331 research outputs found
Lithogenesis role in formation of zones with improved reservoir properties of subsalt carbonate sediments of venda and lower cambrian (Eastern Siberia)
The object of research is pre-salt deposits of carbonate complexes from Vendian and Lower Cambrian Nepa-Botuobiya anteclise (NBA), located in the central part of the Siberian platform, administratively dedicated to the Irkutsk region.
The problems of fluid dynamics within the basement ledges are considered. Their role in the high productivity of overlying carbonate deposits is assessed. Reconstruction of sedimentation conditions and subsequent diagenesis and katagenesis of Nepa formation sediments is made that have the greatest impact on morphostructure of the sedimentary cover. Cuts of Vendian-Cambrian sediments before and after diagenesis and katagenesis are given. Detailed construction helped to establish antiform structure of the sedimentary cover deposition over the basement ledges, allowing visually see in retrospect a sediment`s restructuring and its influence on the formation of hydrocarbon traps. The information on the rising pore pressure within the ledges is provided, due to which there is a subvertical fluid migration through both sulfate-carbonate rocks and interformational mudstones which to the beginning of elysion processes in Nepa formation were also unlithified porous sediments. It is suggested that the most permeable zones in the sulfate-carbonate rocks were formed over the edge portions of the projections as the most deformed during compaction of sand and clay deposits Nepa formation and restructuring of the upper section of the sedimentary cover. It is suggested that the elysion stage of sedimentary basin development within ledges and arched structure of Vendian-Cambrian deposits leads to dissolution and mobilization by aqueous solutions of the sedimentary rocks substance at depth and their migration mostly up. The results outlined in this paper are supported by the core data analysis
Optical detection of a single rare-earth ion in a crystal
Rare-earth-doped laser materials show strong prospects for quantum information storage and processing, as well as for biological imaging, due to their high-Q 4fβ4f optical transitions. However, the inability to optically detect single rare-earth dopants has prevented these materials from reaching their full potential. Here we detect a single photostable Pr(3+) ion in yttrium aluminium garnet nanocrystals with high contrast photon antibunching by using optical upconversion of the excited state population of the 4fβ4f optical transition into ultraviolet fluorescence. We also demonstrate on-demand creation of Pr(3+) ions in a bulk yttrium aluminium garnet crystal by patterned ion implantation. Finally, we show generation of local nanophotonic structures and cell death due to photochemical effects caused by upconverted ultraviolet fluorescence of praseodymium-doped yttrium aluminium garnet in the surrounding environment. Our study demonstrates versatile use of rare-earth atomic-size ultraviolet emitters for nanoengineering and biotechnological applications
Radiation hydrodynamics of SN 1987A: I. Global analysis of the light curve for the first 4 months
The optical/UV light curves of SN 1987A are analyzed with the multi-energy
group radiation hydrodynamics code STELLA. The calculated monochromatic and
bolometric light curves are compared with observations shortly after shock
breakout, during the early plateau, through the broad second maximum, and
during the earliest phase of the radioactive tail. We have concentrated on a
progenitor model calculated by Nomoto & Hashimoto and Saio, Nomoto, & Kato,
which assumes that 14 solar masses of the stellar mass is ejected. Using this
model, we have updated constraints on the explosion energy and the extent of
mixing in the ejecta. In particular, we determine the most likely range of E/M
(explosion energy over ejecta mass) and R_0 (radius of the progenitor). In
general, our best models have energies in the range E = (1.1 +/- 0.3) x 10^{51}
ergs, and the agreement is better than in earlier, flux-limited diffusion
calculations for the same explosion energy. Our modeled B and V fluxes compare
well with observations, while the flux in U undershoots after about 10 days by
a factor of a few, presumably due to NLTE and line transfer effects. We also
compare our results with IUE observations, and a very good quantitative
agreement is found for the first days, and for one IUE band (2500-3000 A) as
long as for 3 months. We point out that the V flux estimated by McNaught &
Zoltowski should probably be revised to a lower value.Comment: 27 pages AASTeX v.4.0 + 35 postscript figures. ApJ, accepte
Room temperature plasmon laser by total internal reflection
Plasmon lasers create and sustain intense and coherent optical fields below
light's diffraction limit with the unique ability to drastically enhance
light-matter interactions bringing fundamentally new capabilities to
bio-sensing, data storage, photolithography and optical communications.
However, these important applications require room temperature operation, which
remains a major hurdle. Here, we report a room temperature semiconductor
plasmon laser with both strong cavity feedback and optical confinement to
1/20th of the wavelength. The strong feedback arises from total internal
reflection of surface plasmons, while the confinement enhances the spontaneous
emission rate by up to 20 times.Comment: 8 Page, 2 Figure
Quantum Statistics of Surface Plasmon Polaritons in Metallic Stripe Waveguides
Single surface plasmon polaritons are excited using photons generated via
spontaneous parametric down-conversion. The mean excitation rates, intensity
correlations and Fock state populations are studied. The observed dependence of
the second order coherence in our experiment is consistent with a linear
uncorrelated Markovian environment in the quantum regime. Our results provide
important information about the effect of loss for assessing the potential of
plasmonic waveguides for future nanophotonic circuitry in the quantum regime.Comment: 21 pages, 6 figures, published in Nano Letters, publication date
(web): March 27 (2012
Enhanced reaction kinetics in biological cells
The cell cytoskeleton is a striking example of "active" medium driven
out-of-equilibrium by ATP hydrolysis. Such activity has been shown recently to
have a spectacular impact on the mechanical and rheological properties of the
cellular medium, as well as on its transport properties : a generic tracer
particle freely diffuses as in a standard equilibrium medium, but also
intermittently binds with random interaction times to motor proteins, which
perform active ballistic excursions along cytoskeletal filaments. Here, we
propose for the first time an analytical model of transport limited reactions
in active media, and show quantitatively how active transport can enhance
reactivity for large enough tracers like vesicles. We derive analytically the
average interaction time with motor proteins which optimizes the reaction rate,
and reveal remarkable universal features of the optimal configuration. We
discuss why active transport may be beneficial in various biological examples:
cell cytoskeleton, membranes and lamellipodia, and tubular structures like
axons.Comment: 10 pages, 2 figure
Π‘ΠΠΠ’ΠΠΠ¨ΠΠΠΠ Π ΠΠΠΠΠΠΠ«Π₯ ΠΠΠ‘ΠΠΠΠΠΠ ΠΠΠΠΠΠΠΠΠ‘ΠΠΠΠ Π ΠΠΠΠΠΠΠΠΠ‘ΠΠΠΠ ΠΠΠΠ ΠΠ‘Π’Π ΠΠ Π’ΠΠ Π ΠΠ’ΠΠ ΠΠ ΠΠΠΠΠΠΠΠ Π§ΠΠ‘Π’Π ΠΠΠ’ΠΠ-Π‘ΠΠ―ΠΠ‘ΠΠΠ Π‘ΠΠΠΠΠ§ΠΠ’ΠΠ ΠΠΠΠΠ‘Π’Π
Fault structures in folded areas are an important element of the geological structure. Their age and history of development affect seismicity, distribution of minerals, and engineering and geological characteristics of the area. The geological structure of the Altai-Sayan folded area was mainly formed during the Paleozoic and transformed during the Cenozoic activation. Geoinformation methods and technologies were used to compare between the Paleozoic and Cenozoic fault networks. It is shown that the degree of reactivation of the Paleozoic faults varies greatly within the territory.Conjugate analysis of the orientation and spatial distribution of faults of different ages in the study area does not confirm that the Cenozoic fault system was formed by reactivation or inherited development of the Paleozoic fault system. These two systems arose at different compression orientations. The left-lateral strike-slip ensemble was formed under sublatitudinal compression in the Paleozoic, and the right-lateral strike-slip ensemble - under submeridional compression in the Cenozoic. A significant coincidence between the directions of the main faults of different ages is due to their dominant strike along the boundaries of the accretionary complexes in the region.Π Π°Π·Π»ΠΎΠΌΠ½ΡΠ΅ ΡΡΡΡΠΊΡΡΡΡ Π² ΡΠΊΠ»Π°Π΄ΡΠ°ΡΡΡ
ΠΎΠ±Π»Π°ΡΡΡΡ
ΡΠ²Π»ΡΡΡΡΡ Π²Π°ΠΆΠ½ΡΠΌ ΡΠ»Π΅ΠΌΠ΅Π½ΡΠΎΠΌ Π³Π΅ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΡΡΡΠΊΡΡΡΡ. ΠΡ
Π²ΠΎΠ·ΡΠ°ΡΡ ΠΈ ΠΈΡΡΠΎΡΠΈΡ ΡΠ°Π·Π²ΠΈΡΠΈΡ Π²Π»ΠΈΡΡΡ Π½Π° ΡΠ΅ΠΉΡΠΌΠΈΡΠ½ΠΎΡΡΡ, ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ ΠΏΠΎΠ»Π΅Π·Π½ΡΡ
ΠΈΡΠΊΠΎΠΏΠ°Π΅ΠΌΡΡ
, ΠΈΠ½ΠΆΠ΅Π½Π΅ΡΠ½ΠΎ-Π³Π΅ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠΈ ΠΌΠ΅ΡΡΠ½ΠΎΡΡΠΈ. ΠΠ΅ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠ°Ρ ΡΡΡΡΠΊΡΡΡΠ° ΠΠ»ΡΠ°Π΅-Π‘Π°ΡΠ½ΡΠΊΠΎΠΉ ΡΠΊΠ»Π°Π΄ΡΠ°ΡΠΎΠΉ ΠΎΠ±Π»Π°ΡΡΠΈ Π² ΠΎΡΠ½ΠΎΠ²Π½ΠΎΠΌ ΡΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π»Π°ΡΡ Π² ΠΏΠ°Π»Π΅ΠΎΠ·ΠΎΠ΅, Π½ΠΎ Π±ΡΠ»Π° ΠΏΡΠ΅ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½Π° Π² Ρ
ΠΎΠ΄Π΅ ΠΊΠ°ΠΉΠ½ΠΎΠ·ΠΎΠΉΡΠΊΠΎΠΉ Π°ΠΊΡΠΈΠ²ΠΈΠ·Π°ΡΠΈΠΈ. ΠΠ΅ΡΠΎΠ΄Π°ΠΌΠΈ Π³Π΅ΠΎΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΠΎΠ½Π½ΡΡ
ΡΠ΅Ρ
Π½ΠΎΠ»ΠΎΠ³ΠΈΠΉ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½ΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΠ΅ ΠΏΠ°Π»Π΅ΠΎΠ·ΠΎΠΉΡΠΊΠΎΠΉ ΠΈ ΠΊΠ°ΠΉΠ½ΠΎΠ·ΠΎΠΉΡΠΊΠΎΠΉ ΡΠ΅ΡΠ΅ΠΉ ΡΠ°Π·Π»ΠΎΠΌΠΎΠ². ΠΠΎΠΊΠ°Π·Π°Π½ΠΎ, ΡΡΠΎ ΡΡΠ΅ΠΏΠ΅Π½Ρ ΡΠ΅Π°ΠΊΡΠΈΠ²Π°ΡΠΈΠΈ ΠΏΠ°Π»Π΅ΠΎΠ·ΠΎΠΉΡΠΊΠΈΡ
ΡΠ°Π·Π»ΠΎΠΌΠΎΠ² ΡΠΈΠ»ΡΠ½ΠΎ Π²Π°ΡΡΠΈΡΡΠ΅ΡΡΡ Π² ΠΏΡΠ΅Π΄Π΅Π»Π°Ρ
ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ.Π‘ΠΎΠΏΡΡΠΆΠ΅Π½Π½ΡΠΉ Π°Π½Π°Π»ΠΈΠ· ΠΎΡΠΈΠ΅Π½ΡΠΈΡΠΎΠ²ΠΊΠΈ ΠΈ ΠΏΡΠΎΡΡΡΠ°Π½ΡΡΠ²Π΅Π½Π½ΠΎΠ³ΠΎ ΡΠ°Π·ΠΌΠ΅ΡΠ΅Π½ΠΈΡ ΡΠ°Π·Π½ΠΎΠ²ΠΎΠ·ΡΠ°ΡΡΠ½ΡΡ
ΡΠ°Π·Π»ΠΎΠΌΠΎΠ² ΠΈΠ·ΡΡΠ°Π΅ΠΌΠΎΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ Π½Π΅ ΠΏΠΎΠ΄ΡΠ²Π΅ΡΠΆΠ΄Π°Π΅Ρ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½ΠΈΠ΅ ΠΎ ΡΠΎΠΌ, ΡΡΠΎ ΠΊΠ°ΠΉΠ½ΠΎΠ·ΠΎΠΉΡΠΊΠ°Ρ ΡΠΈΡΡΠ΅ΠΌΠ° ΡΠ°Π·Π»ΠΎΠΌΠΎΠ² ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π»Π°ΡΡ ΠΏΡΡΠ΅ΠΌ ΡΠ΅Π°ΠΊΡΠΈΠ²Π°ΡΠΈΠΈ ΠΈΠ»ΠΈ ΡΠ½Π°ΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Π½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΏΠ°Π»Π΅ΠΎΠ·ΠΎΠΉΡΠΊΠΎΠΉ ΡΠΈΡΡΠ΅ΠΌΡ ΡΠ°Π·ΡΡΠ²Π½ΡΡ
Π½Π°ΡΡΡΠ΅Π½ΠΈΠΉ. ΠΡΠΈ Π΄Π²Π΅ ΡΠΈΡΡΠ΅ΠΌΡ Π²ΠΎΠ·Π½ΠΈΠΊΠ°Π»ΠΈ ΠΏΡΠΈ ΡΠ°Π·Π½ΡΡ
ΠΎΡΠΈΠ΅Π½ΡΠΈΡΠΎΠ²ΠΊΠ°Ρ
ΡΠΆΠ°ΡΠΈΡ. Π ΠΏΠ°Π»Π΅ΠΎΠ·ΠΎΠ΅ ΠΏΡΠΈ ΡΡΠ±ΡΠΈΡΠΎΡΠ½ΠΎΠΌ ΡΠΆΠ°ΡΠΈΠΈ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π»ΡΡ Π»Π΅Π²ΠΎΡΠ΄Π²ΠΈΠ³ΠΎΠ²ΡΠΉ Π°Π½ΡΠ°ΠΌΠ±Π»Ρ, Π° Π² ΠΊΠ°ΠΉΠ½ΠΎΠ·ΠΎΠ΅ Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ
ΡΡΠ±ΠΌΠ΅ΡΠΈΠ΄ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠΆΠ°ΡΠΈΡ - ΠΏΡΠ°Π²ΠΎΡΠ΄Π²ΠΈΠ³ΠΎΠ²ΡΠΉ. Π‘ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠ΅ ΡΠΎΠ²ΠΏΠ°Π΄Π΅Π½ΠΈΠ΅ Π½Π°ΠΏΡΠ°Π²Π»Π΅Π½ΠΈΠΉ ΠΌΠ°Π³ΠΈΡΡΡΠ°Π»ΡΠ½ΡΡ
ΡΠ°Π·Π»ΠΎΠΌΠΎΠ² ΡΠ°Π·Π½ΠΎΠ³ΠΎ Π²ΠΎΠ·ΡΠ°ΡΡΠ° ΠΎΠ±ΡΡΠ»ΠΎΠ²Π»Π΅Π½ΠΎ ΠΈΡ
Π΄ΠΎΠΌΠΈΠ½ΠΈΡΡΡΡΠΈΠΌ ΠΏΡΠΎΡΡΠΈΡΠ°Π½ΠΈΠ΅ΠΌ ΡΠΎΠ³Π»Π°ΡΠ½ΠΎ Π³ΡΠ°Π½ΠΈΡΠ°ΠΌ Π°ΠΊΠΊΡΠ΅ΡΠΈΠΎΠ½Π½ΡΡ
ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ² ΡΠ΅Π³ΠΈΠΎΠ½Π°
Resonant enhancement of the zero-phonon emission from a color center in a diamond cavity
We demonstrate coupling of the zero-phonon line of individual
nitrogen-vacancy centers and the modes of microring resonators fabricated in
single-crystal diamond. A zero-phonon line enhancement exceeding ten-fold is
estimated from lifetime measurements at cryogenic temperatures. The devices are
fabricated using standard semiconductor techniques and off-the-shelf materials,
thus enabling integrated diamond photonics.Comment: 5 pages, 4 figure
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