Analysis of geomorphology of Niyang River Basin based on digital elevation model
SU Libin1, GUO Yonggang2, WU Yue2, YANG Yongtao2
1. Research Institute of Tibet Plateau Ecology, Tibet Agriculture & Animal Husbandry University, 860000, Linzhi, Tibet, China; 2. Water Conservancy Project & Civil Engineering College, Tibet Agriculture & Animal Husbandry University, 860000, Linzhi, Tibet, China
Abstract:[Background] As an important tributary of the Yarlung Zangbo River, the Niyang River plays an important role in the typical disaster occurrence area. In recent years, the first industry in the Niyang River Basin is developing rapidly. However, due to its special geomorphological features, geological disasters in the basin are frequent and have seriously affected the sustainable economic development of the region. The purpose of this study is to reveal the relationship between geological disasters and topography in the Niyang River Basin, and to classify the risks.[Methods] Taking the Niyang River Basin in Linzhi as an example, based on the digital elevation model(DEM) and other auxiliary data, the topographic factors such as slope direction, slope, terrain fluctuation and elevation were extracted, the GIS was used to produce the thematic maps.[Results] 1) In the Niyang River Basin, the east, southeast, northeast and northwest directions are the main slope directions; the steep slope area is the largest, accounting for 85.98%, followed by the steep cliff, accounting for 11.08% of the area, which is 3.8 times of the gentle slope area. The >25°-45°is a prone area for landslide disasters, the area in the basin accounts for 50.88%, areas with a slope <25℃an be used as cultivated land and is 6 624.19 km2, accounting for 38.03%. 2) The Niyang River Basin is divided into 4 categories according to the mountain elevation:low mountains, median mountains, high mountains and great high mountains. The elevation of the basin is mainly located at ≥ 4 000-6 000 m, accounting for 86.60% of the area, belonging to high mountains and great high mountains. According to the terrain fluctuation, the relative height is mainly in the range of ≥ 200-1 000 m, and the area is 17 103.54 km2, accounting for 95.75%, which belongs to the small and median undulating mountains. 3) Altitude, slope, terrain fluctuation, vegetation coverage, rainfall and other factors have a great impact on the occurrence of disasters. The areas of steep slopes with an altitude of ≥ 3 500-5 500 m, median undulating mountains, small vegetation coverage and heavy rainfall have a large potential risk, and the dangerous sources are distributed in the upper and lower reaches of the main stream and in the middle part of the tributary.[Conculsions] The occurrence of geological disasters is closely related to the regional topography. Altitude, slope, terrain fluctuation, vegetation coverage, rainfall and other factors have a great impact on the occurrence of disasters in the Niyang River Basin. This study may provide reference for further research on the causes and susceptibility of regional disasters, and provide a scientific basis for disaster prevention and mitigation.
苏立彬, 郭永刚, 吴悦, 杨永涛. 基于DEM的尼洋河流域地貌形态分析[J]. 中国水土保持科学, 2020, 18(3): 12-21.
SU Libin, GUO Yonggang, WU Yue, YANG Yongtao. Analysis of geomorphology of Niyang River Basin based on digital elevation model. SSWC, 2020, 18(3): 12-21.
郭芳芳,杨农,张岳桥,等. 基于GIS的滑坡地质灾害地貌因素分析[J]. 地质力学学报,2008,14(1):87. GUO Fangfang, YANG Nong, ZHANG Yueqiao, et al. GIS-based analysis of geomorphological factors for landslide hazards[J]. Journal of Geomechanics, 2008, 14(1):87.
[2]
谢吉尊,冯文凯,杨少帅,等. 则木河断裂带活动特征和地质灾害对地貌演化的影响:以鹅掌河流域为例[J]. 工程地质学报,2017,25(3):772. XIE Jizun, FENG Wenkai, YANG Shaoshuai, et al. Active characteristics and geohazard of Zemuhe fault and their influence on morphological evolution in Ezhang river[J]. Journal of Engineering Geology, 2017, 25(3):772.
[3]
苏琦,梁明剑,袁道阳,等.白龙江流域构造地貌特征及其对滑坡泥石流灾害的控制作用[J].地球科学,2016,41(10):1758. SU Qi, LIANG Mingjian, YUANG Daoyang, et al. Geomorphic features of the Bailongjiang River Drainage Basin and its relationship with geological disaster[J]. Earth Science, 2016, 41(10):1758.
[4]
唐川,马国超. 基于地貌单元的小区域地质灾害易发性分区方法研究[J]. 地理科学,2015,35(1):91. TANG Chuan, MA Guochao. Small regional geohazards susceptibility mapping based on geomorphic unit[J]. Scientia Geographica Sinica, 2015, 35(1):91.
[5]
孙建伟,汤国安. 域间流域及自动提取方法研究[J]. 地球信息科学学报,2013,15(6):871. SUN Jianwei, TANG Guoan. Inter-watershed and its automatic extraction based on DEMs[J]. Journal of Geo-Information Science, 2013, 15(6):871.
[6]
方磊,刘文兆,李怀有. 基于GIS的黄土高塬沟壑区砚瓦川流域地形特征提取与分析[J]. 水土保持研究,2010,17(3):7. FANG Lei, LIU Wenzhao, LI Huaiyou. Terrain feature extraction and analysis of the Yanwachuan basin in loess tableland-gully region based on GIS[J]. Research of Soil and Water Conservation, 2010,17(3):7.
[7]
古格·其美多吉,索朗仁青,次仁,等.尼洋河流域主要地质灾害及其对策[J].山地学报,2010,28(5):607. Guge·Qimei duoji, Sonam renqing, Tsering, et al. Research on the main geologic disaster of Niyang River and countermeasures[J].Journal of Mountain Science,2010,28(5):607.
[8]
蒋芸芸,柯长青.基于遥感和GIS的尼洋河流域土地利用变化研究[J].云南师范大学学报(自然科学版),2007,27(4):63. JIANG Yunyun, KE Changqing. Research on land use change in Niyanghe watershed based on remote sensing and GIS[J].Journal of Yunnan Normal University(Natural Science Edition),2007,27(4):63.
[9]
李秀珍,钟卫,张小刚,等. 川藏交通廊道滑坡崩塌灾害对道路工程的危害方式分析[J]. 工程地质学报,2017,25(5):1245. LI Xiuzhen, ZHONG Wei, ZHANG Xiaogang, et al. Hazard ways of landslides and avalanches on road engineering in Sichuan-Tibet traffic corridor[J]. Journal of Engineering Geology, 2017,25(5):1245.
[10]
胡桂胜,陈宁生,邓虎. 基于GIS的西藏林芝地区泥石流易发与危险区分析[J]. 水土保持研究,2012,19(3):195. HU Guisheng, CHEN Ningsheng, DENG Hu. Analysis of debris flow-prone and dangerous area in Nyingchi of Tibet Based on GIS[J]. Research of Soil and Water Conservation, 2012, 19(3):195.
[11]
屈永平,唐川,刘洋,等. 西藏林芝地区冰川降雨型泥石流调查分析[J]. 岩石力学与工程学报,2015,34(S2):4013. QU Yongping, TANG Chuan, LIU Yang, et al. Investigation and analysis of glacier debris flow in Nyingchi area, Tibet[J]. Chinese Journal of Rock Mechanics and Engineering, 2015,34(S2):4013.
[12]
徐静, 任立良, 程媛华, 等. 不受DEM空间分辨率影响的地形指数计算. 清华大学学报(自然科学版), 2008, 48(6), 983. XU Jing,REN Liliang,CHENG Yuanhua,et al. Topographic index calculation that is independent of the DEM spatial resolution[J].Journal of Tsinghua University (Science and Technology), 2008, 48(6), 983.
[13]
郭兰勤,杨勤科,胡洁,等. 基于分形的中低分辨率坡度降尺度变换[J]. 西北农林科技大学学报(自然科学版), 2011.39(12):173. GUO Lanqin, YANG Qinke, HU Jie, et al. Research on method of re-scaling coarser resolution slope based on fractal analysis approach[J]. Journal of Northwest A&F University(Natural Science Edition), 2011.39(12):173.
[14]
王彦龙,王晓丽,马玉寿.坡向对长江源区高寒草地植被生长和土壤养分特征的影响[J].草业科学,2018,35(10):2336. WANG Yanlong, WANG Xiaoli, MA Yushou. Effect of slope aspect on vegetation growth and soil nutrient characteristics of alpine grassland in the source region of Yangtze River[J].Pratacultural Science, 2018, 35(10):2336.
[15]
何晓蓉,李辉霞,范建容,等.青藏高原流域廊道体系对生态环境的影响:以尼洋河流域为例[J].水土保持研究,2004,11(2):97. HE Xiaorong, LI Huixia, FAN Jianrong, et al. Influences of corridor system on eco-environment of basin in the Qinghai-Tibet Plateau:Take the Niyang River Basin for example[J].Research of Soil and Water Conservation,2004,11(2):97.
[16]
汤国安,宋佳. 基于DEM坡度图制图中坡度分级方法的比较研究[J]. 水土保持学报,2006,20(2):157. TANG Guoan,SONG Jia. Comparison of slope classification methods in slope mapping from DEMs[J]. Journal of Soil and Water Conservation, 2006,20(2):157.
[17]
郭果,陈筠,李明惠,等. 土质滑坡发育概率与坡度间关系研究[J].工程地质学报,2013,21(4):607. GUO Guo, CHEN Yun, LI Minghui, et al. Statistic relationship between slope gradient and landslide probability in soil slopes around reservoir[J].Journal of Engineering Geology, 2013,21(4):607.
[18]
中国科学院地理研究所. 中国1:100万地貌制图规范(征求意见稿)[M]. 北京:科学出版社,1987:4. Institute of Geography, Chinese Academy of Sciences. China 1:100 million landform mapping specifications (draft for comments)[M]. Beijing:Science Press, 1987:4.
[19]
许丽,李江海,刘持恒,等.基于数字高程模型(DEM)的可可西里地貌及区划研究[J].北京大学学报(自然科学版),2017,53(5):833. XU Li, LI Jianghai, LIU Chiheng, et al. Research on geomorphological morphology and regionalization of Hoh Xil based on digital elevation model (DEM)[J]. Acta Scientiarum Naturalium Universitatis Pekinnensis, 2017, 53(5):833.