Abstract
As one of most active gully types in the Chinese Loess Plateau, bank gullies generally indicate soil loss and land degradation. This study addressed the lack of detailed, large scale monitoring of bank gullies and proposed a semi-automatic method for extracting bank gullies, given typical topographic features based on 5 m resolution DEMs. First, channel networks, including bank gullies, are extracted through an iterative channel burn-in algorithm. Second, gully heads are correctly positioned based on the spatial relationship between gully heads and their corresponding gully shoulder lines. Third, bank gullies are distinguished from other gullies using the newly proposed topographic measurement of “relative gully depth (RGD).” The experimental results from the loess hilly area of the Linjiajian watershed in the Chinese Loess Plateau show that the producer accuracy reaches 87.5%. The accuracy is affected by the DEM resolution and RGD parameters, as well as the accuracy of the gully shoulder line. The application in the Madigou watershed with a high DEM resolution validated the duplicability of this method in other areas. The overall performance shows that bank gullies can be extracted with acceptable accuracy over a large area, which provides essential information for research on soil erosion, geomorphology, and environmental ecology.
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References
Afana A, del Barrio G (2009). An adaptive approach for channel network delineation from digital elevation models. In: Proceedings of Geomorphometry. Zurich, 224–230
Barnes R, Lehman C, Mulla D (2014). Priority-flood: an optimal depression-filling and watershed-labeling algorithm for digital elevation models. Comput Geosci, 62(1): 117–127
Benaïchouche A, Stab O, Tessier B, Cojan I (2016). Evaluation of a landscape evolution model to simulate stream piracies: insights from multivariable numerical tests using the example of the Meuse basin, France. Geomorphology, 253: 168–180
Betts H D, Trustrum N A, Rose R C D (2003). Geomorphic changes in a complex gully system measured from sequential digital elevation models, and implications for management. Earth Surf Process Landf, 28(10): 1043–1058
Cao M, Tang G A, Zhang F, Yang J (2013). A cellular automata model for simulating the evolution of positive–negative terrains in a small loess watershed. Int J Geogr Inf Sci, 27(7): 1349–1363
Castillo C, Gómez J (2016). A century of gully erosion research: urgency, complexity and study approaches. Earth Sci Rev, 160: 300–319
Chen L, Wei W, Fu B, Lü Y (2007). Soil and water conservation on the Loess Plateau in China: review and perspective. Prog Phys Geogr, 31 (4): 389–403
Congalton R G (1991). A review of assessing the accuracy of classifications of remotely sensed data. Remote Sens Environ, 37 (1): 35–46
Coppola E, Tomassetti B, Mariotti L, Verdecchia M, Visconti G (2007). Cellular automata algorithms for drainage network extraction and rainfall data assimilation. Hydrol Sci J, 52(3): 579–592
Dunkerley D (1997). Banded vegetation: development under uniform rainfall from a simple cellular automaton model. Plant Ecol, 129(2): 103–111
Evans M, Lindsay J (2010). High resolution quantification of gully erosion in upland peatlands at the landscape scale. Earth Surf Process Landf, 35(8): 876–886
Fairfield J, Leymarie P (1991). Drainage networks from grid digital elevation models. Water Resour Res, 27(5): 709–717
Gan Z M (1990). Geomorphology and Soil Erosion Research in Loess Plateau of China. Xi’an: Shaanxi People’s Publishing House (in Chinese)
Garbrecht J, Martz L (1997). The assignment of drainage direction over flat surfaces in raster digital elevation models. J Hydrol (Amst), 193 (1–4): 204–213
Harvey A (2001). Coupling between hillslopes and channels in upland fluvial systems: implications for landscape sensitivity, illustrated from the Howgill Fells, northwest England. Catena, 42(2): 225–250
Harvey A M (2002). Effective timescales of coupling within fluvial systems. Geomorphology, 44(3–4): 175–201
Hellweger F (1997). AGREE-DEM surface reconditioning system. Dissertation for PhD degree. University of Texas at Austin
Hessel H (2002). Modelling Soil Erosion in a Small Catchment on the Chinese Loess Plateau. Dissertation for PhD degree. University Utrecht, 61
Hessel R, van Asch T (2003). Modelling gully erosion for a small catchment on the Chinese Loess Plateau. Catena, 54(1): 131–146
Hu G, Wu Y Q (2005). Progress in the study of geomorphic threshold theory in channel (gully) erosion. Mountain Research, 23(5): 565–570 (in Chinese)
Jiang L, Tang G A, Zhao M W, Song X D (2013). Extraction and analysis of loess gully heads considering geomorphological structures. Geogr Res, 32(11): 2153–2162 (in Chinese)
Jing K (1986). A study on gully erosion on the Loess Plateau. Scientia Geographica Sinica, 6: 340–347 (in Chinese)
Jones R (2002). Algorithms for using a DEM for mapping catchment areas of stream sediment samples. Comput Geosci, 28(9): 1051–1060
Knight J, Spencer J, Brooks A, Phinn S (2007). Large-area, highresolution remote sensing-based mapping of alluvial gully erosion in Australia’s tropical rivers. In: Proceedings of the 5th Australian Stream Management Conference. New South Wales:199–204
Lashermes B, Foufoula‒Georgiou E, Dietrich W E (2007). Channel network extraction from high resolution topography using wavelets. Geophys Res Lett, 34: L23S04
Li B, Huang L, Feng L, Ma D (2014). Uncertainty of gully sediment budgets based on laser point cloud data. Transactions of the Chinese Society of Agricultural Engineering, 30(17): 183–191 (in Chinese)
Li Y, Poesen J, Yang J C, Fu B, Zhang J H (2003). Evaluating gully erosion using 137Cs and 210Pb/137Cs ratio in a reservoir catchment. Soil Tillage Res, 69(1): 107–115
Li Z, Zhang Y, Yao WJ, Zhu Q K (2011). Estimating gully development rates in hilly loess region of western Shanxi Province based on Quickbird images. Transactions of the Chinese Society of Agricultural Engineering, 28(22): 141–148 (in Chinese)
Li Z, Zhang Y, Zhu Q K, He Y M, Yao W J (2015). Assessment of bank gully development and vegetation coverage on the Chinese Loess Plateau. Geomorphology, 228: 462–469
Li Z, Zhang Y, Zhu Q K, Yang S, Li H J, Ma H (2017). A gully erosion assessment model for the Chinese Loess Plateau based on changes in gully length and area. Catena, https://doi.org/10.1016/j.catena.2016. 04.018
Liang C, MacKay D S (2000). A general model of watershed extraction and representation using globally optimal flow paths and up-slope contributing areas. Int J Geogr Inf Sci, 14(4): 337–358
Liu D S (1985). Loess and Environment. Beijing: Science Press
Liu Y B, Zhu X M, Zhou P H, Tang K L (1988). The law of hillslope channel erosion occurrence and development on loess plateau. Research of Soil and Water Conservation, 7: 9–18 (in Chinese)
Luo L X (1956). A tentative classification of landforms in the loess plateau. Acta Geogr Sin, 22(3): 201–222 (in Chinese)
Martínez-Casasnovas J (2003). A spatial information technology approach for the mapping and quantification of gully erosion. Catena, 50(2): 293–308
Martz L W, Garbrecht J (1992). Numerical definition of drainage network and subcatchment areas from digital elevation models. Comput Geosci, 18(6): 747–761
Metternicht G, Zinck J (1998). Evaluating the information content of JERS-1 SAR and Landsat TM data for discrimination of soil erosion features. ISPRS J Photogramm Remote Sens, 53(3): 143–153
Na J M, Yang X, Li M, Ding H, Tang G A (2016). Progress in geomorphology research on young gully in loess plateau. Geography and Geo-Information Science, 32(4): 68–75 (in Chinese)
Nyssen J, Poesen J, Moeyersons J, Luyten E, Veyret-Picot M, Deckers J, Haile M, Govers G (2002). Impact of road building on gully erosion risk: a case study from the northern Ethiopian highlands. Earth Surf Process Landf, 27(12): 1267–1283
O’Callaghan J F, Mark DM (1984). The extraction of drainage networks from digital elevation data. Comput Vis Graph Image Process, 28(3): 323–344
Oostwoud Wijdenes D J, Poesen J, Vandekerckhove L, Ghesquiere M (2000). Spatial distribution of gully head activity and sediment supply along an ephemeral channel in a Mediterranean environment. Catena, 39(3): 147–167
Persendt F, Gomez C (2016). Assessment of drainage network extractions in a low-relief area of the Cuvelai Basin (Namibia) from multiple sources: LiDAR, topographic maps, and digital aerial orthophotographs. Geomorphology, 260(s 1–2): 32–50
Poesen J, Nachtergaele J, Verstraeten G, Valentin C (2003). Gully erosion and environmental change: importance and research needs. Catena, 50(2–4): 91–133
Rengers F, Tucker G, Mahan S (2016). Episodic bedrock erosion by gully-head migration, Colorado High Plains, USA. Earth Surf Process Landf, 41(11): 1574–1582
Saunders W (1999). Preparation of DEMs for use in environmental modeling analysis. In: SRI User Conference. Beijing: China Cartographic Publishing House, 24–30
Schumm S A (1956). Evolution of drainage systems and slopes in badlands at Perth Amboy, New Jersey. Geol Soc Am Bull, 67(5): 597–646
Seginer I (1966). Gully development and sediment yield. J Hydrol (Amst), 4(4): 236–253
Shruthi R B, Kerle N, Jetten V (2011). Object-based gully feature extraction using high spatial resolution imagery. Geomorphology, 134(3): 260–268
Shruthi R B, Kerle N, Jetten V, Abdellah L, Machmach I (2015). Quantifying temporal changes in gully erosion areas with objectoriented analysis. Catena, 128: 262–277
Shruthi R B, Kerle N, Jetten V, Stein A (2014). Object-based gully system prediction from medium resolution imagery using Random Forests. Geomorphology, 216: 283–294
Sidorchuk A (1999). Dynamic and static models of gully erosion. Catena, 37(3–4): 401–414
Song X D, Tang G A, Li F Y, Jiang L, Zhou Y, Qian K J (2013). Extraction of loess shoulder-line based on the parallel GVF snake model in the loess hilly area of China. Comput Geosci, 52(1): 11–20
Stolte J, Liu B, Ritsema C, Van den Elsen H, Hessel R (2003). Modelling water flow and sediment processes in a small gully system on the Loess Plateau in China. Catena, 54(1): 117–130
Strahler A (1963). The Earth. NY: Sciences, Harper and Row, 557
Strahler A N (1957). Quantitative analysis of watershed geomorphology. Eos (Wash DC), 38(6): 913–920
Tang G A, Xiao C C, Jia D X, Yang X (2007). DEM based investigation of loess shoulder-line. In: Geoinformatics 2007: Geospatial Information Science. Nanjing: SPIE, 67532E
Tarboton D G (1997). A new method for the determination of flow directions and upslope areas in grid digital elevation models. Water Resour Res, 33(2): 309–319
Tarboton D G, Bras R L, Rodriguez-Iturbe I (1991). On the extraction of channel networks from digital elevation data. Hydrol Processes, 5(1): 81–100
Turcotte R, Fortin J P, Rousseau A, Massicotte S, Villeneuve J P (2001). Determination of the drainage structure of a watershed using a digital elevation model and a digital river and lake network. J Hydrol (Amst), 240(3–4): 225–242
Valentin C, Poesen J, Li Y (2005). Gully erosion: impacts, factors and control. Catena, 63(2): 132–153
Wang L, Liu H (2006). An efficient method for identifying and filling surface depressions in digital elevation models for hydrologic analysis and modelling. Int J Geogr Inf Sci, 20(2): 193–213
Wolman M G, Gerson R (1978). Relative scales of time and effectiveness of climate in watershed geomorphology. Earth Surf Processes, 3(2): 189–208
Wondzell S M, Cunningham G L, Bachelet D (1996). Relationships between landforms, geomorphic processes, and plant communities on a watershed in the northern Chihuahuan Desert. Landsc Ecol, 11(6): 351–362
Wu Y, Cheng H (2005). Monitoring of gully erosion on the Loess Plateau of China using a global positioning system. Catena, 63(2–3): 154–166
Wu Y, Zheng Q, Zhang Y, Liu B, Cheng H, Wang Y (2008). Development of gullies and sediment production in the black soil region of northeastern China. Geomorphology, 101(4): 683–691
Yan S J, Tang G A, Li F Y, Zhang L (2014). Snake model for the extraction of loess shoulder-line from DEMs. J Mt Sci, 11(6): 1552–1559
Zhang W, Yang X, Tang G A, Zhu S J, Li C L (2012). DEM-based flow direction algorithms study of stream extraction and watershed delineation in the low relief areas. Science of Surveying and Mapping, 37(2): 94–96 (in Chinese)
Zhang Y, Yang S, Li Z, Li H, He Y (2015). Effect of narrow terrace on gully erosion in Northern Shaanxi loess area. Transactions of the Chinese Society of Agricultural Engineering, 31(7): 125–130 (in Chinese)
Zhao J, Amerce M, Chen L, Govers G (2016). Vegetation cover and topography rather than human disturbance control gully density and sediment production on the Chinese Loess Plateau. Geomorphology, 274: 92–105
Zhou G, Sun Z, Fu S (2016). An efficient variant of the priority-flood algorithm for filling depressions in raster digital elevation models. Comput Geosci, 90: 87–96
Zhou Y, Tang G A, Yang X, Xiao C C, Zhang Y, Luo M L (2010). Positive and negative terrains on northern Shaanxi Loess Plateau. J Geogr Sci, 20(1): 64–76
Zhu H C, Tang G A, Qian K J, Liu H Y (2014). Extraction and analysis of gully head of Loess Plateau in China based on Digital Elevation Model. Chin Geogr Sci, 24(3): 328–338
Zhu X M (1956). Classification on the soil erosion in the loess region. Acta Pedologica Sinica, 4: 99–115 (in Chinese)
Acknowledgements
This research was supported by the National Natural Science Foundation of China (Nos. 41771415, 41471316, and 41271438) and a project funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions No. 164320H116. We thank Dr. Liyang XIONG who gave us many useful suggestions, Dr. Rui ZHU from The Hong Kong Polytechnic University for the language improvement, three anonymous reviewers for their useful suggestions, and Jilong LI, Wen DAI, Min LI, and Dr. Kai LIU for their field work assistance.
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Yang, X., Na, J., Tang, G. et al. Bank gully extraction from DEMs utilizing the geomorphologic features of a loess hilly area in China. Front. Earth Sci. 13, 151–168 (2019). https://doi.org/10.1007/s11707-018-0700-5
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DOI: https://doi.org/10.1007/s11707-018-0700-5