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  • 1
    Online Resource
    Online Resource
    Madrid :Instituto Geológico y Minero de España,
    Keywords: Geology. ; Geología. ; Underground storage. ; Almacenamiento subterráneo.,. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (227 pages)
    ISBN: 9781512934434
    DDC: 550
    Language: Spanish
    Note: ATLAS DE ESTRUCTURAS DEL SUBSUELO SUSCEPTIBLES DE ALMACENAMIENTO GEOLÓGICO DE CO2 EN ESPAÑA -- PÁGINA LEGAL -- ÍNDICE -- ZONA 1. CADENA CANTÁBRICA Y CUENCA DEL DUERO -- I. GEOLOGÍA GENERAL -- I.1. Encuadre geológico general -- I.2. Síntes is es tratigráfica-(...) -- I.3. Pares de formación (...) -- I.4. Áreas y estructuras (...) -- II. MAPAS DE ÁREAS Y ESTRUCTURAS (...) -- II.1. Plataforma de (...) -- II.2. Plataforma de (...) -- II.3. Matienzo-Lías (CD-GE-04) -- II.4. Matienzo-Buntsandstein (...) -- II.5. Ancillo (CD-GE-07) -- II.6. Cubeta Oeste (...) -- II.7. Cubeta Oeste de (...) -- II.8. Banda Plegada (...) -- II.9. Banda Plegada de (...) -- II.10. Montes Obarenes (...) -- II.11. Rioja Norte (CD-GE-24) -- II.12. Rioja Sur (CD-GE-25) -- II.13. Iglesias-Cretácico (...) -- II.14. Iglesias-Utrillas (...) -- II.15. Iglesias-Jurásico (...) -- II.16. Iglesias-Buntsandstein (...) -- II.17. Duero C entro-meridional (...) -- II.18. Duero C entro-meridional (...) -- II.19. Don Juan E ste (...) -- II.20. Don Juan Este- (...) -- II.21. Don Juan Este (...) -- II.22. Don Juan Este (...) -- II.23. Don Juan Oeste (...) -- II.24. Don Juan Oeste (...) -- II.25. Don Juan Oeste (...) -- II.26. Honrubia-Nieva (...) -- II.27. Honrubia-Nieva (...) -- II.28. San Pedro (CD-GF-01) -- II.29. El Campillo (CD-GF-02) -- II.30. Boñar (CD-GF-03) -- II.31. Villameriel (CD-GF-04) -- II.32. Hontomín (CD-GF-05) -- II.33. Miranda de Ebro (CD-GF-06) -- II.34. Ribero (CD-GF-07) -- ZONA 2. CADENA PIRENAICA Y CUENCA DEL EBRO -- I. GEOLOGÍA GENERAL -- I.1. Encuadre geológico general -- I.2. Síntesis estratigráfica-(...) -- I.3. Pares de formación (...) -- I.4. Áreas y estructuras (...) -- II. MAPAS DE ÁREAS Y ESTRUCTURAS (...) -- II.1. Zuera (pe-ge-01) -- II.2. Sariñena (pe-ge-02) -- II.3. Arnedo (pe-ge-03) -- II.4. Magallón (pe-ge-04) -- II.5. Zona de enlace-(...). , II.6. Zona de enlace(...) -- II.7. Olsón (PE-GE-07) -- II.8. B (PE-GE-08) -- II.9. Santa creu-graus(PE-GE-09) -- II.10. Tamurcia (PE-GE-10) -- II.11. Sierras marginales (...) -- II.12. Isona (PE-GE-12) -- II.13. Roncal (...) -- II.14. Leyre-berdún (...) -- II.15. Lopín (PE-GF-01) -- II.16. Monegrillo (PE-GF-02) -- ii.17. Caspe-mayals (pe-gf-03) -- ii.18. Reus (pe-gf-04) -- ii.19. Centenera (pe-gf-05) -- ZONA 3. CADENA IBÉRICA Y CUENCAS DEL (...) -- I. GEOLOGÍA GENERAL -- I.1. Encuadre (...) -- I.2. Síntesis (...) -- i.3. Pares de formación (...) -- I.4. Áreas y estructuras (...) -- II. MAPAS DE ÁREAS Y (...) -- II.1. Salsadella (it-ge-01) -- II.2. dDlta del ebro-1 (it-ge-02) -- II.3. Delta del ebro-2 (it-ge-03) -- II.4. Baides-1 (it-ge-04) -- II.5. Baides-2 (IT-GE-05) -- II.6. Tielmes-1 (it-ge-06) -- II.7. Telmes-2 (it-ge-07) -- II.8. Altomira (it-ge-08) -- II.9. Tribaldos (it-ge-09) -- II.10. Almazán septentrional (...) -- II.11. Almazán septentrional (...) -- II.12. Gormaz (IT-GE-12 -- II.13. Burgo de osma (it-ge-13) -- II.14. La ventosa (it-ge-14) -- ii.15. Obón-oliete (it-ge-15) -- ii.16. Belmontejo 1 (it-ge-16) -- II.17. Belmontejo 2 (it-ge-17) -- II.18. Gabaldón (it-ge-18) -- II.19. El hito (IT-GE-19) -- II.20. Tres cantos-s.s. de (...) -- II.21. puerta pareja (it-gf-02) -- II.22. cuenca de almazán (...) -- II.23. Maestrazgo-1 (it-gf-04) -- II.24. Maestrazgo-2 (it-gf-05) -- II.25. Maestrazgo-3 (it-gf-06) -- ZONA 4. CADENAS BÉTICAS Y CUENCA (...) -- I. GEOLOGÍA GENERAL -- I.1. Encuadre geológico general -- I.2. Síntesis estratigráfica-(...) -- I.3. Pares de formación (...) -- I.4. Áreas y estructuras (...) -- II. MAPAS DE ÁREAS Y (...) -- II.1. Río guadalquivir (...) -- II.2. Alto guadalquivir (...) -- II.3. Guadiana menor (bg-ge-03) -- II.4. Sinclinal de pétrola (...) -- II.5. Sierra de benejama (...) -- II.6. Sierra de salinas (bg-ge-06). , II.7. La macaroba (...) -- II.8. Murcia b-1/río segura (...) -- II.9. Sierra seca (bg-ge-09) -- II.10. Plataforma tabular de (...) -- II.11. Almonte (bg-gf-01) -- II.12. Campo de gibraltar (...) -- II.13. Fuensanta (bg-gf-03) -- II.14. Río guadalquivir h-1 (bg-gf-04) -- II.15. Benejúzar-rojales (bg-gf-05).
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 89 (1985), S. 4809-4814 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 95 (1991), S. 7338-7344 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 97 (1992), S. 6309-6321 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: The reaction rates of the muonium (Mu) atom with HBr and HI in ∼1 atm N2 moderator have been measured over the temperature range 160–490 K using the μSR technique. While both abstraction and exchange reactions are possible, only the abstraction reaction should be observable, being moderately exothermic. Comparisons with the corresponding H(D) reactions reveal small kinetic isotope effects in both reactions, which do not vary strongly with temperature (kMu/kH≈3.5 near 300 K), consistent with the (classical) ratio of mean velocities. Surprisingly, quantum tunneling, normally facile for similarly exothermic reactions of the ultralight Mu atom (mMu/mH≈1/9), appears to be of little importance here. This despite the fact that the (temperature-independent) experimental activation energies are much less than the expected vibrationally adiabatic barrier heights (estimated to be ≈1.5 kcal mol−1) and, particularly in the case of Mu+HI, much less than the corresponding H-atom activation energy: 0.13±0.03 vs 0.70±0.3 kcal mol−1. In the case of reactions with HBr, the experimental Mu- and H-atom activation energies are much more similar: 0.51±0.03 and 0.74±0.12 kcal mol−1, respectively, over comparable temperature ranges. These data pose a conundrum in which several compensating effects related to the much lighter Mu-atom mass seem to be involved. Theoretical calculations are urgently required.In our view the topography of the potential-energy surface(s) for H2X is poorly known, particularly in the region of the barrier. It may be that the abstraction barriers for both Mu+HI and Mu+HBr are considerably later and even smaller than current calculations indicate, resulting in a cancellation of the effects of zero-point-energy shifts and quantum tunneling at the transition state. Differences in skewing angles between Mu and H+HX could favor a shorter tunneling path for the H-atom reaction, possibly compensating for its heavier mass. Steric or rebound effects from "bottlenecks'' on the (mass-weighted) potential surfaces for Mu reactivity may also play some role. An upper limit for the 300 K reaction rate of Mu+HCl is given as well. In contrast to both HBr and HI, this reaction is quite endothermic and hence exhibits an inverse kinetic isotope effect (kMu(very-much-less-than)kH).
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: Muon polarizations are reported for nitrogen and ethane over a wide pressure range from below 1 to 200 atm for N2 and up to 245 atm for C2H6. The N2 measurements were made at ambient temperature, while those for C2H6 were made at temperatures both above and below the critical temperature (305.3 K). This is the first μSR study of muonium and diamagnetic muon formation to cover the entire range from a low pressure gas to densities typical of liquids. The data are discussed in terms of hot atom and spur models. In the lowest pressure range, below 1.5 atm for N2 and about 10 atm for C2H6, the muonium polarization increases with pressure. This is well understood in terms of epithermal charge exchange. In N2 there is a small diamagnetic fraction, which is ascribed to the N2Mu+ molecular ion. This fraction approaches zero as the pressure is increased to 200 atm, with a corresponding increase in the muonium fraction, consistent with charge neutralization of the molecular ion by electrons from the radiolysis track. In C2H6, there is a decrease in the muonium fraction and a concomitant increase of the diamagnetic fraction with density, the changes occurring in two stages. The initial change is explained by stabilization of the vibrationally excited substitution products of hot muonium reactions. The second one is explained by proton transfer from the molecular ion adduct, C2H6Mu++C2H6→C2H5Mu+C2H+7, trapping the muon in a diamagnetic product. Both N2 and C2H6 have a missing fraction of polarization above 10 atm, most likely due to spin exchange of Mu with paramagnetic species created in the muon track. In N2, the missing fraction is recovered at pressures beyond about 150 atm, which is explained by scavenging of electrons by positive ions. In C2H6 the missing fraction is roughly constant for densities beyond 5 mol l−1 (≈50 atm), and about twice the maximum found for N2. Both facts are consistent with the existence of ethyl radicals and hydrogen atoms in C2H6, which are longer lived than the spur electrons.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 91 (1989), S. 6164-6176 
    ISSN: 1089-7690
    Source: AIP Digital Archive
    Topics: Physics , Chemistry and Pharmacology
    Notes: Bimolecular rate constants for the thermal chemical reactions of muonium (Mu) with the halogen gases—Mu+X2→MuX+X—are reported over the temperature ranges from 500 down to 100, 160, and 200 K for X2=F2,Cl2, and Br2, respectively. The Arrhenius plots for both the chlorine and fluorine reactions show positive activation energies Ea over the whole temperature ranges studied, but which decrease to near zero at low temperature, indicative of the dominant role played by quantum tunneling of the ultralight muonium atom. In the case of Mu+F2, the bimolecular rate constant k(T) is essentially independent of temperature below 150 K, likely the first observation of Wigner threshold tunneling in gas phase (H atom) kinetics. A similar trend is seen in the Mu+Cl2 reaction. The Br2 data exhibit an apparent negative activation energy [Ea=(−0.095±0.020) kcal mol−1], constant over the temperature range of ∼200–400 K, but which decreases at higher temperatures, indicative of a highly attractive potential energy surface. This result is consistent with the energy dependence in the reactive cross section found some years ago in the atomic beam data of Hepburn et al. [J. Chem. Phys. 69, 4311 (1978)]. In comparing the present Mu data with the corresponding H atom kinetic data, it is found that Mu invariably reacts considerably faster than H at all temperatures, but particularly so at low temperatures in the cases of F2 and Cl2. The current transition state calculations of Steckler, Garrett, and Truhlar [Hyperfine Interact. 32, 779 (986)] for Mu+X2 account reasonably well for the rate constants for F2 and Cl2 near room temperature, but their calculated value for Mu+Br2 is much too high. Moreover, these calculations seemingly fail to account for the trend in the Mu+F2 and Mu+Cl2 data toward pronounced quantum tunneling at low temperatures. It is noted that the Mu kinetics provide a crucial test of the accuracy of transition state treatments of tunneling on these early barrier HX2 potential energy surfaces.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 99 (1995), S. 16960-16966 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 99 (1995), S. 17160-17168 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 95 (1991), S. 8423-8425 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1365-2958
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Medicine
    Notes: It is accepted that Saccharomyces cerevisiae genome arose from complete duplication of eight ancestral chromosomes; functionally normal ploidy was recovered because of the massive loss of 90% of duplicated genes. There is evidence that indicates that part of this selective conservation of gene pairs is compelling to yeast facultative metabolism. As an example, the duplicated NADP-glutamate dehydrogenase pathway has been maintained because of the differential expression of the paralogous GDH1 and GDH3 genes, and the biochemical specialization of the enzymes they encode. The present work has been aimed to the understanding of the regulatory mechanisms that modulate GDH3 transcriptional activation. Our results show that GDH3 expression is repressed in glucose-grown cultures, as opposed to what has been observed for GDH1, and induced under respiratory conditions, or under stationary phase. Although GDH3 pertains to the nitrogen metabolic network, and its expression is Gln3p-regulated, complete derepression is ultimately determined by the carbon source through the action of the SAGA and SWI/SNF chromatin remodelling complexes. GDH3 carbon-mediated regulation is over-imposed to that exerted by the nitrogen source, highlighting the fact that operation of facultative metabolism requires strict control of enzymes, like Gdh3p, involved in biosynthetic pathways that use tricarboxylic acid cycle intermediates.
    Type of Medium: Electronic Resource
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