帮助 关于我们

返回检索结果

基于RTK - GPS技术的干热河谷冲沟沟头形态特征
Morphological Characteristics of the Gully Head in Dry-hot Valley Based on the RTK - GPS Technology

查看参考文献31篇

李佳佳 1   熊东红 1 *   卢晓宁 2   董一帆 1   苏正安 1   翟娟 1   杨丹 1  
文摘 采用高精度实时动态差分GPS(以下简称RTK-GPS)技术对干热河谷冲沟进行野外调查,获取36个不同活跃度类型沟头的形态参数,研究不同活跃度类型之间沟头的形态特征差异,并分析集水区、沟床植被盖度与形态特征之间的关系。结果表明:1.沟头不同活跃度类型之间,其跌坎高差、沟床比降差异最为显著,可作为沟头活跃度类型野外判别的主要参考指标;沟壁坡度、宽-深比等的差异较为显著,亦可在一定程度上表征沟头活跃程度。2.沟床植被盖度与各形态特征参数的相关性显著,表明沟床植被盖度可作为形态参数的综合替代性指标。同一活跃度类型的沟头,其跌坎高差、沟床比降等与沟床植被盖度呈极显著负相关关系,说明随着沟床植被盖度的增加(或减小),跌坎高差、沟床比降均呈减小(或增加)趋势。3.集水区植被盖度与各形态特征参数的关系不显著,表明干热河谷集水区植被盖度对沟头发育的贡献有限。
其他语种文摘 The Dry-hot Valley of Jinsha River has lots of gullies,and it suffers serious soil erosion. To carry out the study of gully head,especially its morphological characteristics,is the premise and foundation of further study on gully erosion. In this paper, the high precision real-time kinematical GPS (RTK - GPS) was used to measure the gully morphology in Yuanmou Dry-hot Valley, and the morphological parameters of 36 gully heads were obtained. Furthermore, this paper discussed the morphological characteristic differences of different type of active gully head, and analyzed the relationship between the vegetation coverage of catchments area & gully bed and morphological characteristics separately. The results showed that: (1) Among different active gully head types,both its backward step difference and gully bed slope difference are most significant,they could be regarded as the main index of distinguishing gully head activity type; the difference of furrow bank slope and the difference of width-depth ratio are more significant, they could also attribute the gully head activity to some extent. (2)There was a strong correlation between the gully bed vegetation coverage and the morphological parameters, indicating that the gully bed vegetation coverage could serve as the alternative indicator of morphological parameters. Among gully heads that were in the same activity type, its backward step and gully bed slope had a significant negative correlation with the gully bed vegetation coverage, indicating that when the gully bed vegetation coverage increase (or decrease),the backward step and gully bed slope values showed a decrease (or increase) trend. (3) The correlation between catchments vegetation coverage and morphological parameters was not significant, indicating that catchments vegetation coverage made a limited contribution to the development of gully head.
来源 山地学报 ,2014,32(6):706-716 【核心库】
关键词 冲沟形态特征 ; 沟头活跃度 ; 植被盖度 ; RTK-GPS技术
地址

1. 中国科学院水利部成都山地灾害与环境研究所, 中国科学院山地灾害与地表过程重点实验室, 四川, 成都, 610041  

2. 成都信息工程学院资源环境学院, 四川, 成都, 610225

语种 中文
文献类型 研究性论文
ISSN 1008-2786
学科 农业基础科学
基金 中国科学院知识创新工程重要方向项目 ;  中国科学院“百人计划”项目 ;  国家自然科学基金
文献收藏号 CSCD:5382699

参考文献 共 31 共2页

1.  钟祥浩. 干热河谷区生态系统退化及恢复与重建途径. 长江流域资源与环境,2000,9(3):376-383 被引 51    
2.  张建平. 元谋干热河谷区生态环境变迁探讨. 地理科学,2000,20(2):148-152 被引 27    
3.  张荣祖. 横断山区干旱河谷,1992 被引 73    
4.  Poesen J. Gully erosion and environmental change: importance and research needs. Catena,2003,50:91-133 被引 124    
5.  Valentin C. Gully erosion: Impacts, factors and control. Catena,2005,63:132-153 被引 69    
6.  王小丹. 金沙江干热河谷元谋盆地冲沟沟头形态学特征研究. 地理科学,2005,25(1):63-67 被引 23    
7.  Vandekerckhove L. Thresholds for gully initiation and sedimentation in Mediterranean Europe. Earth Surface Processes and Landforms,2000,25:1201-1220 被引 16    
8.  Patton P C. Gully erosion, Northwestern Colorado: a threshold phenomenon. Geology,1975(3):88-90 被引 1    
9.  Vandaele K. Geomorphic threshold conditions for ephemeral gully incision. Geomorphology,1996,16(2):161-173 被引 24    
10.  Montgomery D R. Landscape dissection and drainage area-slope thresholds. Process Models and Theoretical Geomorphology,1994:221-246 被引 4    
11.  Morgan R P C. Threshold conditions for initiation of valley-side gullies in the Middle Veld of Swaziland. Catena,2003,50:401-414 被引 10    
12.  Vandekerckhove L. Topographical thresholds for ephemeral gully initiation in intensively cultivated areas of the Mediterranean. Catena,1998,33:271-292 被引 11    
13.  Bocco G. Gully erosion: processes and models. Progress in Physical Geography,1991,15(4):392-406 被引 7    
14.  Thompson J R. Quantitative effect of watershed variables on rate of gully head advancement. Transactions of the ASAE,1964(7):54-55 被引 1    
15.  Williams A R. Geomorphologic mapping applied to erosion evaluation. Journal of Soil and Wa-ter Conservation,1976,31:164-168 被引 3    
16.  Stocking M A. Examination of the factors controlling gully growth. Assessment of Erosion,1980:505-520 被引 3    
17.  Donker N H W. Gully system development and assessment of gully initiation risk in Miocene deposits near Daroca-Spain. Zeitschrift fur Geomorphologie, N. F., Supplement-band,1984,49:37-50 被引 4    
18.  Wu Yongqiu. Monitoring of gully erosion on the Loess Plateau of China using a global positioning system. Catena,2005,63:154-166 被引 25    
19.  胡刚. GPS和GIS进行短期沟蚀研究初探--以东北漫川漫岗黑土区为例. 水土保持学报,2004,18(4):16-19 被引 43    
20.  游智敏. 利用GPS进行切沟侵蚀监测研究. 水土保持学报,2004,18(5):91-94 被引 30    
引证文献 9

1 张素 干热河谷不同活跃程度冲沟沟床土体抗冲性差异 水土保持学报,2015,29(3):13-17
被引 5

2 张素 冲沟不同部位土壤机械组成及抗冲性差异 土壤,2016,48(6):1270-1276
被引 11

显示所有9篇文献

论文科学数据集
PlumX Metrics
相关文献

 作者相关
 关键词相关
 参考文献相关

版权所有 ©2008 中国科学院文献情报中心 制作维护:中国科学院文献情报中心
地址:北京中关村北四环西路33号 邮政编码:100190 联系电话:(010)82627496 E-mail:cscd@mail.las.ac.cn 京ICP备05002861号-4 | 京公网安备11010802043238号