Person: Martín Duque, José Francisco
Loading...
First Name
José Francisco
Last Name
Martín Duque
Affiliation
Universidad Complutense de Madrid
Faculty / Institute
Ciencias Geológicas
Department
Geodinámica, Estratigrafía y Paleontología
Area
Geodinámica Externa
Identifiers
17 results
Search Results
Now showing 1 - 10 of 17
Item Baseline to evaluate off-sitesuspended sediment-related mining effects in the Alto Tajo Natural Park, Spain(Land Degradation and Development, 2017) Zapico Alonso, Ignacio; Laronne, Jonathan; Martín Moreno, Cristina; Martín Duque, José Francisco; Ortega, Ana; Sánchez Castillo,LázaroMining is a human activity with considerable environmental impact. To evaluate such impacts, international laws require undertaking local studies based on direct sampling to establish baseline conditions of parameters modified by human activities. Mining takes place near the Alto Tajo Natural Park, where a suspended sediment concentration (SSC) baseline is required to determine whether mining affects water quality. To this end, we have monitored the Tajo River and its tributary the Tajuelo following Before–After Control-Impact (BACI) techniques, recommended by Australian and New Zealand laws, requiring a specific method based on continuous monitoring and sampling to enable evaluation of SSCs. An SSC baseline has been defined at stations situated upstream of the mining area and compared with those downstream. The highest detected SSC upstream of the Tajuelo mines was 24 g l−1 whereas the highest simultaneous downstream value was 391 g l−1, more than one order of magnitude higher than the supposed baseline (24 g l−1). Additionally, this value is 1000 times more than the average concentration of 25 mg l−1, used by the European Union until 2015, to guarantee the quality of salmonid waters. Following a BACI approach, a statistically significant SSC impact has been identified. The mined areas are the only source that can explain this increase. This is the first instance that such an increase and baseline have been found using this method. BACI is a simple and reliable method recommended for studying degraded areas rather than an irrelevant, fixed standard as included in most international laws.Item Geomorphic landscape design integrated with progressive mine restoration in clay quarries of Catalonia(International Journal of Mining, Reclamation and Environment, 2021) Martín Duque, José Francisco; Tejedor, M.; Martín Moreno, Cristina; Nicolau Ibarra, José Manuel; Sanz Santos, Miguel Ángel; Sánchez Donoso, Ramón; Gómez Díaz, José M.Geomorphic-based mine restoration of clay quarries in Tortosa (Catalonia) was co-funded by the European Union’s LIFE programme. The landform design was made with GeoFluv-Natural Regrade. Their building was performed with existing machinery pool and operators. The main constraint was the impossibility of setback regrading of pre-existing-benched highwalls. Progressive geomorphic mine restoration neither reduced mineral production nor changed the operations. The approach has resulted in higher landscape functionality and integration. Monitoring showed localised erosion due to poorly planned discharge of road runoff and sporadic tunnel erosion. Sediment movement at the designed drainage network is similar to the local fluvial dynamics.Item The Ribagorda sand gully (east-central Spain): Sediment yield and human-induced origin(Geomorphology, 2014) Martín Moreno, Cristina; Fidalgo Hijano, C.; Martín Duque, José Francisco; González Martín, J.A.; Zapico Alonso, Ignacio; Laronne, JonathanGullies are developed under different climatic conditions and lithologies; however, those formed on sands have been scarcely described. This paper reports the study of the Ribagorda sand gully, 2.57 ha in area (east-central Spain). The main objectives were to characterize and quantify its geomorphic dynamics and to trace its origin. We described the landforms of the gully and measured the surface strength of the sand. We monitored, for six years, the filling of the storage areas of three check dams built downstream from the gully, and related it with rainfall characteristics. We also described the nature of the sediments trapped by the dams and estimated the amount of sediment eroded since the gully formation. Finally, we consulted historical records and maps to determine past land uses and transformations that may have affected the origin of the gully. The study shows a high diversity of landforms, denoting active processes, consistent with a measured mean annual sediment yield of 114 Mg ha−1 yr−1. A statistically significant relationship exists between the mass of sediment (Mg) and: 1) the total rainfall (mm) (P = 0.0007) or 2) the analysed rainfall intensities. Among five identified facies in the sedimentarywedge, the sandy ones are predominant. The total amount of sediment eroded by the Ribagorda gully since its originwas 962,800Mg. The results are unequivocal signs of an intense geomorphic activity within the gully, with an alluvial-fan type deposition in the dams.We interpret that the Ribagorda gully was initiated by deforestation after the 13th century, when forests began to be intensively logged, and before the 18th century,when the gullywas first indirectly described in print. The age, origin, evolution and dynamics of this gully indicate that this landscape is currently evolving towards a new steady state, after human disturbances over centuries. Given the gully evolution and local extent, we suggest that no correction measures are needed for its management.Item Erosión minera en la cuenca del arroyo Peñalén (Parque Natural del Alto Tajo, Guadalajara)(Comprendiendo el relieve: del pasado al futuro, 2016) Martín Moreno, Cristina; Martín Duque, José Francisco; Nicolau Ibarra, José Manuel; Muñoz Martín, AlfonsoItem Geomorphic rehabilitation in Europe: recognition as best available technology and its role in LIFE projects(2019) Martín Duque, José Francisco; Tejedor, M.; Martín Moreno, Cristina; Nicolau Ibarra, José Manuel; Zapico Alonso, Ignacio; Fourie, A. B.; Tibbett, M.Geomorphic rehabilitation ([GR], also known as geomorphic reclamation or geomorphic restoration) is a general term to describe alternative methods and procedures to conventional mine rehabilitation. The main aim of GR is to replicate ‘natural’ landforms for the new conditions after mining and to restore functionality and diversity of ecosystems at degraded sites. The correct application of the GR technique ensures visual integration with surrounding landscapes. Although GR is a broad term, referring to any geomorphic restoration of land, GR is often synonymous with fluvial GR, mostly following the GeoFluvTM-Natural Regrade method. This paper describes how and why the application of GR through GeoFluv-Natural Regrade in Spain since 2009 has attracted formal recognition by the European Commission (EC) of the European Union (EU) as one, among others, of a catalogue of best available techniques (BATs) for the management of waste from extractive industries, in accordance with the European Directive 2006/21/EC. GR has been recognised as BAT at the EU for multiple reasons, including mine site monitoring results that demonstrate increased physical stability with minimised erosion from stormwater and snowmelt runoff; natural hydrological function being established; the variability within the formed landform promotes ecological diversity for vegetation and wildlife communities; construction and short and long-term maintenance and repair costs are minimised; and visual impact of the mined landscape is reduced. This paper describes also the role of GeoFluv-Natural Regrade GR in the L’Instrument Financier pour l’Environnement (LIFE) program, which is the EU’s most important funding instrument addressing environment and climate action. A focus is provided on the LIFE TECMINE project, described in detail, since it is the most recent and complete GeoFluv-Natural Regrade example in Europe. The TECMINE project is a geomorphic-based ecological restoration project in the Valencia province, within the Iberian Mountain Range and where conventional mine rehabilitation practice, based on gradient terraces, shows general and widespread failure. The demonstration project is fostered by the Administration of the Valencia Region, which seeks to test innovative techniques (GR, micro-catchments, soil amendments and new protocols of revegetation) for mine rehabilitation, promote improved practices and disseminate the best practice output through their development and analysis. Testing GR is the main focus of the project. The application of GR at the TECMINE project included (a) finding ‘natural’ and ‘stable’ landforms and landscapes to be used as reference or analogues for replication in GR, although difficult, was possible due to ancestral land transformation; (b) the steep terrain, characteristic of the Iberian Range, challenged the formation of GR GeoFluv-Natural Regrade designs, but the project demonstrated that they can be implemented in that mountain setting; (b) the mining company reported similar cost estimations for this alternative GR rehabilitation (as-built) as that for a conventional restoration design (projected); (c) a holistic approach to GR, not dealing only with topography, allowed the identification and use of limestone colluvium as an adequate growth media for initiating soil development; this solution not used before for rehabilitation in this region provided a clear and advanced contribution from the project.Item Transformación del Territorio y Cambio Global(2011) Martín Duque, José Francisco; de Alba, S.; Alcázar, M.; Barbero, F.; Cermeño, I.; Lucia, Angelo; Martín Moreno, Cristina; Zapico Alonso, Ignacio; Pérez-Monserrat, Elena M.; Charco Romero, MaríaItem Effects of Topography and Surface Soil Cover on Erosion for Mining Reclamation: The Experimental Spoil Heap at El Machorro Mine (Central Spain)(Land Degradation and Development, 2016) Martín Moreno, Cristina; Martín Duque, José Francisco; Nicolau Ibarra, José Manuel; Hernando Rodríguez, Néstor; Sanz Santos, Miguel Ángel; Sánchez Castillo, LázaroMining reclamation tries to reduce environmental impacts, including accelerated runoff, erosion and sediment load in the nearby fluvial networks and their ecosystems. This study compares the effects of topography and surface soil cover on erosion on man-made slopes coming from surface mining reclamation in Central Spain. Two topographic profiles, linear and concave, with two surface soil covers, subsoil and topsoil, were monitored for two hydrologic years. Sediment load, rill development and plant colonization from the four profiles were measured under field conditions. The results show that, in the case of this experiment, a thick and non-compacted topsoil cover on a linear slope yielded less sediment than carbonate colluvium or topsoil cover on a concave slope. This study also shows that vegetation establishment, which plays an important role in erosion control, depends on topography. Plant cover was more widespread and more homogeneous on linear profiles with topsoil cover. On concave slopes, plant establishment was severely limited on the steepest upper part and favoured in the bottom. This study suggests that management of topography and surface soil cover should be approached systematically, taking three outcomes into consideration: (i) topsoil can lead to a successful mining reclamation regardless of topography, (ii) created concave slopes can lead to a successful mining reclamation and (iii) topography determines the vegetation colonization pattern.Item Impacto hidrogeomorfológico de las minas y escombreras de Peñalén (Guadalajara) sobre el Parque Natural del Alto Tajo(Cuaternario y geomorfología, 2009) Martín Duque, José Francisco; Martín Moreno, Cristina; Nicolau Ibarra, José Manuel; Sanz Santos, Miguel Ángel; Lucía Vela, AnaEl municipio de Peñalén (Guadalajara) alberga un conjunto de minas y escombreras degradadas, cuyo impacto ambiental sobre el inmediato Parque Natural del Alto Tajo es objeto de constante discusión. En este trabajo se ha llevado a cabo una primera aproximación al problema, tratando de caracterizar los condicionantes geomorfológicos del impacto hidrológico, de identificar las principales fuentes de sedimentos y de cuantificar los sedimentos que son emitidos desde estas zonas mineras y desde sus alrededores a la red fluvial. Esta aproximación ha puesto de manifiesto tres evidencias claras: (i) las zonas mineras de Peñalén se sitúan en localizaciones muy vulnerables a la erosión hídrica; (ii) los procesos erosivos y de emisión de sedimentos hacia el río Tajo son muy importantes desde esas zonas mineras y desde cárcavas naturales; (iii) existe una conexión hidrológica directa entre las fuentes de sedimentos de las zonas mineras degradadas de Peñalén y el río Tajo.Item Hacia una Minería Sostenible en el 95 entorno del Parque Natural del Alto Tajo. La escombrera experimental de la mina ‘El Machorro’(Poveda de la Sierra, Guadalajara)(Conferencia Internacional - Minería Sostenible. Santiago de Compostela. Cámara Oficial Mineira de Galicia, 2009, 2009) Hernando, Nestor; Martín Moreno, Cristina; Sánchez Castillo, Lázaro; Martín Duque, José Francisco; Sanz Santos, Miguel Ángel; Nicolau Ibarra, José ManuelPor su situación en el entorno de un espacio natural protegido, y sobre una ladera de pendiente y longitud elevadas, la restauración de la mina El Machorro constituye un importante reto científico y profesional. La empresa propietaria de esta mina, CAOBAR S.A., tiene entre sus objetivos demostrar la compatibilidad de la actividad minera con la conservación del medio ambiente. Por todo ello está acometiendo sucesivas revisiones de su Plan de Restauración del Espacio Natural (PREN), tratando de incorporar las mejores prácticas internacionales al respecto. Todo ello en colaboración con las universidades Complutense y de Alcalá (Madrid) y bajo la supervisión de la Dirección del Parque Natural del Alto Tajo. Una de las acciones más destacadas a ese respecto ha sido la construcción de una escombrera experimental, específicamente diseñada para mejorar la restauración de los terrenos afectados por la mina. En ella se estudia el comportamiento erosivo que tienen diferentes diseños de escombreras mediante la combinación de: (a) distintas topografías (cóncava y en terrazas); (b) distintos tipos de sustrato (estériles, coluviones y suelos originales); y (c) distintos tipos de revegetación (como hidrosiembras). En la comunicación se describen los detalles de la puesta en funcionamiento de esta escombrera experimental, así como los resultados obtenidos para el periodo 1 de noviembre de 2008 a 31 de marzo de 2009.Item Reconstrucción geomorfológica de restauraciones mineras. El modelo "cuenca en ladera" de la cantera de La Higuera (Segovia)(Avances de la geomorfología en España, 2008-2010. XI Reunión Nacional de Geomorfología, Solsona 2010, 2010) Martín Duque, José Francisco; Feria, María; Martín Moreno, Cristina; Nicolau Ibarra, José Manuel; Sanz Santos, Miguel Ángel; Úbeda, X.; Vericat, D.; Batalla, R.J.Se explica un modelo de restauración minera basado en principios geomorfológicos, denominado ‘cuencas en ladera’. El modelo establece un manejo experto de la escorrentía a partir de un diseño que compartimenta el relieve en pequeñas cuencas hidrográficas. Adicionalmente incluye criterios sobre el manejo de formaciones superficiales y suelos. Una restauración minera llevada a cabo según este modelo fue ejecutada durante el otoño de 2008 en una cantera de arcillas situada en La Higuera (Segovia). El seguimiento de la superficie restaurada pone de manifiesto un éxito de la restauración en términos de respuesta erosiva.