WANG Geng, LI Sujuan, ZHANG Xingguo. Classification of Geomorphic Forms of Huaihe River Source Based on DEM[J]. Bulletin of Soiland Water Conservation, 2018, 38(2): 292-296.
DOI:
WANG Geng, LI Sujuan, ZHANG Xingguo. Classification of Geomorphic Forms of Huaihe River Source Based on DEM[J]. Bulletin of Soiland Water Conservation, 2018, 38(2): 292-296. DOI: 10.13961/j.cnki.stbctb.2018.02.048.
Classification of Geomorphic Forms of Huaihe River Source Based on DEM
[Objective] Studying on the classification of geomorphologic types in Huaihe River Source to provide reference for land use
tourism
urban planning and biodiversity conservation in this area.[Methods] Taking Huaihe River source as an object of study
adopting the representative landform classification scheme in the Chai Zongxin scheme
Xu Hanming scheme and Gao Xuanyu scheme
using neighborhood analysis
reclassification
map algebra
and conversion tools in spatial analysis
the geomorphologic types of Huaihe River source were classified under each scheme and compared with the actual survey terrain based on the DEM data with a resolution of 30 meters so as to find the most suitable scheme for the basic morphologic classification of the Huaihe River source landforms.[Results] The Chai Zongxin scheme is single factor and can not reflect the basic features of the geomorphology. Gao Xuanyu scheme did not proved its advantages fully in the two grade classification for the study area
as it is more suitable for the area with high elevation and complex landform. The Xu Hanming scheme is based on 2 conditions
both relative height and altitude
that is to say
objective effect and subjective feeling of height were considered for basic morphologic classification of the geomorphology. Therefore
the Xu Hanming scheme is more suitable for the division of geomorphology in Huaihe River Source.[Conclusion] According to the Xu Hanming scheme
the geomorphic form of Huaihe River Source region was divided into 4 types:plain
hilly
low mountain and middle and low mountain
it is mainly covered by plain and hill
is low in the east and the north part and high in the west and the south part.