Inmaculada Rodriguez-Santalla

Dr. Inmaculada Rodriguez-Santalla

Department of Biology and Geology, Physics and Inorganic Chemistry of the Rey Juan Carlos University, Mostoles, Spain
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Research Focus & Metrics

Academic Career Length

18Years (2009-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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IRInmaculada Rodriguez-Santalla
Inmaculada Rodriguez-Santalla
NNNuria Navarro
Nuria Navarro
Coastal wetlands are dynamic ecosystems that exist at the interface between land and sea. They represent environments with a great diversity of habitats and communities, high carbon sequestration capacity and a wide range of ecosystem services. In the Mediterranean, the largest coastal wetlands are found in deltaic areas like that of the Ebro River (Spain), which has a coastline length of approximately 50 km, occupying a total area of 325 km2. The Ebro Delta is included in different national and international frameworks for environmental conservation, despite which there are several risks that threaten it. The lack of sedimentary contributions due to the regulation of the Ebro riverbed (irrigation, reservoirs, and hydroelectric power generation) has caused erosion and the retreat of certain sections of its coastline. To this situation of sediment deficit must be added the threat posed by the effects of global change, such as the rise in sea level, the increase in temperature and in the frequency and intensity of storms. This study analyses the particularities of the coastal wetland of the Ebro Delta, identifying the main threats it faces, as well as possible adaptation and mitigation strategies to these changes.

22 February 2021 in Remote Sensing
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IRInmaculada Rodriguez-Santalla
Inmaculada Rodriguez-Santalla
DGDavid Gomez-Ortiz
David Gomez-Ortiz
TMTomás Martín-Crespo
Tomás Martín-Crespo
MSMaría José Sánchez-García
María José Sánchez-García
IMIsabel Montoya-Montes
Isabel Montoya-Montes
Francisco Javier Gracia PrietoFrancisco Javier Gracia Prieto
Francisco Javier Gracia Prieto
La Banya spit, located at the south of the River Ebro Delta, is a sandy formation, developed by annexation of bars forming successive beach ridges, which are oriented and modeled by the eastern and southern waves. The initial ridges run parallel to the coastline, and above them small dunes developed, the crests of which are oriented by dominant winds, forming foredune ridges and barchans. This study attempted to test a number of techniques in order to understand the dune dynamic on this coastal spit between 2004 and 2012: LiDAR data were used to reconstruct changes to the surface and volume of the barchan dunes and foredunes; ground-penetrating radar was applied to obtain an image of their internal structure, which would help to understand their recent evolution. GPS data taken on the field, together with application of GIS techniques, made possible the combination of results and their comparison. The results showed a different trend between the barchan dunes and the foredunes. While the barchan dunes increased in area and volume between 2004 and 2012, the foredunes lost thickness. This was also reflected in the radargrams: the barchan dunes showed reflectors related to the growth of the foresets while those associated with foredunes presented truncations associated with storm events. However, the global balance of dune occupation for the period 2004–2012 was positive.

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NNNuria Navarro
Nuria Navarro
IRInmaculada Rodriguez-Santalla
Inmaculada Rodriguez-Santalla
Coastal wetlands are valuable and sensitive environments that are among the most productive yet highly threatened systems in the world

15 September 2022 in Remote Sensing
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SMSilvia Martín
Silvia Martín
IRInmaculada Rodriguez-Santalla
Inmaculada Rodriguez-Santalla
NSNikoletta Ropero Szymañska
Nikoletta Ropero Szymañska
DGDavid Gomez-Ortiz
David Gomez-Ortiz
TMTomás Martín-Crespo
Tomás Martín-Crespo
CICristina de Ignacio
Cristina de Ignacio
The Hiendelaencina district in Spain was the most important silver producer in Europe during 1844–1925. At the end of the 20th century, with mines having closed, some waste rock dumps were reprocessed, and the sludge from the flotation process was stored in two tailings ponds. When this activity ceased, the residues began to be eroded and disperse. In this study, the state of degradation of both deposits was evaluated using historical mapping and light detection and ranging (LiDAR) data, incorporated into a Geographic Information System. In the aerial images (1946–2018), mine tailings and their main erosive and sedimentary forms were mapped. Geoforms linked to hydrological (channels, gullies, alluvial cones), wind (eolian mantles), hydric–gravitational (colluvium) and anthropic (motorbike tracks) processes which move sludge into the surrounding areas were identified. A net loss of 8849 m3 of sludge, a release of 10.3 t of potentially polluting substances and a high erosion rate of 346 t/ha*year were calculated based on LiDAR data from 2009 and 2014. The ponds show a current high degree of erosion that could increase due to both human activity and the growing frequency of drought and torrential rain periods if stabilization measures are not undertaken.

1 October 2016 in Applied Geography
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Juan Ramírez-CuestaJuan Ramírez-Cuesta
Juan Ramírez-Cuesta
IRInmaculada Rodriguez-Santalla
Inmaculada Rodriguez-Santalla
FGF. Javier Gracia
F. Javier Gracia
MSMaría José Sánchez-García
María José Sánchez-García
Fernando Barrio-ParraFernando Barrio-Parra
Fernando Barrio-Parra