定程度后粗糙度过渡为缓慢增大并达到稳定的状态。在尺寸为8m*8m的滑动取样窗口下,起伏度与粗糙度随着冲洪积扇年龄的增加,呈现先减小而后增大的趋势,这恰好反映了冲洪积扇的动态演化过程。
英文摘要	Range-front alluvial fan deposition in arid and semiarid environments records vast amounts of climatic and tectonic information. Differentiating and characterizing alluvial fan morphology is an important part in Quaternary alluvial fan research. Traditional method such as field observations is a most important part of deciphering and mapping the alluvial fan. Large-scale automatically mapping of alluvial fan stratigraphy before traditional field observations could provide guidance for mapping alluvial fan morphology,thus improving subsequent field work efficiency. In this research,highresolution topographic data were used to quantify relief and roughness of alluvial fan within the Laohushan. These data suggest that mean surface roughness plotted against the size of the moving window is characterized by an initial increase in surface roughness with increased window size,but it shows no longer increase as a function of windows size. These data also suggest that alluvial fans in this study site smooth out with time until a threshold is crossed where roughness increases at greater wavelength with age as a result of surface runoff and headward tributary incision into the oldest surfaces which suggests the evolution process of alluvial fan. Researchers usually differentiate alluvial morphology by mapping characteristics of fan surface in the field by describing surface clast size, rock varnish accumulation, and desert pavement development and analysis of aerial photographs or satellite imagery. Recently,the emergence of high-resolution topographic data has renewed interest in the quantitative characterization of alluvial and colluvium landforms. Surface morphology that fan surface initially tends to become smoother with increasing age due to the formation of desert pavement and the degradation of bar-and-swale topography and subsequently,landforms become more dissected due to tectonics and climatic change induced increased erosion and channelization of the surface with time is widely used to distinguish alluvial fan types. Those characteristics would reflect various kinds of morphology metrics extracted from high-resolution topographic data. In the arid and semiarid regions of northwestern China,plenty of alluvial fans are preserved completely for lack of artificial reforming,and there exists sparse surface vegetation. In the meantime,range-front alluvial fan displaced by a number of active faults formed a series of dislocated landforms with different offsets which is a major reference mark in fault activity research. In this research,six map units( Qf6Qf1 ),youngest to oldest,were observed in the study area by mapping performed by identifying geomorphic features in the field that are spatially discernible using hill-shade and digital orthophoto map. Alluvial fan relief and roughness were computed across multiple observation scales( 2m2m to 100m100m) based on the topographic parameters of altitude difference and standard deviation of slope,curvature and aspect. In this research,mean relief keeps increasing with increased window size while mean surface roughness is characterized by a rapid increase over wavelengths of 6 ~ 15m,representing the typical length scale of bar-and-swale topography. At longer wavelengths,surface roughness values increase by only minor amounts,suggesting the topographic saturation length is 6 ~ 15m for those fan surfaces in which saturation length of standard deviation of curvature is less than 8m.
中文关键词	冲洪积扇 ; 高精度地形数据 ; 起伏度 ; 粗糙度 ; 自动划分 ; 地貌演化
英文关键词	alluvial-proluvial fan high-resolution terrain data relief roughness automatic division,landform evolution
类型	Article
语种	中文
国家	中国
收录类别	CSCD
WOS类目	Geology
WOS研究方向	Geology
CSCD记录号	CSCD:6488667
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/239034
作者单位	韩龙飞, 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029, 中国.; 刘静, 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029, 中国.; 袁兆德, 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029, 中国.; 王伟, 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029, 中国.; 姚文倩, 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029, 中国.; 王鹏, 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029, 中国.; 徐心悦, 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029, 中国.; 邵延秀, 中国地震局兰州地震研究所, 兰州, 甘肃 730000, 中国.; 梁欧博, 中国地震局地壳应力研究所, 北京 100085, 中国.
推荐引用方式 GB/T 7714	韩龙飞,刘静,袁兆德,等. 基于高分辨率地形数据的冲洪积扇特征提取与演化模式讨论以海原断裂带老虎山地区冲洪积扇为例[J],2019,41(2):251-265.
APA	韩龙飞.,刘静.,袁兆德.,邵延秀.,王伟.,...&徐心悦.(2019).基于高分辨率地形数据的冲洪积扇特征提取与演化模式讨论以海原断裂带老虎山地区冲洪积扇为例.地震地质,41(2),251-265.
MLA	韩龙飞,et al."基于高分辨率地形数据的冲洪积扇特征提取与演化模式讨论以海原断裂带老虎山地区冲洪积扇为例".地震地质 41.2(2019):251-265.