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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第46卷

期数:

2024年第02期

页码:

154-168

栏目:

环境与可持续发展

出版日期:

2024-04-10

文章信息/Info

Title:

Geomorphic Development Characteristics andEvolution Process in Luo River Basin, Loess Plateau, China

文章编号:

1672-6561(2024)02-0154-15

作者:

张天宇¹; 2; 3; 刘 凡²; 3; 洪增林¹; 3; 邓亚虹²; 3

(1. 陕西省地质调查院,陕西 西安 710068; 2. 长安大学 地质工程与测绘学院,陕西 西安 710054; 3. 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)

Author(s):

ZHANG Tian-yu¹; 2; 3;  LIU Fan²; 3;  HONG Zeng-lin¹; 3;  DENG Ya-hong²; 3

(1. Shaanxi Institute of Geological Survey, Xi'an 710068, Shaanxi, China; 2. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 3. Key Laboratory of Mine Geological Hazards Mechanism and Control of Ministry of Natural Resources, Xi'an 710054, Shaanxi, China)

关键词:

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

Keywords:

loess landform;  geomorphic differentiation;  geomorphic evolution;  geomorphic pattern;  quantitative analysis;  geomorphic factor;  principal component analysis;  Luo River Basin

分类号:

P931.6

DOI:

10.19814/j.jese.2023.11006

文献标志码:

A

摘要:

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。

Abstract:

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 mainfactors 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 headwarderoded and expanded downward with water system developed from downstream to upstream, and finally formed the present morphologicalspatialdifferentiation pattern.

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收稿日期:2023-11-07; 修回日期:2024-01-21
基金项目:国家自然科学基金项目(42201011); 陕西省公益性地质调查项目(202101)
作者简介:张天宇(1987-),男,山东滨州人,陕西省地质调查院工程师,工学博士,博士后,E-mail:1538861175@163.com。

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更新日期/Last Update: 2024-04-10