2021
DOI: 10.1007/s12665-021-09480-2
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Hydrogeomorphological analysis for hydraulic public domain definition: case study in Carrión River (Palencia, Spain)

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Cited by 5 publications
(5 citation statements)
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“…Depositional forms were set apart into low terraces, colluviums, structural surfaces, alluvial cones, fans, bars and plains. More details on the methodology can be found in Lombana and Martinez [12] (Figure 3). Based on these models, geomorphic elements were classified into different grou differentiating the units associated with sedimentary and erosion processes.…”
Section: Methodsmentioning
confidence: 99%
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“…Depositional forms were set apart into low terraces, colluviums, structural surfaces, alluvial cones, fans, bars and plains. More details on the methodology can be found in Lombana and Martinez [12] (Figure 3). Based on these models, geomorphic elements were classified into different grou differentiating the units associated with sedimentary and erosion processes.…”
Section: Methodsmentioning
confidence: 99%
“…Erosion g morphic units were delimited under four categories: low-water channels, second drainages, abandoned channels and historical channels. Depositional forms were set ap into low terraces, colluviums, structural surfaces, alluvial cones, fans, bars and pla More details on the methodology can be found in Lombana and Martinez [12] (Figure Subsequently, secondary, abandoned, and historical channels were categorized into Type A, B and C flows [21]: (a) Type A flows are those channels that in recent years have presented flows associated with low return periods (less than 5 years); (b) Type B drainages are related to higher return periods, and although surface flow is not directly observed, riparian vegetation can be found adjacent to its course; (c) Type C flows correspond to channels that could eventually present a flow of water in high return periods (greater than 50 years) and are associated with fluvial escarpments. This classification was made considering current water flows, which can be identified using high-resolution aerial imagery.…”
Section: Methodsmentioning
confidence: 99%
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“…It has a channel length of 197 km, with a drainage area of 3368 km 2 , average values of width of 40 m, river level of 0.5 m, discharges of 12 m 3 /s, and an annual maximum of 38 m 3 /s [30]. This river presents a marked lateral migration with a wide alluvial plain, where an active and/or abandoned drainage network can be identified [31]. Throughout its alluvial plain, agricultural activities and urban land uses can be found, so different elements can be exposed to flood risks [32].…”
Section: Introductionmentioning
confidence: 99%