SwePub
Sök i SwePub databas

  Utökad sökning

Träfflista för sökning "WFRF:(Dubrovinsky L) srt2:(2000-2004)"

Sökning: WFRF:(Dubrovinsky L) > (2000-2004)

  • Resultat 1-29 av 29
Sortera/gruppera träfflistan
   
NumreringReferensOmslagsbildHitta
1.
  •  
2.
  • Cerenius, Y, et al. (författare)
  • Compressibility measurements on iridium
  • 2000
  • Ingår i: JOURNAL OF ALLOYS AND COMPOUNDS. - : ELSEVIER SCIENCE SA. - 0925-8388. ; 306:1-2, s. 26-29
  • Tidskriftsartikel (refereegranskat)abstract
    • The compressibility of iridium was determined by energy-dispersive X-ray diffraction and synchrotron radiation up to a pressure of 65 GPa in the diamond-anvil cell. The bulk modulus (B-0) was determined to be B-0,=306 (23) with B-0'=6.8 (1.5) when using a
  •  
3.
  •  
4.
  •  
5.
  •  
6.
  • Dubrovinsky, L., et al. (författare)
  • Iron-silica interaction at extreme conditions and the electrically conducting layer at the base of Earth's mantle
  • 2003
  • Ingår i: Nature. - : Springer Science and Business Media LLC. - 0028-0836 .- 1476-4687. ; 422:6927, s. 58-61
  • Tidskriftsartikel (refereegranskat)abstract
    • The boundary between the Earth's metallic core and its silicate mantle is characterized by strong lateral heterogeneity and sharp changes in density, seismic wave velocities, electrical conductivity and chemical composition(1-7). To investigate the composition and properties of the lowermost mantle, an understanding of the chemical reactions that take place between liquid iron and the complex Mg-Fe-Si-Al-oxides of the Earth's lower mantle is first required(8-15). Here we present a study of the interaction between iron and silica (SiO2) in electrically and laser-heated diamond anvil cells. In a multianvil apparatus at pressures up to 140 GPa and temperatures over 3,800 K we simulate conditions down to the core-mantle boundary. At high temperature and pressures below 40 GPa, iron and silica react to form iron oxide and an iron-silicon alloy, with up to 5 wt% silicon. At pressures of 85-140 GPa, however, iron and SiO2 do not react and iron-silicon alloys dissociate into almost pure iron and a CsCl-structured (B2) FeSi compound. Our experiments suggest that a metallic silicon-rich B2 phase, produced at the core-mantle boundary (owing to reactions between iron and silicate(2,9,10,13)), could accumulate at the boundary between the mantle and core and explain the anomalously high electrical conductivity of this region(6).
  •  
7.
  •  
8.
  •  
9.
  • Dubrovinsky, L, et al. (författare)
  • Pressure-induced invar effect in Fe-Ni alloys
  • 2001
  • Ingår i: PHYSICAL REVIEW LETTERS. - 0031-9007. ; 86:21, s. 4851-4854
  • Tidskriftsartikel (refereegranskat)abstract
    • We have measured the pressure-volume (P-V) relations for cubic iron-nickel alloys for three different compositions: Fe0.64Ni0.36, Fe0.55Ni0.45, and Fe0.20Ni0.80. It is observed that for a certain pressure range the bulk modulus does not change or can even
  •  
10.
  • Dubrovinsky, L. S., et al. (författare)
  • Materials science - The hardest known oxide
  • 2001
  • Ingår i: Nature. - : Springer Science and Business Media LLC. - 0028-0836 .- 1476-4687. ; 410:6829, s. 653-654
  • Tidskriftsartikel (refereegranskat)
  •  
11.
  •  
12.
  • Dubrovinsky, L, et al. (författare)
  • Stability of (Mg0.5Fe0.5)O and (Mg0.8Fe0.2)O magnesiowustites in the lower mantle
  • 2001
  • Ingår i: EUROPEAN JOURNAL OF MINERALOGY. - : E SCHWEIZERBARTSCHE VERLAGS. - 0935-1221. ; 13:5, s. 857-861
  • Tidskriftsartikel (refereegranskat)abstract
    • We have heated magnesiowtistites (Mg0.5Fe0.5)O and (Mg0.8Fe0.2)O to temperatures of over 1000 K at pressures of over 80 GPa simulating the stability of the solid solution at physical conditions relevant to the Earth's lower mantle. The X-ray study of the
  •  
13.
  •  
14.
  • El, Goresy A, et al. (författare)
  • A monoclinic post-stishovite polymorph of silica in the Shergotty meteorite
  • 2000
  • Ingår i: SCIENCE. - : AMER ASSOC ADVANCEMENT SCIENCE. - 0036-8075. ; 288:5471, s. 1632-1634
  • Tidskriftsartikel (refereegranskat)abstract
    • A post-stishovite phase of silica was identified in the Shergotty meteorite by x-ray diffraction and field emission scanning electron microscopy. The diffraction pattern revealed a monoclinic Lattice, similar to the baddeleyite-structured polymorph with t
  •  
15.
  • El, Goresy A, et al. (författare)
  • An ultradense polymorph of rutile with seven-coordinated titanium from the Ries crater
  • 2001
  • Ingår i: SCIENCE. - : AMER ASSOC ADVANCEMENT SCIENCE. - 0036-8075. ; 293:5534, s. 1467-1470
  • Tidskriftsartikel (refereegranskat)abstract
    • We report the discovery of an ultradense post-rutile polymorph of titanium dioxide in shocked gneisses of the Ries crater in Germany. The microscopic diagnostic feature is intense blue internal reflections in crossed polarizers in reflected light. X-ray d
  •  
16.
  • Gillet, P, et al. (författare)
  • Natural NaAlSi3O8-hollandite in the shocked Sixiangkou meteorite
  • 2000
  • Ingår i: SCIENCE. - : AMER ASSOC ADVANCEMENT SCIENCE. - 0036-8075. ; 287:5458, s. 1633-1636
  • Tidskriftsartikel (refereegranskat)abstract
    • The hollandite high-pressure polymorph of plagioclase has been identified in shock-induced melt veins of the Sixiangkou 16 chondrite. It is intimately intergrown with feldspathic glass within grains previously thought to be "maskelynite." The crystallogra
  •  
17.
  •  
18.
  • Mattesini, M., et al. (författare)
  • Cubic TiO2 as a potential light absorber in solar-energy conversion
  • 2004
  • Ingår i: Physical Review B. Condensed Matter and Materials Physics. - 1098-0121 .- 1550-235X. ; 70:11
  • Tidskriftsartikel (refereegranskat)abstract
    • Materials are currently sought for use in the photo-induced decomposition of water on crystalline electrodes. Titanium dioxide is valuable in this respect. The electronic structural properties of cubic TiO2 polymorphs were investigated by means of first-principles methods. We demonstrate that both fluorite- and pyrite-type TiO2 have important optical absorptive transitions in the region of the visible light. A cubic TiO2 phase that can efficiently absorb the sunlight would be an important candidate material for the development of the solar cells. Also, we present results on the Ti L edges for the two different titania forms. We predict that a qualitative spectroscopic discrimination of the cubic polymorphs can be achieved by following the Ti 2p → 3d x-ray transitions.
  •  
19.
  •  
20.
  •  
21.
  •  
22.
  •  
23.
  • Talyzin, Alexandre, et al. (författare)
  • High pressure Raman study of C60S16
  • 2002
  • Ingår i: Solid State Communications. ; 123:3-4, s. 93-96
  • Tidskriftsartikel (refereegranskat)
  •  
24.
  •  
25.
  •  
26.
  •  
27.
  •  
28.
  • Talyzin, A V, et al. (författare)
  • Superhard and superelastic films of polymeric C60
  • 2001
  • Ingår i: Diamond and related materials. - 0925-9635 .- 1879-0062. ; 10:11, s. 2044-2048
  • Tidskriftsartikel (refereegranskat)abstract
    • The C60 thin film deposited on steel substrate was transformed by high pressure-high temperature treatment to a superhard and superclastic material. The films were studied by Raman spectroscopy in situ at 20 GPa after heating at 300░C and ex situ after the quenching. The hardness and elastic properties of the high-pressure phases have been characterized with nanoindentation. The hardness of the films were determined to be 0.5 ▒ 0.1 GPa and 61.9 ▒ 9 GPa for unmodified C60 and HPHT treated films, respectively. The hardness of the pressurized film is higher than for cubic BN but lower than hardness values reported for ultrahard fullerite samples prepared from powders. An interesting observation was that the HPHT treated film showed an extreme elastic response with an elastic recovery of approximately 90%. ⌐ 2001 Elsevier Science B.V. All rights reserved.
  •  
29.
  • Tutti, F., et al. (författare)
  • Stability of KAlSi3O8 hollandite-type structure in the earth's lower mantle conditions
  • 2001
  • Ingår i: Geophysical Research Letters. - 0094-8276. ; 28:14, s. 2735-2738
  • Tidskriftsartikel (refereegranskat)abstract
    • The stability of KAISi3O8 hollandite-type structure is investigated in a series of synthesis experiments between 20 and 95 GPa at 650(±50) °C and between 1200 to 2300 °C, using electrically- and laser-heated diamond anvil cells, respectively. Potassium feldspar transformed to a hollandite-type structure in the experimental pressure range from 20 to 95 GPa at temperatures between 1200 to 2300 °C, whereas it remained amorphous at 65(±5) GPa and 650(±50) °C. KAISi3O8 hollandite is, therefore, a stable phase under the pressure and temperature conditions of at least 2200 km deep in the lower mantle and could be an important host for potassium in that region.
  •  
Skapa referenser, mejla, bekava och länka
  • Resultat 1-29 av 29

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy