Combined gully profiles for expressing surface morphology and evolution of gully landforms

Jingwei LI , Liyang XIONG , Guo’an TANG

Front. Earth Sci. ›› 2019, Vol. 13 ›› Issue (3) : 551 -562.

PDF (1787KB)
Front. Earth Sci. ›› 2019, Vol. 13 ›› Issue (3) : 551 -562. DOI: 10.1007/s11707-019-0752-1
RESEARCH ARTICLE
RESEARCH ARTICLE

Combined gully profiles for expressing surface morphology and evolution of gully landforms

Author information +
History +
PDF (1787KB)

Abstract

The expression of gully landforms can be regarded as an indicator of the evolutionary process of gullies. Most existing studies on the expression of gully landforms focus on plane characteristics. However, the vertical characteristics of a gully should be given considerable attention because gullies have mainly eroded the surface in the vertical direction. Current studies on vertical characteristics of gullies mainly focused on a single gully or rarely a few gullies, thereby failing to express the entire gully landform in a certain area. In this study, gully profile combination (GPC) was proposed to investigate the morphology and reveal the evolution of gully landforms. It was defined as the combination of vertical projection of all gully profiles in the entire drainage basin. Then, a gully evolution index and its statistic values were used to reveal the evolution of gully landforms based on GPC. The proposed method was applied and validated in three typical loess gully landform areas (i.e., loess tableland, ridge, and hill) in the Loess Plateau of China. Results show that GPC can effectively express gully landforms. The specific geomorphological feature (monoclinic loess tableland) can also be identified using GPC. The gully evolution index results also demonstrate different magnitudes of gully evolutionary stages in a certain area, which reflect the diversity of gullies. The average and median values of the gully evolution index increase in the three typical loess gully landforms. From loess tableland, loess ridge, and loess hill, the average values are 0.653, 0.703, and 0.763, and the median values are 0.661, 0.719, and 0.783, respectively. This method is also found to be stable with gully extraction thresholds for distinguishing different loess gully landforms. Accordingly, the evolution magnitudes of loess gully are obtained.

Keywords

gully profile combination / gully evolution / gully morphology / loess landform

Cite this article

Download citation ▾
Jingwei LI, Liyang XIONG, Guo’an TANG. Combined gully profiles for expressing surface morphology and evolution of gully landforms. Front. Earth Sci., 2019, 13(3): 551-562 DOI:10.1007/s11707-019-0752-1

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

Baker V R, Hamilton C W, Burr D M, Gulick V C, Komatsu G, Luo W, Rice J W Jr, Rodriguez J A P (2015). Fluvial geomorphology on Earth-like planetary surfaces: a review. Geomorphology, 245: 149–182

[2]

Berlin M M, Anderson R S (2007). Modeling of knickpoint retreat on the Roan Plateau, western Colorado. J Geophys Res Earth, 112(F3): F03S06

[3]

Bhowmik A K, Metz M, Schäfer R B (2015). An automated, objective and open source tool for stream threshold selection and upstream riparian corridor delineation. Environ Model Softw, 63: 240–250

[4]

Bishop P, Hoey T B, Jansen J D, Artza I L (2005). Knickpoint recession rate and catchment area: the case of uplifted rivers in Eastern Scotland. Earth Surf Process Landf, 30(6): 767–778

[5]

Cao J, Tang G, Fang X, Li J, Liu Y, Zhang Y, Zhu Y, Li F (2018). Terrain relief periods of loess landforms based on terrain profiles of the Loess Plateau in northern Shaanxi Province, China. Front Earth Sci, 13(2): 410–421

[6]

Casalí J, Loizu J, Campo M, De Santisteban L, Álvarez-Mozos J (2006). Accuracy of methods for field assessment of rill and ephemeral gully erosion. Catena, 67(2): 128–138

[7]

Castillo C, Gómez J A (2016). A century of gully erosion research: Urgency, complexity and study approaches. Earth Sci Rev, 160: 300–319

[8]

Castillo C, Taguas E V, Zarco-Tejada P, James M R, Gómez J A (2014). The normalized topographic method: an automated procedure for gully mapping using GIS. Earth Surf Process Landf, 39(15): 2002–2015

[9]

Castillo M (2017). Landscape evolution of the graben of Puerto Vallarta (west-central Mexico) using the analysis of landforms and stream long profiles. J S Am Earth Sci, 73: 10–21

[10]

Chang R (2015). Studies on gully erosion assessment and partitionin loess plateau based on shoulder lines. Dissertation for the Master’s Degree. Nanjing: Nanjing Normal University (in Chinese)

[11]

Daba S, Rieger W, Strauss P (2003). Assessment of gully erosion in eastern Ethiopia using photogrammetric techniques. Catena, 50(2-4): 273–291

[12]

Deng Q, Qin F, Zhang B, Wang H, Luo M, Shu C, Liu H, Liu G (2015). Characterizing the morphology of gully cross-sections based on PCA: A case of Yuanmou Dry-Hot Valley. Geomorphology, 228: 703–713

[13]

Di Stefano C, Ferro V, Pampalone V, Sanzone F (2013). Field investigation of rill and ephemeral gully erosion in the Sparacia experimental area, South Italy. Catena, 101: 226–234

[14]

Ferro-Vázquez CLang C, Kaal J, Stump D (2017). When is a terrace not a terrace? The importance of understanding landscape evolution in studies of terraced agriculture. J Environ Manage, 202(Pt 3): 500–513

[15]

Frankl A, Stal C, Abraha A, Nyssen J, Rieke-Zapp D, De Wulf A, Poesen J (2015). Detailed recording of gully morphology in 3D through image-based modelling. Catena, 127: 92–101

[16]

Guo R, Li F, He W, Yang S, Sun G 2010. Spatial and temporal variability of annual precipitation during 1958–2007 in Loess Plateau, China. In International Conference on Computer and Computing Technologies in Agriculture, 551–560

[17]

Gyasi-Agyei Y, Willgoose G, De Troch F P (1995). Effects of vertical resolution and map scale of digital elevation models on geomorphological parameters used in hydrology. Hydrol Process, 9: 363–382

[18]

Hayakawa Y S, Oguchi T (2006). DEM-based identification of fluvial knickzones and its application to Japanese mountain rivers. Geomorphology, 78(1-2): 90–106

[19]

Mararakanye N, Nethengwe N S (2012). Gully features extraction using remote sensing techniques. S Afr J Geomat, 1(2): 109–118

[20]

Klik A, Kluibenschädl F, Strohmeier S, Ziadat F, Zucca C (2016). Assessment of gully erosion using conventional field measurements: A case study from northern Ethiopia. J Soil Water Conserv, 71(6): 134A–139A

[21]

Kompani-Zare M, Soufi M, Hamzehzarghani H, Dehghani M (2011). The effect of some watershed, soil characteristics and morphometric factors on the relationship between the gully volume and length in Fars Province, Iran. Catena, 86(3): 150–159

[22]

Korzeniowska K, Pfeifer N, Landtwing S (2018). Mapping gullies, dunes, lava fields, and landslides via surface roughness. Geomorphology, 301: 53–67

[23]

Kosmowski F (2018). Soil water management practices (terraces) helped to mitigate the 2015 drought in Ethiopia. Agric Water Manage, 204: 11–16

[24]

Lv G, Xiong L, Chen M, Tang G, Sheng Y, Liu X, Song Z, Lu Y, Yu Z, Zhang K (2017). Chinese progress in geomorphometry. J Geogr Sci, 27(11): 1389–1412

[25]

Martínez-Casasnovas J A (2003). A spatial information technology approach for the mapping and quantification of gully erosion. Catena, 50(2-4): 293–308

[26]

Martins A A, Cabral J, Cunha P P, Stokes M, Borges J, Caldeira B, Martins A C (2017). Tectonic and lithological controls on fluvial landscape development in central-eastern Portugal: insights from long profile tributary stream analyses. Geomorphology, 276: 144–163

[27]

Na J, Yang X, Dai W, Li M, Xiong L, Zhu R, Tang G (2017). Bidirectional DEM relief shading method for extraction of gully shoulder line in loess tableland area. Phys Geogr, 39(4): 1–19

[28]

Onyelowe K C, Bui Van D, Ikpemo O C, Ubachukwu O A, Van Nguyen M (2018). Assessment of rainstorm induced sediment deposition, gully development at Ikot Ekpene, Nigeria and the devastating effect on the environment. Environmental Technology & Innovation, 10: 194–207

[29]

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

[30]

Oparaku L A, Iwar R T (2018). Relationships between average gully depths and widths on geological sediments underlying the Idah-Ankpa Plateau of the North Central Nigeria. Int Soil Water Conse, 6(1): 43–50

[31]

Perron J T, Kirchner J W, Dietrich W E (2009). Formation of evenly spaced ridges and valleys. Nature, 460(7254): 502–505

[32]

Phillips J D, Lutz J D (2008). Profile convexities in bedrock and alluvial streams. Geomorphology, 102(3-4): 554–566

[33]

Reddy G P O, Kumar N, Sahu N, Singh S K (2018). Evaluation of automatic drainage extraction thresholds using ASTER GDEM and Cartosat-1 DEM: a case study from basaltic terrain of Central India. Egypt J Remote Sens Space Sci, 21(1): 95–104

[34]

Rijal S, Wang G, Woodford P B, Howard H R, Hutchinson J M S, Hutchinson S, Schoof J, Oyana T J, Li R, Park L O (2018). Detection of gullies in Fort Riley military installation using LiDAR derived high resolution DEM. J Terramechs, 77: 15–22

[35]

Shruthi R B V, Kerle N, Jetten V (2011). Object-based gully feature extraction using high spatial resolution imagery. Geomorphology, 134(3-4): 260–268

[36]

Song X, Tang G, Li F, Jiang L, Zhou Y, Qian K (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

[37]

Strahler A N (1952). Hypsometric (area-altitude) analysis of erosional topography. Geol Soc Am Bull, 63(11): 1117–1142

[38]

Tang G, Jia Y, Yang X, Li F, Qumu W 2009. The profile spectrum of catchment boundary basing on DEMs in loess plateau. In: the 24th International Cartographic Conference, Santiago, Chile, 15–21

[39]

Taruvinga K (2009). Gully mapping using remote sensing: case study in KwaZulu-Natal, South Africa. Dissertation for the Master’s Degree. Waterloo: University of Waterloo

[40]

Valentin C, Poesen J, Li Y (2005). Gully erosion: impacts, factors and control. Catena, 63(2-3): 132–153

[41]

Wang K, Wang C, Qingfeng Z, Kailong D (2015). Loess shoulder line extraction based on openness and threshold segmentation. Acta Geodaetica Et Cartographica Sinica, 44: 67–75 (in Chinese)

[42]

Wang T, Yang X, Ye J, Wang C (2014). Identification of fluvial knickpoints and analysis of its scale effect based on DEMs. Journal of Geo-information Science, 16(6): 882–899 (in Chinese)

[43]

Willett S D, McCoy S W, Perron J T, Goren L, Chen C Y (2014). Dynamic reorganization of river basins. Science, 343(6175): 1248765

[44]

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

[45]

Xiong L Y, Tang G A, Li F Y, Yuan B Y, Lu Z C (2014). Modeling the evolution of loess-covered landforms in the Loess Plateau of China using a DEM of underground bedrock surface. Geomorphology, 209(1): 18–26

[46]

Xiong L Y, Tang G A, Strobl J, Zhu A X (2016). Paleotopographic controls on loess deposition in the Loess Plateau of China. Earth Surf Process Landf, 41(9): 1155–1168

[47]

Xiong L Y, Tang G A, Zhu A X, Yuan B Y, Lu B Y, Dang T M (2017). Paleotopographic controls on modern gully evolution in the loess landforms of China. Sci China Earth Sci, 60(3): 438–451

[48]

Xu M, Li Q, Wilson G (2016). Degradation of soil physicochemical quality by ephemeral gully erosion on sloping cropland of the hilly Loess Plateau, China. Soil Tillage Res, 155: 9–18

[49]

Yang X, Li M, Na J, Liu K (2017). Gully boundary extraction based on multidirectional hill-shading from high-resolution DEMs. Trans GIS, 21(6): 1204–1216

[50]

Yang X, Na J, Tang G, Wang T, Zhu A (2018). Bank gully extraction from DEMs utilizing the geomorphologic features of a loess hilly area in China. Front Earth Sci, 13(1): 151–168

[51]

Zabihi M, Mirchooli F, Motevalli A, Khaledi Darvishan A, Pourghasemi H R, Zakeri M A, Sadighi F (2018). Spatial modelling of gully erosion in Mazandaran Province, northern Iran. Catena, 161: 1–13

[52]

Zhang W, Hayakawa Y S, Oguchi T (2011). DEM and GIS based morphometric and topographic-profile analyses of Danxia landforms. Geomorphometry, 121–124

[53]

Zhao H, Fang X, Ding H, Josef S, Xiong L, Na J, Tang G (2017). Extraction of terraces on the Loess Plateau from high-resolution DEMs and imagery utilizing object-based image analysis. ISPRS Int Geo-Inf, 6(6): 157

[54]

Zhao J, Vanmaercke 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

[55]

Zhu H, Zhao Y, Liu H (2018). Scale characters analysis for gully structure in the watersheds of loess landforms based on digital elevation models. Front Earth Sci, 12(2): 431–443

[56]

Zhu S, Tang G, Xiong L, Zhang G (2014). Uncertainty of slope length derived from digital elevation models of the Loess Plateau, China. J Mt Sci, 11(5): 1169–1181

[57]

Zhu T X (2012). Gully and tunnel erosion in the hilly Loess Plateau region, China. Geomorphology, 153-154: 144–155

RIGHTS & PERMISSIONS

Higher Education Press and Springer-Verlag GmbH Germany, part of Springer Nature

AI Summary AI Mindmap
PDF (1787KB)

750

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/