Encontrados 12 documentos, a visualizar página 1 de 2
Reconstruction of remote climate change from borehole temperature measurement i...
Barkaoui, Alae-Eddine; Correia, António; Zarhloule, Yassine; Rimi, Abdelkrim; Carneiro, Júlio; Boughriba, Mimoun; Verdoya, MassimoData from temperature measurements in boreholes are indicators of the temperature variations associated with past climate change. This paper is a contribution to reconstruct the ground surface temperature history (GSTH) from geothermal data in the eastern part of Morocco. From a set of several temperature logs, measured in the study area, only two were found suitable for estimating the ground surface temperatur...
Reconstruction of remote climate change from borehole temperature measurement i...
Barkaoui, Alae-Eddine; Correia, António; Zarhloule, Yassine; Rimi, Abdelkrim; Carneiro, Júlio; Boughriba, Mimoun; Verdoya, MassimoData from temperature measurements in boreholes are indicators of the temperature variations associated with past climate change. This paper is a contribution to reconstruct the ground surface temperature history (GSTH) from geothermal data in the eastern part of Morocco. From a set of several temperature logs, measured in the study area, only two were found suitable for estimating the ground surface temperatur...
CCS infrastructure development scenarios for the integrated Iberian Peninsula a...
Kanudia, Amit; Berghout, Niels; Boavida, Dulce; Van den Broek, Machteld; Cabal, Helena; Carneiro, Júlio; Fortes, Patrícia; Gargiulo, MaurizioThis paper briefly illustrates a method to represent national energy systems and the geographical details of CCS infrastructures in the same technical-economic model. In the MARKAL-TIMES modeling framework a model of Morocco, Portugal and Spain with both spatial and temporal details has been implemented. As a function of assumptions on the development to 2050 of mitigation levels, economic growth and CO2 captur...
Planning CCS development in the West Mediterranean
Boavida, Dulce; Carneiro, Júlio; Martinez, Roberto; Van den Broek, Machteld; Ramirez, Andrea; Rimi, Abdelkrim; Tosato, GianCarlo; Gastine, MarieTransport and storage of CO2 are the elements in the CCS chain with the lowest cost, but they may well prove to be the elements defining the timeline for CCS development. The EU FP7 COMET project aimed to pave the road towards CCS development in the West Mediterranean (Portugal, Spain and Morocco). This paper provides the main highlights of the work conducted within COMET. The project addressed the temporal and...
Region specific challenges of a CO2 pipeline infrastructure in the West Mediter...
Van den Broek, Machteld; Mesquita, Paulo; Carneiro, Júlio; Silva, José Rafael; Berghout, Niels; Ramirez, Andrea; Gouveia, João Pedro; Seixas, JúliaThis paper presents results of potential CCS infrastructures in the West Mediterranean region including trajectories for CO2 pipelines. The preliminary results are generated with a combination of geographical (GIS) and partial equilibrium optimization modelling (MARKAL/TIMES-COMET). Furthermore, as a result of active stakeholder involvement in the research project, the CCS infrastructures were critically review...
Towards a de-carbonized energy system in North-Eastern Morocco: Prospective Geo...
Rimi, Abdelkrim; Zarhloule, Yassine; Barkaoui, Alae Eddine; Correia, António; Carneiro, Júlio; Verdoya, Massimo; Lucazeau, FrancisGeothermal data has been indicating promising potentialities in the north-eastern Morocco. This paper presents new temperature data, recently recorded in water boreholes located in the Berkane and Oujda areas. Generally, the observed temperature gradients are rather high. One hole near Berkane, revealed an average geothermal gradient of more than 110 °C/km at depths greater than 300 m. This result confirms the ...
Structural and hydrogeological features of a Lias carbonate aquifer in the Trif...
Sardinha, João; Carneiro, Júlio; Zarhloule, Yassine; Barkaoui, Alae Eddine; Correia, António; Boughriba, Mimoun; Rimi, Abdelkrim; Houadi, B. ElThe rising demand for water and the contamination of shallow water table aquifers has led authorities in NE Morocco to look for deeper groundwater resources in the Triffa Plain, namely in Lower Jurassic (Lias) dolomitic limestones. The liassic aquifer is of strategic importance for the development of the region, however, its hydrodynamic behaviour is poorly understood due to lack of hydrogeological data and blo...
Evaluation of climate change effects in a coastal aquifer in Morocco using a de...
Carneiro, Júlio; Boughriba, Mimoun; Correia, António; Zarhloule, Yassine; Rimi, Abdelkrim; El Houadi, BoubkerA density-dependent numerical groundwater model was applied to study the climate change impact in a shallow aquifer in the Mediterranean coast of Morocco, the Saidia aquifer. The stresses imposed to the model were derived from the IPCC emission scenarios and included recharge variation and sea level rise. The main effect of the climate change in the Saidia aquifer will be a decrease in renewable resources, whic...
New Geothermal Prospect in North-Eastern Morocco
Rimi, Abdelkrim; Correia, António; Carneiro, Júlio; Verdoya, Massimo; Zarhloule, Yassine; Lucazeau, Francis; Boughriba, Mimoun; Barkaoui, Alae EddineGeothermal data has been indicating promising potentialities in the north-eastern Morocco. This paperpresents new temperature data, recently recorded in water borehole located in the Berkane and Oujda areas. Generally, the observed temperature gradients are rather high. One hole near Berkane, revealed an average geothermal gradient of more than 110 ºC/km at depths greater than 300 m. This result confirms the ge...
CLIMATE CHANGE AND HUMAN ACTIVITIES IMPACT ON THE GROUNDWATER OF THE EASTERN MO...
Zarhloule, Yassine; Fekkoul, A.; Boughriba, Mimoun; Carneiro, Júlio; Correia, António; Kabbabi, A.; Rimi, Abdelkrim; Houadi, B.ElLocated at the North-eastern part of Morocco the plain of Triffa and the area of Saïdia are under a semiarid climate (Fig1). The water resources in this zone are rather fragile and influenced by a highly irregular rainfall distribution, both in time (annual and inter-annual distribution) and in space with a yearly average which does not exceed 240 mm.
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