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21.
Problems of site selection for nuclear waste disposal in a loess-covered hill environment in Hungary
Problems of the long-term storage of nuclear waste produced by the Paks power plant have recently come to the fore in Hungary. After an extensive debate between investors and the local population the decision makers took the side of those having opposed the establishment of the waste disposal site in the initially proposed environment. Several studies have been conducted to support both pros and cons. Although the idea was rejected finally, this debate has proven that comprehensive research prior to decision making is indispensable in similar cases.Regretfully, the academic staff of the GRIHAS was invited to participate in the expertise too late, in 1988, to investigate the geomorphological and social-economic environmental conditions of the proposed site. The latter cannot be neglected since the settlement pattern, demographic structure, character of economic activities, the level and state of the infrastructure — though indirectly — exert a long-term impact on the circumstances of the operation of the site, the living conditions of the people working there and on the use of the environment. Any harmful effect from the secondary wastes to be deposited could endanger the security of the local population, that is why a thorough geographical analysis based on field research in the immediate and wider surroundings of the site is necessary already in the phase of decision preparation. 相似文献
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Robert E. Ulanowicz John M. Lindsay William C. Caplins Tibor T. Polgar 《Estuaries and Coasts》1982,5(1):57-67
Previous simulations of potential ichthyoplankton entrainment by power generating stations on the Potomac estuary have not included the influence of lateral transport in distributing eggs and larvae over the nursery area. Therefore, two-dimensional, vertically-averaged hydrodynamic and kinematic models of passive organism transport were developed to represent advective and dispersive processes near the proposed Douglas Point Nuclear Generating Station. Although the more refined model did not substantially alter the estimate of ichthyoplankton entrainment, it did reveal that lateral inhomogeneities in hydrodynamics could engender severalfold differences in entrainment probabilities on opposite sides of the estuary. Models of higher resolution and greater biological detail did not project greater total entrainment by the Douglas Point plant, because the volume of nontidal flow past the site was large in comparison to the proposed rate of cooling water withdrawal. 相似文献
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Slávo Chalupka Tibor Kolbenheyer Reviewer V. Vyskočil 《Studia Geophysica et Geodaetica》1972,16(4):339-343
Summary The Fourier transform of the vertical component of the attraction of a homogeneous horizontal infinite elliptical cylinder is computed. By comparing this function with the Fourier transform of the vertical component, determined experimentally, it is possible to determine the mass of the cylinder per unit length, as well as the position of the centre and of both the foci of the ellipse representing the cross-section of the cylinder.Decicated to Academician Alois Zátopek on His 65th Birthday 相似文献
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Anne R. Remsberg James N. Boland Tibor Gasparik Robert C. Liebermann 《Physics and Chemistry of Minerals》1988,15(5):498-506
An experiment conducted in a 2000-ton uniaxial split-sphere apparatus (USSA-2000) utilizes large sample volume and a substantial temperature gradient to synthesize intergrowths of the olivine and spinel polymorphs of Co2SiO4. The olivine starting material consists of a finegrained fraction (<20μm) which records the stable polymorphs along the length of the sample plus large olivine grains (100–500 μm) which help decipher the mechanism of the phase transformation. At conditions near equilibrium, the olivine-spinel transformation in the large grains occurs by inward growth of a few large single crystals of spinel nucleated on the surfaces of the olivine. The overall rate of transformation is governed by the mobility of the interphase boundary, whose morphology is crystallographically controlled by the spinel. No renucleation of spinel is observed in the host olivine crystal, even in the region immediately adjacent to the olivine/spinel interface; analysis of this region with transmission electron microscopy reveals an extremely high density of dislocations induced by plastic flow accommodating the volume change associated with the phase transformation. 相似文献
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Tibor Gasparik 《Geochimica et cosmochimica acta》1985,49(5):1277-1279
Solubility of Ti4+ in ureyite (cosmochlor, NaCrSi2O6) was experimentally studied at 1 atmosphere and ≈1000°C, using sodium disilicate as flux. Microprobe analyses indicate that at low titanium concentrations the substitution of titanium in ureyite is almost exclusively in the M1 site, coupled with a vacancy in the M2 site. At higher TiO2 contents, a small additional amount enters the tetrahedral site. If the solubility of titanium is similar in jadeite and acmite, the □TiSi2O6 substitution could contribute significantly to the vacancy content of natural titanium bearing omphacites. 相似文献
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The study has been carried for visual discrimination of natural salt affected soils on FCC images of IRS 1 B in Pali district of Rajasthan. The salt affected soils show wide variations in salinity (EC2.53.7 to 28 dSm-1), alkalinity (pH 8.5-9.8), cover ofP. juliflora (10-90%), salt tolerant grasses (10–55%) and gravelly surface (20–35%). ThoughP. juliflora and grasses were present at most of the observation points their cover decreased with soil EC2.5 values more than 10 and 13 dSm-1, respectively. Five darkness categories derived as the result of visual interpretation of FCCs; and ground and laboratory studies revealed that the darkness category 1 represented fewer plant community with high salinity (EC 28.7 dSm-1) and gravelly surface, categories 2 and 3 were characterised by grass cover and moderate salt affected soils (EC 3-10 dSm-1) whereas category 4 was dominated by thicket ofP. juliflora. The derived numerical darkness categories of the FCC images were slightly low for February images. The darkness values of observation pixel on February images correlated positively withP. juliflora cover and negatively with grass cover and soil pH indicating that surface features on FCC were related with the immediate observation pixels. 相似文献
28.
Omri Gadol Gideon Tibor Uri ten Brink John K. Hall Gavrielle Groves-Gidney Gideon Bar-Am Christian Hübscher Yizhaq Makovsky 《Basin Research》2020,32(5):1156-1183
Understanding continental-slope morphological evolution is essential for predicting basin deposition. However, separating the imprints and chronology of different seafloor shaping processes is difficult. This study explores the utility of bathymetric spectral decomposition for separating and characterizing the variety of interleaved seafloor imprints of mass wasting, and clarifying their role in the morphological evolution of the southeastern Mediterranean Sea passive-margin slope. Bathymetric spectral decomposition, integrated with interpretation of seismic profiles, highlights the long-term shape of the slope and separates the observed mass transport elements into several genetic groups: (1) a series of ~25 km wide, now-buried slide scars and lobes; (2) slope-parallel bathymetric scarps representing shallow faults; (3) slope-perpendicular, open slope slide scars; (4) bathymetric roughness representing debris lobes; (5) slope-confined gullies. Our results provide a multi-scale view of the interplay between sediment transport, mass transport and shallow faulting in the evolution of the slope morphology. The base of the slope and focused disturbances are controlled by ~1 km deep salt retreat, and mimic the Messinian base of slope. The top of the open-slope is delimited by faults, accommodating internal collapse of the margin. The now-buried slides were slope-confined and presumably cohesive, and mostly nucleated along the upper-slope faults. Sediment accumulations, infilling the now-buried scars, generated more recent open-slope slides. These latter slides transported ~10 km3 of sediments, depositing a significant fraction (~3 m in average) of the sediments along the base of the studied slope during the past < 50 ka. South to north decrease in the volume of the open-slope slides highlight their role in counterbalancing the northwards diminishing sediment supply and helping to maintain a long-term steady-state bathymetric profile. The latest phase slope-confined gullies were presumably created by channelling of bottom currents into slide-scar depressions, possibly establishing incipient canyon headword erosion. 相似文献
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