[1]段宇英,汤 军,段宇雄.基于DEM的山西黄土高原面积高程积分研究[J].水土保持研究,2020,27(05):81-86.
 DUAN Yuying,TANG Jun,DUAN Yuxiong.Area Elevation Integral in Shanxi Section of Loess Plateau Based on DEM[J].Research of Soil and Water Conservation,2020,27(05):81-86.
点击复制

基于DEM的山西黄土高原面积高程积分研究

参考文献/References:

[1]胡胜.黄土高原滑坡空间格局及其对地貌演化的影响[D].西安:西北大学,2019.
[2]Chen Y C, Sung Q, Cheng K Y. Along-strike variations of morphotectonic features in the Western Foothills of Taiwan: tectonic implications based on stream-gradient and hypsometric analysis[J]. Geomorphology, 2003,56(1):109-137.
[3]Hamdouni R E, Irigaray C, Fernández, et al. Assessment of relative active tectonics, southwest border of the Sierra Nevada(southern Spain)[J]. Geomorphology, 2008,96(1/2):150-173.
[4]李玉辉,丁智强,吴晓月.基于Strahler面积—高程分析的云南石林县域喀斯特地貌演化的量化研究[J].地理学报,2018,73(5):973-985.
[5]章桂芳,陈凯伦,张浩然,等.基于DEM的丹霞地貌演化阶段划分[J].中山大学学报:自然科学版,2018,57(2):12-21.
[6]Lifton N A, Chase C G. Tectonic, climatic and lithologic influences on landscape fractal dimension and hypsometry, implications for landscape evolution in the San Gabriel Mountains, California[J]. Geomorphology,1992,5(1/2):77-114.
[7]张敬春,李川川,张梅,等.格尔木河流域面积—高程积分值的地貌学分析[J].山地学报,2011,29(3):257-268.
[8]Simon H. Brocklehurst, Kelin X. Whipple. Hypsometry of glaciated landscapes[J]. Earth Surface Processes and Landforms,2004,29(7):907-926.
[9]Ansan V, Mangold N. New observations of WarregoValles, Mars:Evidence for precipitation and surface runoff[J]. Planetary and Space Science, 2006,54(3):219-242.
[10]Harlin J M. Statistical moments of the hypsometric curve and its density function[J]. Mathematical Geology, 1978,10(1):59-72.
[11]Strahler A H. Hypsometric(area-altitude)analysis of erosional topography[J]. GSA Bulletin, 1952, 63(11):1117-1142.
[12]艾南山.侵蚀流域系统的信息熵[J].水土保持学报,1987,1(2):3-10.
[13]艾南山,岳天祥.再论流域系统的信息熵[J].水土保持学报,1988,2(4):3-11.
[14]励强,陆中臣,袁宝印.地貌发育阶段的定量研究[J]. ActaGeographica Sinica,1990,57(1):110-120.
[15]祝士杰, 汤国安, 李发源,等.基于DEM的黄土高原面积高程积分研究[J].地理学报,2013,68(7):921-932.
[16]吕萌.山西省黄土崩塌地质灾害的现状及水敏感性分析[D].太原:太原理工大学,2016.
[17]彭建,杨明德,梁虹.基于GIS的路南巴江喀斯特流域地貌演化定量研究[J].中国岩溶,2002,21(2):89-94.
[18]Luo W. Hypsometric analysis with a geographic information system[J]. Computers & Geosciences,1998,24(8):815-821.
[19]Meerkerk A L, Wesemael B V, Bellin N. Application of connectivity theory to model the impact of terrace failure on runoff in semi-arid catchments[J]. Hydrological Processes,2009,23(19):2792-2803.
[20]王林,何仲太,马保起.岱海流域地貌演化及其对断裂活动性的指示意义[J].第四纪研究,2008,28(2):310-318.
[21]李发源.黄土高原地面坡谱及空间分异研究[D].成都:中国科学院水利部成都山地灾害与环境研究所,2007.
[22]汤国安,李发源,熊礼阳.黄土高原数字地形分析研究进展[J].地理与地理信息科学,2017,33(4):1-7.
[23]熊礼阳.基于DEM的黄土地貌继承性研究[D].南京:南京师范大学,2015.

备注/Memo

收稿日期:2020-03-01修回日期:2020-03-13
资助项目:国家自然科学基金青年基金,顾及空间上下文关系的能量最小化地图多要素协同移位方法,41701537
第一作者:段宇英(1996—),女,山西临汾人,硕士研究生,研究方向为水土保持。E-mail:2889088991@qq.com
通信作者:汤军(1964—),男,陕西勉县人,博士,硕士生导师,研究方向为地理信息。E-mail:374216030@qq.com

更新日期/Last Update: 2020-08-25