现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2014年
2期
443-448
,共6页
邱海军%曹明明%刘闻%郝俊卿%胡胜%高宇%刘琪
邱海軍%曹明明%劉聞%郝俊卿%鬍勝%高宇%劉琪
구해군%조명명%류문%학준경%호성%고우%류기
滑坡%变维分形%空间分布%陕西宁强
滑坡%變維分形%空間分佈%陝西寧彊
활파%변유분형%공간분포%협서저강
landslide%variable fractal%spatial distribution%Ningqiang,Shaanxi
定量研究滑坡的空间分布特征对研究滑坡灾害的孕育发展具有重要意义。以陕西省宁强县滑坡为例,采用变维分形方法,探讨滑坡在空间分布上的变维分形特征。结果表明:区域滑坡与不同影响因子,即高程、起伏度、坡度、距河流距离、距断裂带距离和地层岩性之间全部呈一阶累积和变维分形分布特征,且分形维数分别是0.5111、1.1357、1.2906、0.9038、1.1895、0.9799。由此可见滑坡对于不同影响因子的敏感度由高到低分别是坡度>距断裂带距离>起伏度>地层岩性>距河流距离>高程。上述研究表明用变维分形理论来研究滑坡的空间分布特征是完全可行的,它能够定量地反映滑坡的空间分布与各影响因素之间的敏感性关系,特别是对于GIS空间叠加分析时权重的确定有着重要的意义。
定量研究滑坡的空間分佈特徵對研究滑坡災害的孕育髮展具有重要意義。以陝西省寧彊縣滑坡為例,採用變維分形方法,探討滑坡在空間分佈上的變維分形特徵。結果錶明:區域滑坡與不同影響因子,即高程、起伏度、坡度、距河流距離、距斷裂帶距離和地層巖性之間全部呈一階纍積和變維分形分佈特徵,且分形維數分彆是0.5111、1.1357、1.2906、0.9038、1.1895、0.9799。由此可見滑坡對于不同影響因子的敏感度由高到低分彆是坡度>距斷裂帶距離>起伏度>地層巖性>距河流距離>高程。上述研究錶明用變維分形理論來研究滑坡的空間分佈特徵是完全可行的,它能夠定量地反映滑坡的空間分佈與各影響因素之間的敏感性關繫,特彆是對于GIS空間疊加分析時權重的確定有著重要的意義。
정량연구활파적공간분포특정대연구활파재해적잉육발전구유중요의의。이합서성저강현활파위례,채용변유분형방법,탐토활파재공간분포상적변유분형특정。결과표명:구역활파여불동영향인자,즉고정、기복도、파도、거하류거리、거단렬대거리화지층암성지간전부정일계루적화변유분형분포특정,차분형유수분별시0.5111、1.1357、1.2906、0.9038、1.1895、0.9799。유차가견활파대우불동영향인자적민감도유고도저분별시파도>거단렬대거리>기복도>지층암성>거하류거리>고정。상술연구표명용변유분형이론래연구활파적공간분포특정시완전가행적,타능구정량지반영활파적공간분포여각영향인소지간적민감성관계,특별시대우GIS공간첩가분석시권중적학정유착중요적의의。
Quantitative research on characteristics of spatial distribution of landslide is important for analysis of inoculation and development of landslide.Because the fractal can reveal the fine structure hidden in the com-plex and chaotic phenomena,and it is gradually applied to the study of landslide.Taking the landslide of Ningqiang,Shaanxi as an example,this research discussed the fractal structure characteristics of single-land-slide and large-area landslide systems,and the calculation of fractal dimension and variable fractal dimension. The results show that the relationship between the landslide and the influence factor,i.e.elevation,landform amplitude,slope,distances from river and fault,and lithology fits the first-order accumulated variable dimen-sion fractal distribution,and the fractal dimension is 0.511,1,1.135,7,1.290,6,0.903,8,1.189,5 and 0.979,9,respectively.Thus the sensitivity of these influence factors to landslide is in the descending order as slope>distance from fault>landform amplitude>lithology>distance from river>elevation.This research in-dicates that the variable dimension fractal theory is completely feasible to study the spatial distribution charac-teristics of landslide,and it can quantitatively reflect the spatial distribution of landslide and the sensitivity of the influence factor to landslide;it is especially important for the GIS spatial overlay analysis to determine the weight.