A5033097331- Particle physics theoretical and experimental studies
- High-Energy Particle Collisions Research
- Quantum Chromodynamics and Particle Interactions
- Particle Detector Development and Performance
- Dark Matter and Cosmic Phenomena
- Cosmology and Gravitation Theories
- Neutrino Physics Research
- Computational Physics and Python Applications
- Groundwater flow and contamination studies
- Black Holes and Theoretical Physics
- Hydrocarbon exploration and reservoir analysis
- Astrophysics and Cosmic Phenomena
- Reservoir Engineering and Simulation Methods
- Hydraulic Fracturing and Reservoir Analysis
- Distributed and Parallel Computing Systems
- Radiation Detection and Scintillator Technologies
- Geological formations and processes
- Groundwater and Isotope Geochemistry
- Medical Imaging Techniques and Applications
- Geological Formations and Processes Exploration
- Hungarian Social, Economic and Educational Studies
- Particle Accelerators and Free-Electron Lasers
- Seismic Imaging and Inversion Techniques
- Magnetic properties of thin films
- Geophysical and Geoelectrical Methods
Centre de physique des particules de Marseille
2017-2024
Aix-Marseille Université
2015-2024
Centre National de la Recherche Scientifique
2014-2023
HUN-REN Wigner Research Centre for Physics
2014-2023
Institute for Particle and Nuclear Physics
2014-2023
Institut National de Physique Nucléaire et de Physique des Particules
2012-2023
University of North Carolina at Chapel Hill
2022-2023
Sapientia Hungarian University of Transylvania
2023
Corvinus University of Budapest
2023
The University of Adelaide
2013-2022
Theoretically, three types of flow systems may occur in a small basin: local, intermediate, and regional. The local are separated by subvertical boundaries, the different order subhorizontal boundaries. higher topographic relief, greater is importance systems. lines large unconfined do not cross major features. Stagnant bodies groundwater at points where meet or branch. Recharge discharge areas alternate; thus only part basin will contribute to baseflow its main stream. Motion sluggish nil...
On the basis of parallel pattern water divides and valleys in parts central Alberta inferred difference permeability between Paskapoo Edmonton formations, basins are considered to be separate units flow groundwater regime. For cross-sectional distribution fluid potential a basin homogeneous lithology an equation is found that relates acceleration gravity, topographic gradient valley flank, horizontal distance divide bottom, elevation table at bottom above impermeable boundary, from bottom....
The design and construction of the silicon strip microvertex detector (SMD) L3 experiment at LEP are described. We present sensors, readout electronics, data acquisition system, mechanical assembly support, displacement monitoring systems radiation system recently installed double-sided, double-layered SMD. This utilizes novel sophisticated techniques for its readout.
Three zones of different generations formation‐fluid flow systems were identified from analyses the potentiometric surface, hypsographic distribution fresh water heads, pressure‐depth relations, table elevations, and dynamic pressure increments observed in five extensive water‐bearing units a 20,400‐mi 2 (52,840 km ) geologically mature area northern Alberta. In each zone, fluids move gravity‐induced maintained by cross‐formational energy transfer subject to past or present boundary...
Abstract The ≈ 40 000 km 2 Hungarian Great Plain portion of the Pannonian Basin consists a basin fill 100 m to more than 7000 thick semi‐ unconsolidated marine, deltaic, lacustrine and fluviatile clastic sediments Neogene age, resting on strongly tectonized Pre‐Neogene basement horst‐and‐graben topography relief in excess 5000 m. is built great variety brittle rocks, including flysch, carbonates metamorphics. relatively continuous Endrőd Aquitard, with permeability less 1 md (10 −15 ) depth...
ABSTRACT On the basis of degree mineralization, approximately 40 percent ground water in Ross Creek Basin may be considered as fresh (TDS < 2,000 ppm), and 60 brackish (2,000 TDS 10,000 ppm). At least 70 is potable within treatable limits. Major ion analyses over 167 samples reveal a strikingly consistent regional pattern hydrochemistry. The hydrochemical correlates with flow basin. Low total dissolved solids contents, high Ca 2+ :Mg ratio, low SO 4 2− , HCO 3 − occur recharge areas,...
The quality analysis of well-logging inversion results has always been an important part formation evaluation. precise calculation hydrocarbon reserves requires the most accurate possible estimation porosity, water saturation, and shale rock-matrix volumes. local method conventionally used to predict above model parameters depth by represents a marginally overdetermined inverse problem, which is rather sensitive uncertainty observed data limited in accuracy. To reduce harmful effect noise on...
$^{57}\mathrm{Fe}$ absorption and $^{57}\mathrm{Co}$ emission M\"ossbauer spectroscopy was applied to iron- cobalt-doped ${\mathrm{YBa}}_{2}$(${\mathrm{Cu}}_{1\mathrm{\ensuremath{-}}\mathrm{x}}$${\mathrm{M}}_{\mathrm{x}}$${0}_{3}$${\mathrm{O}}_{7\mathrm{\ensuremath{-}}\mathit{y}}$ high-temperature superconductors (M${=}^{57}$Fe, $^{57}\mathrm{Co}$; 3.5\ifmmode\times\else\texttimes\fi{}${10}^{\mathrm{\ensuremath{-}}5}$\ensuremath{\le}x\ensuremath{\le}0.1, y=0 y=0.8) between 4.2 295 K with...
Abstract Four natural conditions co-exist inherently with the hydraulic discharge of groundwater: positive gradient fluid potential, low relative topographic position, allochthonous water quality, and temperature. In turn, these are consistently associated springs, seepages, quicksand, soap holes, geysers, frost mounds, pingos, groundwater lakes marshes, certain near-surface surface accumulations salts, landslides, slumps, soil creep gullying, which is considered as an indication that...
ABSTRACT Theoretically, a small drainage basin may be divided into equal areas of downward flow and upward groundwater. In regions where surface water does not obscure the phenomena produced by groundwater, these can differentiated mapping springs, seepages, groundwater levels, flowing wells, chemical quality water, natural vegetation, salt precipitates, crops, soap holes, moist dry depressions. Mapping interpretation field have been carried out in section Ghostpine Creek valley Prairie...