Monitoring the temporal evolution of a Sicilian badland area by unmanned aerial vehicles

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Vincenzo Palmeri , Costanza Di Stefano , Gaetano Guida , Alessio Nicosia , Vito Ferro
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引用次数: 0

Abstract

Badlands are extremely fragmented landforms characterized by soil erosion processes at a short-time scale. In this paper, the annual evolution of hillslope morphological characteristics and erosion/deposition processes in a Sicilian badland area, surveyed on May 2021 and April 2022 by Unmanned Aerial Vehicles (UAVs), was investigated. Three-dimensional (3D) and planimetric (2D) approaches were applied to determine the badland morphometric characteristics. UAV surveys and photogrammetric 3D-model generation allowed for obtaining the digital terrain model and identifying the badland unit. The convergence index method was applied to evaluate the drainage network and its variation due to the erosion processes. The analysis highlighted a decrease of the morphometric indexes with increasing slope, which can be explained by the fact that the drainage network tends to be less tortuous and branched as slopes become steeper. The geomorphic change analysis showed that the soil erosion is evenly distributed along the badland slopes, while it is negligible along the drainage networks. The geomorphic changes due to slope collapses and soil erosion and deposition phenomena lead to a modification of the morphological characteristics of the badland unit, sub-units and the corresponding drainage networks. The results confirmed that badlands are intense erosion spots, with soil loss (approximately 348 t ha−1 y−1) much higher than the soil loss tolerance. Finally, the morphometric indexes were positively related to the sediment yield values, suggesting that in more extended and branched drainage networks sediment transport is more efficient.
利用无人飞行器监测西西里坏境的时间演变
荒地是一种极其破碎的地貌,其特点是土壤侵蚀过程时间很短。本文研究了 2021 年 5 月和 2022 年 4 月无人机(UAV)勘测的西西里坏境地区山坡形态特征和侵蚀/沉积过程的年度演变。采用了三维(3D)和平面测量(2D)方法来确定坏境的形态特征。通过无人机勘测和摄影测量三维模型生成,可以获得数字地形模型并确定坏境单元。收敛指数法用于评估排水网络及其因侵蚀过程而产生的变化。分析结果表明,随着坡度的增加,形态指数有所下降,这是因为随着坡度的增加,排水管网的曲折性和分支性会减弱。地貌变化分析表明,土壤侵蚀沿坏地斜坡均匀分布,而沿排水管网则微不足道。坡面崩塌、土壤侵蚀和沉积现象引起的地貌变化导致坏境单元、子单元和相应排水管网的形态特征发生改变。研究结果证实,坏境是水土流失严重的地方,土壤流失量(约 348 吨/公顷-年-1)远远高于土壤流失的容忍度。最后,形态指数与沉积物产值呈正相关,这表明在延伸和分支更多的排水管网中,沉积物的输送效率更高。
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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