首页|黄土高原洛河流域地貌发育特征与形成演化

黄土高原洛河流域地貌发育特征与形成演化

扫码查看
黄土地貌形态特征、发育机理及演化过程等一直是地学研究的热点和前沿.选取黄土高原洛河流域作为研究对象,从坡面尺度、流域尺度、区域尺度分类选取 14 项地貌因子,较为全面地构建了流域地貌发育形态定量参数体系;提取 646 个小流域为分析单元,利用主成分分析法,获得了描述流域黄土地貌形态特征的 4 个主因子;这 4 个主因子分别反映了 4 种地貌形态空间格局,即南北渐变型、单中心扩散型、东西过渡型、多中心扩散型.结合流域地貌类型和地貌发育程度特征,认为黄土地貌地形起伏和垂直侵蚀特征反映了研究区的总体地貌空间格局,洛河流域黄土地貌主要是在多种因素影响下,随着水系由下游向上游不断地溯源侵蚀、下切扩展,最终形成了现今形态空间分异格局.
Geomorphic Development Characteristics and Evolution Process in Luo River Basin,Loess Plateau,China
The morphological characteristics,developmental mechanism and evolutionary process of loess landform always have been the focus and frontier of geoscience research.14 geomorphic factors were selected from slope scale,basin scale and regional scale to construct a comprehensive quantitative parameter system for characterizing the landform development in Luo River Basin,and the factor values and interpolation maps were obtained from 646 small watershed units.Through principal component analysis(PCA),four main factors were obtained,and reflected four spatial patterns of geomorphic morphological,including south-north gradient type,single-center diffusion type,east-west transitional type,and multi-center diffusion type.Combined with geomorphic types and development degree,it is indicated that the characteristics of loess geomorphic relief and vertical erosion reflect the overall geomorphic spatial pattern in Luo River Basin.Under multi-factor influence,the loess geomorphology of Luo River Basin has been continuously headward eroded and expanded downward with water system developed from downstream to upstream,and finally formed the present morphological spatial differentiation pattern.

loess landformgeomorphic differentiationgeomorphic evolutiongeomorphic patternquantitative analysisgeomorphic factorprincipal component analysisLuo River Basin

张天宇、刘凡、洪增林、邓亚虹

展开 >

陕西省地质调查院,陕西 西安 710068

长安大学 地质工程与测绘学院,陕西 西安 710054

自然资源部矿山地质灾害成灾机理与防控重点实验室,陕西 西安 710054

黄土地貌 地貌分异 地貌演化 地貌格局 定量分析 地貌因子 主成分分析 洛河流域

国家自然科学基金陕西省公益性地质调查项目

42201011202101

2024

地球科学与环境学报
长安大学

地球科学与环境学报

CSTPCD北大核心
影响因子:1.422
ISSN:1672-6561
年,卷(期):2024.46(2)
  • 63