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Artykuły w czasopismach na temat "Fractured weathered rock"
Colegial-Gutiérrez, Juan Diego, María Camila Forero-Quintero, María Alejandra Fuentes-Rueda i Sully Gomez Isidro. "Characterization of weathering profiles of the crystal rocks of eastern Bucaramanga and definition of hydrogeological properties". Boletín de Ciencias de la Tierra, nr 41 (1.01.2017): 16–30. http://dx.doi.org/10.15446/rbct.n41.59347.
Pełny tekst źródłaHasan, Muhammad, Yanjun Shang, Weijun Jin i Gulraiz Akhter. "Assessment of Aquifer Vulnerability Using Integrated Geophysical Approach in Weathered Terrains of South China". Open Geosciences 11, nr 1 (31.12.2019): 1129–50. http://dx.doi.org/10.1515/geo-2019-0087.
Pełny tekst źródłaSalami, A. S., i E. M. Babafemi. "Delineation of Near-Surface Structural Features Suitable for Groundwater Accommodation Using 1-D and 2-D Resistivity Methods in Igarra, Akoko-Edo, Southwestern Nigeria". Journal of Applied Sciences and Environmental Management 24, nr 7 (7.08.2020): 1209–15. http://dx.doi.org/10.4314/jasem.v24i7.13.
Pełny tekst źródłaMahi, Shuaibu, Abubakar Yusuf i Garba Lawal. "Geoelectrical Assessment of Groundwater Potential within Zamfara and its Environs, Northwestern Nigeria". Caliphate Journal of Science and Technology 4, nr 1 (10.02.2022): 54–70. http://dx.doi.org/10.4314/cajost.v4i1.8.
Pełny tekst źródłaBriški, Maja, Andrej Stroj, Ivan Kosović i Staša Borović. "Characterization of Aquifers in Metamorphic Rocks by Combined Use of Electrical Resistivity Tomography and Monitoring of Spring Hydrodynamics". Geosciences 10, nr 4 (10.04.2020): 137. http://dx.doi.org/10.3390/geosciences10040137.
Pełny tekst źródłaThi Luan, Bui, i Lieu Kim Phuong. "Petrographic characterization and petroleum potential of Mesozoic carbonate rock in Block 106, Northern Red river basin". Science and Technology Development Journal - Natural Sciences 2, nr 6 (26.01.2020): 146–64. http://dx.doi.org/10.32508/stdjns.v2i6.876.
Pełny tekst źródłaChang, Seeun, Wooyong Um, Won-Seok Kim i HyunJu Kim. "Effect of seawater intrusion on radioactive strontium (90Sr) sorption and transport at nuclear power plants". Radiochimica Acta 106, nr 2 (26.01.2018): 147–60. http://dx.doi.org/10.1515/ract-2016-2724.
Pełny tekst źródłaZhang, Qian, Shu Cai Li, Li Ping Li i Qian Qing Zhang. "Experimental Study on Creep of Highly-Weathered Breccia". Applied Mechanics and Materials 477-478 (grudzień 2013): 588–91. http://dx.doi.org/10.4028/www.scientific.net/amm.477-478.588.
Pełny tekst źródłaVafidis, A., A. Andronikidis, H. Hamdan, G. Kritikakis, N. Economou, G. Panagopoulos, S. Zanettidis i in. "Rock characterization for the foundation of two water reservoirs using geophysical and borehole data". Bulletin of the Geological Society of Greece 47, nr 3 (21.12.2016): 1345. http://dx.doi.org/10.12681/bgsg.10919.
Pełny tekst źródłaOLICHWER, Tomasz. "HYDROGEOLOGICAL CHARACTERIZATION OF LOCAL GROUNDWATER RESERVOIRS IN THE KŁODZKO LAND (SUDETES - SW POLAND) BASED ON AN ANALYSIS OF THE DISCHARGES OF SPRINGS". Carpathian Journal of Earth and Environmental Sciences 18, nr 1 (7.02.2023): 171–82. http://dx.doi.org/10.26471/cjees/2023/018/249.
Pełny tekst źródłaRozprawy doktorskie na temat "Fractured weathered rock"
Rusagara, Radegonde. "Développement d'un modèle conceptuel de recharge des aquifères de socle cristallin dans la zone sahélienne du Burkina Faso en Afrique de l'Ouest". Electronic Thesis or Diss., Sorbonne université, 2022. http://www.theses.fr/2022SORUS319.
Pełny tekst źródłaGroundwater recharge rate for weathered rock aquifers in the Sahel of West Africa are sparse due to insufficient knowledge of the recharge pathways. This study was initiated in the Tougou ephemeral river catchment (37 km2) to improve understanding of recharge pathways to a weathered rock aquifer in the dryland of Burkina Faso. It is based on field investigations conducted in 2016–2020 on a piezometric transect and large-diameter wells, perpendicular and longitudinal to the river, respectively. Geophysical measurements, lithologs analysis, permeability tests, measurements of groundwater electrical conductivity and temperature, groundwater and river level monitoring, and rainfall measurements were undertaken. The results showed a laterally continuous saprolite aquifer (10–22 m thick) overlain by residual soils beneath the river and discontinuous laterite on the banks. Below the river, the saprolite overlays the weathered schist aquifer with an upward or downward hydraulic gradient regardless of the seasons. The saprolite is replenished by focused recharge from the river and diffuse recharge from the rainfall on the banks, according to information from the groundwater hydrographs, groundwater tracing results, and cross-correlation between the groundwater levels and the two potential recharge sources (rainfall and river water). The values of soil hydraulic conductivity and the presence of the clay in the soil profile indicate restriction of diffuse and focused recharge through soil matrix infiltration, suggesting there are preferential recharge pathways. For the 2018–2020 period, the water table fluctuation method provides recharge estimates of 14-51 mm/year on the left bank, 10-36 mm/year on the right bank and 148-194 mm/year in the riverbed
Nicolas, Madeleine. "Impact de l’hétérogénéité sur la recharge naturelle et artificielle des aquifères cristallins altérés et fracturés : application aux sites de Maheshwaram et Choutuppal (Inde du Sud)". Thesis, Rennes 1, 2019. http://www.theses.fr/2019REN1B016/document.
Pełny tekst źródłaThe factors governing the intensity and distribution of natural and artificial recharge in weathered and fractured crystalline aquifers are poorly understood. However, it is the defining characteristics of this type of rock—these rocks are very heterogeneous—that make the estimation of fluxes and the hydraulic properties controlling them difficult. The first of its two parts provides the theoretical framework on groundwater recharge processes and its estimation methods for comprehending the scientific and societal challenges discussed in this thesis. The second part presents the numerical and experimental work carried out to deepen our understanding of the dynamics of groundwater flows in these heterogeneous underground environments at several scales. The first line of research focuses on natural recharge processes at the watershed scale. Diffuse recharge was modeled with a simple physical infiltration model and compared to previous estimates of total recharge. Our results highlight the strong dependence of recharge on rainfall and irrigation, and the importance of focused recharge. The factors responsible for the spatial distribution of recharge are also studied. The second axis is based on the monitoring of the filling of an artificial recharge basin at a highly monitored and well-equipped site. These observations were interpreted with analytical and numerical models to improve our knowledge of flow dynamics in fractured crystalline rocks at the medium scale. These models illustrated the existence of preferential horizontal flows, but also of a lateral compartmentalization that hinders the propagation of recharge inputs
Jeanpert, Julie. "Structure et fonctionnement hydrogéologiques des massifs de péridotites de Nouvelle-Calédonie". Thesis, La Réunion, 2017. http://www.theses.fr/2017LARE0047/document.
Pełny tekst źródłaWater resources of hard-rock (gneisses or granites) aquifers have significantly been studied in the past two decades. The hydrogeological behavior and structure of these aquifers are thus relatively well understood. On the other hand, aquifers in mantle-type basements, such as peridotites, are poorly studied and understood, mainly because they are not common and of limited extent. In this context, New Caledonia is a great laboratory offering unique opportunity to improve the knowledge of these original types of hydrosystems in tropical climate. Thus, the objective of this thesis is to improve the knowledge of these aquifer systems within weathered peridotites. Firstly, the study focuses on the characterization of the weathered layers of the peridotites composed of, from top to bottom, iron oxides/ferricrete, laterite, coarse saprolite and saprock (ie. top of the bedrock, with up to 20 % of weathered material). More than 60 hydraulic tests are performed and results were compiled with existing data. Mean hydraulic conductivity (K) of laterites is estimated around 1.10-7 m/s while mean value in coarse saprolites and saprock is around 8.10-7 m/s. Heterogeneity of this altered layer is high; K varies between six orders of magnitude and hydraulic head data analysis reveals a hydraulic connection with the deep fractured bedrock. Secondly, the fresh rock part of peridotites is studied. Fracture network analysis is derived from outcrop structural measurements and from the description of about 1000 m of cumulated borehole cores. This work highlights the importance of serpentine network, because of its high density and its critical impact on weathering. Moreover, the observations reveal that hydraulic conductivity decreases with depth within the substratum, due to the vertical decrease of weathered fractures density. These new results allow defining a structural framework of the massifs. It is characterized by a primary decimetrical fracture network closely related to the serpentine network. This network is overprinted by a secondary weathering network which reveals decametric spacing (ca. 30 m) and in places K values of 10-5 m/s. At depth, spacing is hectometrical and fractures are sealed by lithostatic pressure and/or subsequent mineral precipitations. These deca- and hectometric fracture networks, which are also visible on the scale effect of hydraulic conductivity, are primarily vertical and are the result of dissolution instabilities occurring during weathering processes. However, low- angle fractures do occur and allow the percolation of the network. Finally, on the basis of these new results and the integration of all existing data from different massifs a new hydrogeological conceptual model is proposed at the scale of a massif. The model includes a homogeneous lateritic aquitard and a coarse saprolite and saprock aquifer which is about 50 m thick. The bedrock is subdivided into three layers whose hydraulic conductivity decreases from 2.10-7 m/s to 2.10-8 m/s, respectively 50 and 250 m below the aquifer base. Numerical modelling validates this unitary conceptual model and reveals that the saturation of the massifs depends on their morphology. At last, several aspects require further research. The role of the ferricrete layer must be specified and considered in the hydrological model. Moreover, distribution of the fracture network remains to be fully addressed and should be studied with care given the potential development of highly permeable structures that could conform to pseudo-karstic drains. The applied results of this work are available in a “Technical guide” and a “Technical report” of the “HYPERK” CNRT Project
Jaunat, Jessy. "Caractérisation des écoulements souterrains en milieu fissuré par approche couplée hydrologie-géochimie-hydrodynamisme : application au massif de l'Ursuya (Pays Basque, France)". Phd thesis, Université Michel de Montaigne - Bordeaux III, 2012. http://tel.archives-ouvertes.fr/tel-00778427.
Pełny tekst źródłaKsiążki na temat "Fractured weathered rock"
Pilchak, Angela M. Contemporary Musicians. Thomson Gale, 2004.
Znajdź pełny tekst źródłaPilchak, Angela M. Contemporary Musicians: Profiles of the People in Music (Contemporary Musicians). Thomson Gale, 2005.
Znajdź pełny tekst źródłaPilchak, Angela M. Contemporary Musicians: Profiles of the People in Music (Contemporary Musicians). Thomson Gale, 2005.
Znajdź pełny tekst źródłaContemporary Musicians: Profiles of the People in Music (Contemporary Musicians). Thomson Gale, 2004.
Znajdź pełny tekst źródłaPilchak, Angela M. Contemporary Musicians: Profiles Of The People In Music (Contemporary Musicians). Thomson Gale, 2005.
Znajdź pełny tekst źródłaPilchak, Angela M. Contemporary Musicians. Thomson Gale, 2007.
Znajdź pełny tekst źródłaPilchak, Angela M. Contemporary Musicians: Profiles of the People in Music (Contemporary Musicians). Thomson Gale, 2004.
Znajdź pełny tekst źródłaPilchak, Angela M. Contemporary Musicians: Profiles of the People in Music (Contemporary Musicians). Thomson Gale, 2005.
Znajdź pełny tekst źródłaContemporary Musicians: Profiles Of The People In Music (Contemporary Musicians). Thomson Gale, 2005.
Znajdź pełny tekst źródłaPilchak, Angela M. Contemporary Musicians: Profiles Of The People In Music (Contemporary Musicians). Thomson Gale, 2005.
Znajdź pełny tekst źródłaCzęści książek na temat "Fractured weathered rock"
Noland, Scott, i Edward Winner. "Activated Carbon Injection for In-Situ Remediation of Petroleum Hydrocarbons". W Advances in the Characterisation and Remediation of Sites Contaminated with Petroleum Hydrocarbons, 549–89. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-34447-3_16.
Pełny tekst źródła"The conceptual model of weathered hard rock aquifers and its practical applications". W Fractured Rock Hydrogeology, 35–68. CRC Press, 2014. http://dx.doi.org/10.1201/b17016-7.
Pełny tekst źródła"Similarities in groundwater occurrence in weathered and fractured crystalline basement aquifers in the Channel Islands and in Zimbabwe". W Fractured Rock Hydrogeology, 69–82. CRC Press, 2014. http://dx.doi.org/10.1201/b17016-8.
Pełny tekst źródłaR, Abinaya, Antony Ravindran A, Moorthy G.M, Muthusamy S, Vinoth Kingston J i Antony Alosanai Promilton A. "ASSESSMENT OF GROUNDWATER CHARACTERISTIC STUDIES USING THE MAGNETO TELLURIC METHOD IN KALUGUMALAI, TAMIL NADU, INDIA". W Futuristic Trends in Physical Sciences Volume 2 Book 14, 62–69. Iterative International Publishers, Selfypage Developers Pvt Ltd, 2023. http://dx.doi.org/10.58532/v2bs14p1ch7.
Pełny tekst źródłaAdelana, S. "Water pollution by nitrate in a weathered/fractured basement rock aquifer". W Research Basins and Hydrological Planning, 93–98. Taylor & Francis, 2004. http://dx.doi.org/10.1201/9781439833858.ch12.
Pełny tekst źródłaJain, Prabhat, Abhay Soni i Rahul Shende. "Management of Hard Rock Basaltic Aquifer through Aquifer Mapping: A Case Study of Nashik District, Maharashtra, India". W Environmental Sciences. IntechOpen, 2023. http://dx.doi.org/10.5772/intechopen.111644.
Pełny tekst źródłaPower, T., B. J. Smith i W. B. Whalley. "Fracture Patterns and Grain Release in Physically Weathered Granitic Rocks". W Soil Micro-Morphology: A Basic and Applied Science, Proceedings of the VIIIth International Working Meeting of Soil Micromorphology, 545–50. Elsevier, 1990. http://dx.doi.org/10.1016/s0166-2481(08)70371-4.
Pełny tekst źródłaCor, Thomas, Véronique Merrien-Soukatchoff, Damien Rangeard, Céline Rescourio i Jérôme Simon. "Comparisons of different modelling of an excavation realized in fractured and weathered rocks". W Numerical Methods in Geotechnical Engineering, 851–56. CRC Press, 2014. http://dx.doi.org/10.1201/b17017-152.
Pełny tekst źródłaStreszczenia konferencji na temat "Fractured weathered rock"
González, J. A. Mézquita, i J. Comte. "Sensitivity and Uncertainty of Petrophysical Models to Predict Storage Properties in Weathered/Fractured Hard-Rock Aquifers". W 25th European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902380.
Pełny tekst źródłaKumar, Rajeev Ranjan, Sanjoy Kumar Mukherjee, S. K. Biswal, Rajasekar V, Surej Kumar Subbiah, Joseph Zacharia, Rahul Talreja, Atanu Bandyopadhyay i Manish Singh. "Field Scale Geo-Mechanical Analysis To Identify Fracture Sweet Spots Within Deccan Trap, Western Onshore, India". W Offshore Technology Conference. OTC, 2021. http://dx.doi.org/10.4043/31206-ms.
Pełny tekst źródłaKumar, Rajeev Ranjan, Joseph Zacharia, Surej Kumar Subbiah, Rajasekar V, Sanjoy Kumar Mukherjee, Sanjay Lalchand Bagde, P. C. Chaturvedi, K. Vasudevan i B. S. Haldia. "Geomechanics Aided Successful Well Delivery Through Abrasive Rock While Adding New Unconventional Reserves". W Offshore Technology Conference. OTC, 2022. http://dx.doi.org/10.4043/31698-ms.
Pełny tekst źródłaArrofi, Daffa, Israa S. Abu-Mahfouz, Jawad Rafiq, Jarvis R. Cline, Mutaz Al-Jafari i Mohamed Al-Ghamdi. "Natural Fracture Characterization Through Digital Outcrop Model in Southwestern Saudi Arabia Geothermal Field". W International Petroleum Technology Conference. IPTC, 2024. http://dx.doi.org/10.2523/iptc-24657-ea.
Pełny tekst źródłaAl-Marri, Saad Zayed, Gary Peach i Hernan Vigil Fernandez. "TBM Challenges on Musaimeer outfall tunnel". W The 2nd International Conference on Civil Infrastructure and Construction. Qatar University Press, 2023. http://dx.doi.org/10.29117/cic.2023.0017.
Pełny tekst źródłaAadnøy, Bernt S., i Mesfin A. Belayneh. "High Geostress Advantageous for Arctic Field Developments". W ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-78629.
Pełny tekst źródłaCarvalho, Ana, Ricardo Ribeiro, Rui Moura i Alexandre Lima. "GEOPHYSICAL EXPLORATION OF ANTIMONY MINERALIZATIONS: ALTO DO SOBRIDO AND RIBEIRO DA SERRA MINES (PORTUGAL)". W 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/1.1/s03.033.
Pełny tekst źródłaNozaki, M., N. R. Zwarich, M. Prosvirnov, R. Ruysschaert, M. A. Habib i L. A. Johnson. "Completion and Stimulation Design Evolution in Tight Chalk Formations in Offshore Norway". W SPE International Conference and Exhibition on Formation Damage Control. SPE, 2024. http://dx.doi.org/10.2118/217898-ms.
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