Littérature scientifique sur le sujet « Calcare cavernoso »
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Articles de revues sur le sujet "Calcare cavernoso"
Lauriol, Bernard, et Louise Godbout. « Les terrasses de cryoplanation dans le nord du Yukon : distribution, genèse et âge ». Géographie physique et Quaternaire 42, no 3 (18 décembre 2007) : 303–14. http://dx.doi.org/10.7202/032738ar.
Texte intégralLegatzki, Antje, Marian Ortiz, Julia W. Neilson, Sky Dominguez, Gary L. Andersen, Rickard S. Toomey, Barry M. Pryor, Leland S. Pierson et Raina M. Maier. « Bacterial and Archaeal Community Structure of Two Adjacent Calcite Speleothems in Kartchner Caverns, Arizona, USA ». Geomicrobiology Journal 28, no 2 (15 février 2011) : 99–117. http://dx.doi.org/10.1080/01490451003738465.
Texte intégralLegatzki, A., M. Ortiz, J. W. Neilson, R. R. Casavant, M. W. Palmer, C. Rasmussen, B. M. Pryor, L. S. Pierson et R. M. Maier. « Factors Influencing Observed Variations in the Structure of Bacterial Communities On Calcite Formations in Kartchner Caverns, AZ, USA ». Geomicrobiology Journal 29, no 5 (juin 2012) : 422–34. http://dx.doi.org/10.1080/01490451.2011.581326.
Texte intégralPark, Hyung-Jun, Hyun-Cheol Kim, Seung-Hee Yang et Jong-Un Lee. « A Study on Mineralogical and Microbiological Clogging in Water Curtain System of Underground Hydrocarbon Storage Caverns - Calcite and Slime-Forming Bacteria ». Journal of the Korean Society of Mineral and Energy Resources Engineers 54, no 1 (1 février 2017) : 11–19. http://dx.doi.org/10.12972/ksmer.2017.54.1.011.
Texte intégralFrahm, Jan-Peter, Anja Lindlar, Philip Sollman et Eberhard Fischer. « Bryophytes from the Cape Verde Islands ». Bryophyte Diversity and Evolution 12, no 1 (31 décembre 1996) : 123–53. http://dx.doi.org/10.11646/bde.12.1.15.
Texte intégralMansouri, Alireza, Alexandre Boutet, Gavin Elias, Jurgen Germann, Karim Mithani, George Ibrahim, Andres Lozano et Taufik Valiante. « NIMG-25. LESION-NETWORK ANALYSIS TO IDENTIFY PREFERENTIALLY-ENGAGED NETWORKS IN EPILEPTOGENIC TUMORS ». Neuro-Oncology 21, Supplement_6 (novembre 2019) : vi166—vi167. http://dx.doi.org/10.1093/neuonc/noz175.696.
Texte intégralBarbagli, Alessio, Fabio Nunzio Antonio Brogna, Ivan Callegari, Enrico Guastaldi, Giovanni Liali, Natalie Marsico, Carmela Rezza et Marilena Trotta. « Multi-isotope and Hydrogeochemical approach for characterizing Saturnia thermal groundwater (Grosseto, Italy) ». Acque Sotterranee - Italian Journal of Groundwater, 30 décembre 2013. http://dx.doi.org/10.7343/as-049-13-0076.
Texte intégralStokes, Tim R., et Paul A. Griffiths. « An Overview of the Karst Areas in British Columbia, Canada ». Geoscience Canada, 29 mars 2019, 49–66. http://dx.doi.org/10.12789/geocanj.2019.46.145.
Texte intégralSEDOR, FERNANDO ANTONIO, POLLYANA A. BORN et FÁBIO M. SOARES DOS SANTOS. « Fósseis pleistocênicos de Scelidodon (Mylodontidae) e Tapirus (Tapiridae) em cavernas paranaenses (PR, sul do Brasil) ». Acta Biológica Paranaense 33 (31 décembre 2004). http://dx.doi.org/10.5380/abpr.v33i0.627.
Texte intégralThèses sur le sujet "Calcare cavernoso"
Capacci, Fausto. « LA GESTIONE DELLE RISORSE IDRICHE E DEL TERRITORIO NELL’AMBITO DELLA PIANIFICAZIONE DI AREA VASTA : L’ESEMPIO DELL’ACQUIFERO DELLA MONTAGNOLA SENESE ». Doctoral thesis, Università di Siena, 2022. http://hdl.handle.net/11365/1217666.
Texte intégralThe Montagnola Senese aquifer (known as “Luco”) is an important and strategic water reserve in Southern Tuscany. With this study we have furthered our knowledge for the geometrical/structural, hydrodynamic and hydrochemical aquifer characterization and for the development of a conceptual model of it. In addition, this model provides the results of a work that aims to create a conceptual model and a first approach to the numerical model of flow in permanent regime for the evaluation and management of groundwater resources, while also assessing its vulnerability to pollution. New aquifer geometry data, represented by carbonate formation of Calcare Cavernoso and Breccia di Grotti, were acquired through geoelectrical surveys, geophysical tomography, borehole stratigraphy, a new deep borehole and compared with the geological mapping of Regione Toscana Continuum Map. This allowed to estimate the outcropping and non-outcropping aquifer extension (166,3 Km2), in respect of a feeding area of about 91,6 Km2. The entire permeable hydrogeological complex is found to have an average thickness of about 178 m. With regard to the hydrodynamic characterisation of the aquifer, which is necessary to describe the spatial and temporal trend of the piezometric surface, it can be stated that, despite the uneven spatial distribution of the measurement points, two main directions of underground water flow have been identified: southward (Piano di Rosia) and northwestward (Abbadia a Isola and Strove). This characterization of flows and hydrodynamic parameters needs further investigation in the future. The assessment of aquifer recharge was approached with two methodologies: - First one, evaluating the total infiltration in relation to the calculated water surplus infiltration, once the recharge area has been defined. This assessment (average data from 1967-2006) leads to estimate an average aquifer recharge of over 21·106 m3/year. - Second one, based on the excursion of the measured groundwater piezometric levels (March 2009-January 2010); it identifies a dynamic resource that, using an effective porosity (ne) of 8%, can be estimated at about 8,1·106 m3/year, to which should be added 12·106 m3/year of water that is currently withdrawn from the aquifer for a total amount of the annual hydric resource of about 20·106 m3. Even with all the limitations associated with this type of evaluation, the results obtained, with the two criteria, are in complete agreement with each other. As far as the water reserve is concerned, it is evaluated at around 1.5 billion m3, that is to say about 100 times greater than the dynamic resource. Comparing the renewable resource evaluations with current drinking water demand, we note that in the face of an average aquifer recharge of about 21·106 m3, water consumption is about 11,7·106 m3. Further utilisation of the aquifer hosted in the Montagnola Senese aquifer is therefore theoretically possible. Based on the knowledge gained, the conceptual model of the aquifer was created. The aquifer system has been represented using a three-dimensional finite element numerical model (FEM), by using FEFLOW (Finite Element subsurface FLOW system) numerical code, operating in permanent regime. Input data have been entered into the system by assigning boundary conditions at the hydraulic loading, at the water outflows and to the material properties such as permeability, porosity and infiltration. Final results made possible to estimate water quantities present in the aquifer, highlighting the importance and role played by meteoric infiltration in balancing the water outflows and keeping the system in balance. Given its strategic importance, to complete the hydrogeological study of Montagnola Senese aquifer, an assessment of its intrinsic vulnerability to pollution was also carried out using a simiparametric method called SIPS. This original methodology, which can be ascribable to a simplified SINTACS, made it possible, through the estimation of four basic parameters, to assess the intrinsic vulnerability of the groundwater aquifer, which is for 75% high to medium-high.
Natali, Francesca. « Rilevamento geologico del settore dell'Elba orientale tra la località Alberone e il Camping Canapai ». Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2022.
Trouver le texte intégralChapitres de livres sur le sujet "Calcare cavernoso"
Hose*, Louise D., Harvey R. DuChene*, Daniel Jones, Gretchen M. Baker*, Zoë Havlena, Donald Sweetkind et Doug Powell. « Hypogenic karst of the Great Basin ». Dans Field Excursions from the 2021 GSA Section Meetings, 77–114. Geological Society of America, 2021. http://dx.doi.org/10.1130/2020.0061(05).
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