[1]刘 欣,等.基于坡度—汇水面积关系的黄土浅沟与切沟沟头形成敏感区模拟[J].山地学报,2020,(5):658-667.[doi:10.16089/j.cnki.1008-2786.000543]
 LIU Xin,WANG Chunmei*,et al.Sensitive Area Simulation of Ephemeral and Permanent Gullies Based on Slope-Area Relationship in the Loess Region[J].Mountain Research,2020,(5):658-667.[doi:10.16089/j.cnki.1008-2786.000543]
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基于坡度—汇水面积关系的黄土浅沟与切沟沟头形成敏感区模拟
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2020年第5期
页码:
658-667
栏目:
山地环境
出版日期:
2020-11-10

文章信息/Info

Title:
Sensitive Area Simulation of Ephemeral and Permanent Gullies Based on Slope-Area Relationship in the Loess Region
文章编号:
1008-2786-(2020)5-658-10
作者:
刘 欣1 2王春梅1 2*庞国伟1 2龙永清1 2王 雷1 2
1.陕西省地表系统与环境承载力重点实验室,西安 710127; 2.西北大学 城市与环境学院,西安 710127
Author(s):
LIU Xin1 2 WANG Chunmei12* PANG Guowei1 2 LONG Yongqing12 WANG Lei1 2
1. Key Laboratory of Earth Surface System and Environmental Carrying Capacity of Shaanxi Province, Northwest University, Xi'an 710127, China; 2. College of Urban and Environmental Science, Northwest University, Xi'an 710127, China
关键词:
无人机 侵蚀沟 沟头 数字高程模型 黄土高原
Keywords:
UAV erosional gully gully head Digital Elevation Model(DEM) the Loess Plateau
分类号:
P91
DOI:
10.16089/j.cnki.1008-2786.000543
文献标志码:
A
摘要:
黄土高原侵蚀沟治理是黄河流域高质量发展中面临的重要问题。本研究以坡面侵蚀沟中的浅沟、切沟为研究对象,基于高分辨率无人机航摄和野外高精度实测,以陕北子洲岔巴沟典型小流域为研究区,得到沟头坡度—汇水面积关系曲线,构建了沟头形成的地形临界模型,进行沟头形成敏感区模拟。结果表明:(1)浅沟、切沟沟头形成临界模型分别为:S≥0.6073A-0.142,S≥1.2065A-0.229;(2)综合运用沟头形成临界模型和流域坡度—汇水面积关系曲线可较为准确地预测浅沟、切沟沟头形成敏感区与非敏感区,浅沟、切沟沟头预测准确度分别为91.43%和71.79%,非沟头区域预测准确度为98.44%。研究结果可为黄土侵蚀沟防治提供技术支撑。
Abstract:
Gully erosion is severe in the Loess Plateau of North China, where gully location modeling remains a challenge. The objective of this study was to explore the methodology for modeling ephemeral gullies(EGs)and permanent gullies(PGs)in gully-sensitive areas in a watershed located in Zizhou, Shaanxi Province. The critical topographic threshold model based on the slope-area relationship was employed as the primary method. High-resolution unmanned aerial vehicle(UAV)photography and high-precision field measures were utilized as data sources. The critical topographic models were S≥0.6073A-0.142 for EGs, and S≥1.2065A-0.229 for PGs. The gully head prediction accuracies for EGs and PGs were 91.43% and 71.79%, respectively, and the prediction accuracy for the non-gully head area was 98.44%. The results improve our understanding of the gully formation and may support gully erosion conservation in the loess region.

参考文献/References:

[1] 朱显谟.黄土高原的综合治理[J]. 土壤通报,1980,2(2):11-15. [ZHU Xianmo. Comprehensive management of Loess Plateau[J]. Chinese Journal of Soil Science, 1980, 2(2): 11-15]
[2] CASTILLO C, GMEZ J A. A century of gully erosion research: urgency, complexity and study approaches[J]. Earth-Science Reviews, 2016, 160: 300-319.
[3] POESEN J. Soil erosion in the Anthropocene: research needs[J]. Earth Surface Processes and Landforms, 2018, 43(1): 64-84.
[4] VANMAERCKE M, POESEN J, VAN M B, et al. How fast do gully headcuts retreat?[J]. Earth-Science Reviews, 2016, 154: 336-355.
[5] TAROLLI P, SOFIA G. Human topographic signatures and derived geomorphic processes across landscapes[J]. Geomorphology, 2016, 255: 140-161.
[6] 陈一先,焦菊英,魏艳红,等. 陕北黄土区退耕前(1976-1997)坡面切沟发育特征[J],农业工程学报,2017,33(17):120-127. [CHEN Yixian, JIAO Juying, WEI Yanhong, et al. Characteristics of gully development in Northern Shaanxi Hilly Loess Region before Grain-for-Green Programme(1976-1997)[J]. Transactions of the Chinese Society of Agricultural Engineering, 2017, 33(17): 120-127]
[7] 刘宝元,杨扬,陆绍娟. 几个常用土壤侵蚀术语辨析及其生产实践意义[J]. 中国水土保持科学,2018,16(1):9-16. [LIU Baoyuan, YANG Yang, LU Shaojuan. Discriminations on common soil erosion terms and their implications for soil and water conservation[J]. Science of Soil and Water Conservation, 2018, 16(1): 9-16.
[8] GUDINO-ELIZONDO N, BIGGS T, CASTILLO C, et al. Measuring ephemeral gully erosion rates and topographical thresholds in an urban watershed using unmanned aerial systems and structure from motion photogrammetric techniques[J]. Land Degradation and Development, 2018, 29: 1896-1905.
[9] PATTON P C, SCHUMM S A. Gully erosion, Northwestern Colorado: a threshold phenomenon[J]. Geology, 1975, 3(2): 88-90.
[10] BEGIN Z B, SCHUMM S A. Instability of alluvial valley floors: a method for its assessment[J]. Transactions of the ASAE, 1979, 22(2): 347-350.
[11] HAYAS A, POESEN J, VANWALLEGHEM T. Rainfall and vegetation effects on temporal variation of topographic thresholds for gully initiation in Mediterranean cropland and Olive groves[J]. Land Degradation and Development, 2017, 28(8): 2540-2552.
[12] TORRI D, POESEN J, ROSSI M, et al. Gully head modelling: A Mediterranean badland case study[J]. Earth Surface Processes and Landforms, 2018, 43(12): 2547-2561.
[13] HYDE K D, WILCOX A C, JENCSO K, et al. Effects of vegetation disturbance by fire on channel initiation thresholds[J]. Geomorphology, 2014, 214:84-96.
[14] GEETER S D, POESEN J, VANMAERCKE M. Does the topographic threshold concept explain the initiation points of sunken lanes in the European loess belt?[J]. Catena, 2020, 192:12.
[15] 胡刚,伍永秋,刘宝元,等. 东北漫川漫岗黑土区浅沟和切沟发生的地貌临界模型探讨[J]. 地理科学,2006,26(4):449-454. [HU Gang, WU Yongqiu, LIU Baoyuan, et al. Geomorphic threshold model for ephemeral gully incision in Rolling Hills with black soil in Northeast China[J]. Scientia Geographica Sinica, 2006, 26(4): 449-454]
[16] 李斌兵,郑粉莉,张鹏. 黄土高原丘陵沟壑区小流域浅沟和切沟侵蚀区的界定[J]. 水土保持通报,2008,28(5):16-20. [LI Binbing, ZHENG Fenli, ZHANG Peng. Geomorphic threshold determination for ephemeral gully and gully erosion areas in the Loess Hilly Gully Region[J]. Bulletin of Soil and Water Conservation, 2008, 28(5): 16-20]
[17] 李安怡,吴秀芹,朱清科. 陕北黄土区浅沟分布特征及其与立地类型的关系[J]. 西北农林科技大学学报(自然科学版),2010,38(4):79-85. [LI Anyi, WU Xiuqin, ZHU Qingke. Distribution characteristics and relation with site type of ephemeral gully in Loess Plateau of Northern Shaanxi Province[J]. Journal of Northwest A&F University(Natural Science Edition), 2010, 38(4): 79-85]
[18] 丁晓斌,郑粉莉,王彬,等. 子午岭地区坡面浅沟侵蚀临界模型研究[J]. 水土保持通报,2011,31(3):122-125. [DING Xiaobin, ZHENG Fenli, WANG Bin, et al. Predicting ephemeral gully erosion on hillslopes of Ziwuling area[J]. Bulletin of Soil and Water Conservation, 2011, 31(3): 122-125]
[19] WU Y, CHENG H. Monitoring of gully erosion on the Loess Plateau of China using a global positioning system [J]. Catena, 2005, 63(2-3): 154-166.
[20] CHENG H, ZOU X, WU Y, et al. Morphology parameters of ephemeral gully in characteristics hillslopes on the Loess Plateau of China [J]. Soil & Tillage Research, 2007, 94(1): 4-14.
[21] 郑粉莉,徐锡蒙,覃超. 沟蚀过程研究进展[J]. 农业机械学报,2016,47(8):48-59. [ZHENG Fenli, XU Ximeng, TAN Chao. A review of gully erosion process research[J]. Transactions of the Chinese Society for Agricultural Machinery, 2016, 47(8): 48-59]
[22] LI H,CRUSE R M,BINGNER R L, et al. Evaluating ephemeral gully erosion impact on Zea mays L. yield and economics using AnnAGNPS[J]. Soil and Tillage Research, 2016, 155: 157-165.
[23] RENGERS F K, TUCKER G E. The evolution of gully headcut morphology: a case study using terrestrial laser scanning and hydrological monitoring[J]. Earth Surface Processes and Landforms, 2015, 40(10): 1304-1317.
[24] 刘宝元,刘刚,王大安,等. 区域沟蚀野外调查方法——以东北地区为例[J]. 中国水土保持科学,2018,16(4):34-40. [LIU Baoyuan, LIU Gang, WANG Daan, et al. A field survey method for regional gully erosion: a case study in Northeastern China[J]. Science of Soil and Water Conservation, 2018, 16(4): 34-40]
[25] ANDERSON C J. Comparing the slope–area threshold for stream initiation in primeval and managed forests of Northern Michigan[J], Forest Science, 2020, 66(1): 130-139.
[26] 李浩,杨薇,刘晓冰,等. 沟蚀发生的地貌临界理论计算中数据获取方法及应用[J]. 农业工程学报,2019,35(18):128-134. [LI Hao, YANG Wei, LIU Xiaobing, et al. Data obtained method and application for topographic threshold theory calculation of gully initiation[J]. Transactions of the Chinese Society of Agricultural Engineering, 2019, 35(18): 128-134]
[27] MONTGOMERY D R. Slope distributions, threshold hillslopes, and steady-state topography[J]. American Journal of Science, 2001, 301(4-5): 432-454.
[28] TAROLLI P, FONTANA G D. Hillslope-to-valley transition morphology: new opportunities from high resolution DTMs[J]. Geomorphology, 2009, 113(1-2): 47-56.
[29] GUDINO-ELIZONDO N, BIGGS T W, CASTILLO C, et al. Measuring ephemeral gully erosion rates and topographical thresholds in an urban watershed using unmanned aerial systems and structure from motion photogrammetric techniques[J]. Land Degradation and Development, 2018, 29(6): 1896-1905.
[30] VANDEKERCKHOVE L, POESEN J, WIJDENES D O, et al. Thresholds for gully initiation and sedimentation in Mediterranean Europe[J]. Earth Surface Processes & Landforms, 2000, 25(11): 1201-1220.
[31] 王楠,陈一先,白雷超等. 陕北子洲县“7·26”特大暴雨引发的小流域土壤侵蚀调查[J]. 水土保持通报,2017,37(4):338-344,347. [WANG Nan, CHEN Yixian, BAI Leichao, et al. Investigation on soil erosion in small watersheds under “7·26” extreme rainstorm in Zizhou county, Northern Shaanxi province[J]. Bullet of Soil and Water Conservation, 2017, 37(4): 338-344,347]
[32] JUSTIN M G, BERGEN J M, EMMANUEL M S, et al. Mapping the gap of water and erosion control measures in the rapidly urbanizing Mbezi river catchment of Dar es Salaam[J]. Water, 2018. 10(1): 64.
[33] ARABAMERI A, CERDA A, PRADHAN B, et al. A methodological comparison of head-cut based gully erosion susceptibility models: combined use of statistical and artificial intelligence[J]. Geomorphology, 2020, 359: 107136.

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备注/Memo

备注/Memo:
收稿日期(Received date):2020-08-06; 修回日期(Accepted date):2020-10-07
基金项目(Foundation item):国家自然科学基金(41977062,41601290); 国家重点研发计划(2017YFD0800502)。[National Natural Science Foundation of China(41977062, 41601290); National Key Research and Development Program of China(2017YFD0800502)]
作者简介(Biography):刘欣(1993-),男,黑龙江安达人,硕士研究生,主要研究方向:数字地形分析与GIS应用。[LIU Xin(1993-), male, born in Anda, Heilongjiang province, M. Sc. candidate, research on digital terrain analysis and GIS application] E-mail: 201831809@stumail.nwu.edu.cn
*通讯作者(Corresponding author):王春梅(1983-),女,山东临邑人,副教授,硕士生导师,主要研究方向:侵蚀地形分析。[WANG Chunmei(1983-), female, Ph. D., associate professor, research on soil erosion assessment based on remote sensing and GIS] E-mail: cmwang@nwu.edu.cn
更新日期/Last Update: 2020-09-30