Modeling the evolution of loess-covered landforms in the Loess Plateau of China using a DEM of underground bedrock surface
文献类型：期刊论文
| 作者 | Xiong, Li-Yang1; Tang, Guo-An1; Li, Fa-Yuan1; Yuan, Bao-Yin2; Lu, Zhong-Chen3 |
| 刊名 | GEOMORPHOLOGY
 |
| 出版日期 | 2014-03-15 |
| 卷号 | 209页码:18-26 |
| 关键词 | Underlying paleotopography Landscape evolution Loess thickness DEM |
| ISSN号 | 0169-555X |
| DOI | 10.1016/j.geomorph.2013.12.009 |
| 文献子类 | Article |
| 英文摘要 | The evolution of loess-covered landforms is largely controlled by the pre-Quaternary underlying bedrock terrain, which is one of the most important factors in understanding the formation mechanism of the landforms. This study used multiple data sources to detect 1729 outcropping points of underlying terrain, in order to construct a digital elevation model (DEM) of the paleotopography of an area of the Loess Plateau subject to severe soil erosion. Four terrain characteristics, including terrain texture, slope gradient the hypsometric curve, and slope aspect, were used to quantify topographic differences and reveal the loess-deposition process during the Quaternary. A loess thickness map was then created to show the spatial distribution of loess deposits in the test area. Finally, the geomorphological inheritance characteristics of the loess-covered landforms were evaluated in different landform divisions. The results showed the significant inheritance of modern topography from the underlying topography with a similar general relief trends. The average thickness of loess deposits was computed to be 104.6 m, with the thickest part located in the Xifeng loess tableland area. In addition, the slope aspects of the North and Northwest seem to have favored Quaternary loess deposition, which supported the hypothesis of an eolian origin for loess in China. The modem surface has lower topographic relief compared to the underlying terrain due to loess deposition. Crown Copyright (C) 2013 Published by Elsevier B.V. All rights reserved. |
| WOS关键词 | LANDSCAPE EVOLUTION ; SOIL-EROSION ; SEDIMENT ; WATER ; FLOW ; CATCHMENT ; AREA |
| WOS研究方向 | Physical Geography ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000332265000002 |
| 出版者 | ELSEVIER SCIENCE BV |
| 资助机构 | National Natural Science Foundation of China(40930531 ; National Natural Science Foundation of China(40930531 ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; National High Technology Research and Development Program of China(2011AA120303) ; National High Technology Research and Development Program of China(2011AA120303) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; 41171320) ; 41171320) ; National Natural Science Foundation of China(40930531 ; National Natural Science Foundation of China(40930531 ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; National High Technology Research and Development Program of China(2011AA120303) ; National High Technology Research and Development Program of China(2011AA120303) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; 41171320) ; 41171320) ; National Natural Science Foundation of China(40930531 ; National Natural Science Foundation of China(40930531 ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; National High Technology Research and Development Program of China(2011AA120303) ; National High Technology Research and Development Program of China(2011AA120303) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; 41171320) ; 41171320) ; National Natural Science Foundation of China(40930531 ; National Natural Science Foundation of China(40930531 ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; Open Foundation of State Key Laboratory of Resources and Environmental Information System(2010KF0002SA) ; National High Technology Research and Development Program of China(2011AA120303) ; National High Technology Research and Development Program of China(2011AA120303) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; Foundation of Graduate Innovation Plan of Jiangsu Province(CXZZ13_0401) ; 41171320) ; 41171320) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/86498]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Tang, Guo-An |
| 作者单位 | 1.Nanjing Normal Univ, Key Lab Virtual Geog Environm, Minist Educ, Nanjing 210023, Jiangsu, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Ecoenvironm Sci Res Ctr, Beijing 100085, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xiong, Li-Yang,Tang, Guo-An,Li, Fa-Yuan,et al. Modeling the evolution of loess-covered landforms in the Loess Plateau of China using a DEM of underground bedrock surface[J]. GEOMORPHOLOGY,2014,209:18-26. |
| APA | Xiong, Li-Yang,Tang, Guo-An,Li, Fa-Yuan,Yuan, Bao-Yin,&Lu, Zhong-Chen.(2014).Modeling the evolution of loess-covered landforms in the Loess Plateau of China using a DEM of underground bedrock surface.GEOMORPHOLOGY,209,18-26. |
| MLA | Xiong, Li-Yang,et al."Modeling the evolution of loess-covered landforms in the Loess Plateau of China using a DEM of underground bedrock surface".GEOMORPHOLOGY 209(2014):18-26. |
入库方式： OAI收割
来源：地质与地球物理研究所
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