21 research outputs found
Computation of charge distribution and electrostatic potential in silicates with the use of chemical potential equalization models
New parameters for the electronegativity equalization model (EEM) and the split-charge equilibration (SQE) model are calibrated for silicate materials, based on an extensive training set of representative isolated systems. In total, four calibrations are carried out, two for each model, either using iterative Hirshfeld (HI) charges or ESP grid data computed with density functional theory (DFT) as a reference. Both the static (ground state) reference quantities and their responses to uniform electric fields are included in the fitting procedure. The EEM model fails to describe the response data, whereas the SQE model quantitatively reproduces all of the training data. For the ESP-based parameters, we found that the reference ESP data are only useful at those grid points where the electron density is lower than 0.001 a.u. The density value correlates with a distance criterion used for selecting grid points in common ESP fitting schemes. All parameters are validated with DFT computations on an independent set of isolated systems (similar to the training set), and on a set of periodic systems including dense and microporous crystalline silica structures, zirconia, and zirconium silicate. Although the transferability of the parameters to new isolated systems poses no difficulties, the atomic hardness parameters in the HI-based models must be corrected to obtain accurate results for periodic systems. The SQE/ESP model permits the calculation of the ESP with similar accuracy in both isolated and periodic systems
Environmental conditions of interstadial (MIS 3) and features of the last glacial maximum on the King George island (West Antarctica)
The interstadial marine deposits stratum was described in the Fildes Peninsula (King George Island) due to field and laboratory investigations during 2008β2011. The stratum fragments occur in the west and north-west parts of peninsula in following forms: sections of soft sediments, containing fossil shells, marine algae, bones of marine animals and rich marine diatom complexes in situ (11 sites); fragments of shells and bones on the surface (25 sites). According to the results of radiocarbon dating, these deposits were accumulated within the period 19β50 ky BP. Geographical and altitude settings of the sites, age characteristics, taxonomy of fossil flora and fauna, and good safety of the soft deposits stratum allow to make following conclusions: during interstadial, sea water covered significant part of King George Island up to the present altitude of 40 m a.s.l., and the King George Island glaciation had smaller size then; environmental conditions for the interstadial deposit stratum accumulation were at least not colder than today; probably, the King George island territory was covered entirely by ice masses of Last glacial maximum not earlier than 19 ky BP; during Last glacial maximum, King George Island was covered by thin, Β«coldΒ», not mobile glaciers, which contribute to conservation of the soft marine interstadial deposits filled with fossil flora and fauna
Π£ΡΠ»ΠΎΠ²ΠΈΡ ΠΈΠ½ΡΠ΅ΡΡΡΠ°Π΄ΠΈΠ°Π»Π° (MIS3) ΠΈ Ρ Π°ΡΠ°ΠΊΡΠ΅Ρ ΠΎΠ»Π΅Π΄Π΅Π½Π΅Π½ΠΈΡ Π² ΠΏΠΎΡΠ»Π΅Π΄Π½ΠΈΠΉ Π»Π΅Π΄Π½ΠΈΠΊΠΎΠ²ΡΠΉ ΠΌΠ°ΠΊΡΠΈΠΌΡΠΌ Π½Π° ΠΎ. ΠΠΈΠ½Π³ ΠΠΆΠΎΡΠ΄ΠΆ (ΠΠ°ΠΏΠ°Π΄Π½Π°Ρ ΠΠ½ΡΠ°ΡΠΊΡΠΈΠΊΠ°)
The interstadial marine deposits stratum was described in the Fildes Peninsula (King George Island) due to field and laboratory investigations during 2008β2011. The stratum fragments occur in the west and north-west parts of peninsula in following forms: sections of soft sediments, containing fossil shells, marine algae, bones of marine animals and rich marine diatom complexes in situ (11 sites); fragments of shells and bones on the surface (25 sites). According to the results of radiocarbon dating, these deposits were accumulated within the period 19β50 ky BP. Geographical and altitude settings of the sites, age characteristics, taxonomy of fossil flora and fauna, and good safety of the soft deposits stratum allow to make following conclusions: during interstadial, sea water covered significant part of King George Island up to the present altitude of 40 m a.s.l., and the King George Island glaciation had smaller size then; environmental conditions for the interstadial deposit stratum accumulation were at least not colder than today; probably, the King George island territory was covered entirely by ice masses of Last glacial maximum not earlier than 19 ky BP; during Last glacial maximum, King George Island was covered by thin, Β«coldΒ», not mobile glaciers, which contribute to conservation of the soft marine interstadial deposits filled with fossil flora and fauna.Π Ρ
ΠΎΠ΄Π΅ ΡΠΊΡΠΏΠ΅Π΄ΠΈΡΠΈΠΎΠ½Π½ΡΡ
ΠΈ Π»Π°Π±ΠΎΡΠ°ΡΠΎΡΠ½ΡΡ
ΡΠ°Π±ΠΎΡ 2008β2012Β Π³Π³. ΠΈΠ·ΡΡΠ΅Π½Ρ ΡΠ°ΡΠΏΡΠΎΡΡΡΠ°Π½ΡΠ½Π½ΡΠ΅ Π½Π° ΠΏ-ΠΎΠ²Π΅Β Π€Π°ΠΉΠ»Π΄Ρ (ΠΎ.Β ΠΠΈΠ½Π³ ΠΠΆΠΎΡΠ΄ΠΆ) ΠΌΠΎΡΡΠΊΠΈΠ΅ ΠΎΡΠ»ΠΎΠΆΠ΅Π½ΠΈΡ ΠΈΠ½ΡΠ΅ΡΡΡΠ°Π΄ΠΈΠ°Π»Π°. Π Π°Π·ΡΠ΅Π·Ρ ΠΎΡΠ»ΠΎΠΆΠ΅Π½ΠΈΠΉ Π² Π½Π΅Π½Π°ΡΡΡΠ΅Π½Π½ΠΎΠΌ Π·Π°Π»Π΅Π³Π°Π½ΠΈΠΈ, ΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠΈΠ΅ ΠΌΠΎΡΡΠΊΠΈΠ΅ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΡ Π΄ΠΈΠ°ΡΠΎΠΌΠ΅ΠΉ, ΡΠ°ΠΊΠΎΠ²ΠΈΠ½Ρ, Π²ΠΎΠ΄ΠΎΡΠΎΡΠ»ΠΈ ΠΈ ΠΊΠΎΡΡΠΈ ΠΌΠΎΡΡΠΊΠΈΡ
ΠΆΠΈΠ²ΠΎΡΠ½ΡΡ
, ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Ρ Π² 11Β ΡΠΎΡΠΊΠ°Ρ
; Π²ΡΡΡΠΏΠΊΠΈ ΡΠ°ΠΊΠΎΠ²ΠΈΠ½ ΠΈ ΠΊΠΎΡΡΠ΅ΠΉ Π½Π° ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ ΠΌΡΡΠΎΠ², ΠΌΠΎΡΠ΅Π½ ΠΈ ΡΠΊΠ»ΠΎΠ½ΠΎΠ² Π΄ΠΎΠ»ΠΈΠ½ ΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½Ρ Π² 25Β ΡΠΎΡΠΊΠ°Ρ
. Π‘ΠΎΠ³Π»Π°ΡΠ½ΠΎ ΡΠ°Π΄ΠΈΠΎΡΠ³Π»Π΅ΡΠΎΠ΄Π½ΠΎΠΌΡ Π΄Π°ΡΠΈΡΠΎΠ²Π°Π½ΠΈΡ, ΡΡΠΈ ΠΎΡΠ»ΠΎΠΆΠ΅Π½ΠΈΡ Π½Π°ΠΊΠ°ΠΏΠ»ΠΈΠ²Π°Π»ΠΈΡΡ Π² ΠΏΠ΅ΡΠΈΠΎΠ΄ ΠΌΠ΅ΠΆΠ΄Ρ 19 ΠΈ 50Β ΡΡΡ.Β Π».Π½. ΠΡΠΎΡΡΡΠ°Π½ΡΡΠ²Π΅Π½Π½ΠΎΠ΅ ΠΈ Π²ΡΡΠΎΡΠ½ΠΎΠ΅ ΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΠ΅ ΠΎΡΠ»ΠΎΠΆΠ΅Π½ΠΈΠΉ, ΠΈΡ
ΡΡΡΠΎΠ΅Π½ΠΈΠ΅, Π²ΠΎΠ·ΡΠ°ΡΡ, Π° ΡΠ°ΠΊΠΆΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ Π²ΠΈΠ΄ΠΎΠ²ΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π° ΠΈΡΠΊΠΎΠΏΠ°Π΅ΠΌΠΎΠΉ ΡΠ»ΠΎΡΡ ΠΈ ΡΠ°ΡΠ½Ρ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ Π·Π°ΠΊΠ»ΡΡΠΈΡΡ ΡΠ»Π΅Π΄ΡΡΡΠ΅Π΅: 1)Β Π² ΠΏΠ΅ΡΠΈΠΎΠ΄ ΠΈΠ½ΡΠ΅ΡΡΡΠ°Π΄ΠΈΠ°Π»Π° ΠΌΠΎΡΡΠΊΠΈΠ΅ Π²ΠΎΠ΄Ρ ΡΠ°ΡΠΏΡΠΎΡΡΡΠ°Π½ΡΠ»ΠΈΡΡ Π½Π° ΠΎ.Β ΠΠΈΠ½Π³ ΠΠΆΠΎΡΠ΄ΠΆ ΠΊΠ°ΠΊ ΠΌΠΈΠ½ΠΈΠΌΡΠΌ Π΄ΠΎ ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ
Π²ΡΡΠΎΡΠ½ΡΡ
ΠΎΡΠΌΠ΅ΡΠΎΠΊ 40Β ΠΌ, Π° ΠΏΠ»ΠΎΡΠ°Π΄Ρ ΠΎΡΡΡΠΎΠ²Π° ΠΈ ΠΎΠ»Π΅Π΄Π΅Π½Π΅Π½ΠΈΡ Π·Π°ΠΌΠ΅ΡΠ½ΠΎ ΡΠΎΠΊΡΠ°ΡΠ°Π»Π°ΡΡ; 2)Β ΡΡΠ»ΠΎΠ²ΠΈΡ Π½Π°ΠΊΠΎΠΏΠ»Π΅Π½ΠΈΡ ΠΎΡΠ»ΠΎΠΆΠ΅Π½ΠΈΠΉ ΠΈΠ½ΡΠ΅ΡΡΡΠ°Π΄ΠΈΠ°Π»Π° Π±ΡΠ»ΠΈ, ΠΏΠΎ ΠΊΡΠ°ΠΉΠ½Π΅ΠΉ ΠΌΠ΅ΡΠ΅, Π½Π΅ Ρ
ΠΎΠ»ΠΎΠ΄Π½Π΅Π΅ Π½Π°Π±Π»ΡΠ΄Π°ΡΡΠΈΡ
ΡΡ Π² ΡΡΠΎΠΌ ΡΠ°ΠΉΠΎΠ½Π΅ ΡΠ΅ΠΉΡΠ°Ρ; 3)Β ΡΠ°Π·Π²ΠΈΡΠΈΠ΅ ΠΎΠ»Π΅Π΄Π΅Π½Π΅Π½ΠΈΡ ΠΏΠΎΡΠ»Π΅Π΄Π½Π΅Π³ΠΎ Π»Π΅Π΄Π½ΠΈΠΊΠΎΠ²ΠΎΠ³ΠΎ ΠΌΠ°ΠΊΡΠΈΠΌΡΠΌΠ°Β (ΠΠΠ) Π½Π° ΠΎ.Β ΠΠΈΠ½Π³ ΠΠΆΠΎΡΠ΄ΠΆ Π½Π°ΡΠ°Π»ΠΎΡΡ Π΄ΠΎΠ²ΠΎΠ»ΡΠ½ΠΎ ΠΏΠΎΠ·Π΄Π½ΠΎ; Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎ, Π΄ΠΎ 19Β ΡΡΡ.Β Π».Π½. ΠΎΡΡΡΠΎΠ² Π½Π΅ Π±ΡΠ» ΠΏΠΎΠ»Π½ΠΎΡΡΡΡ ΠΏΠΎΠΊΡΡΡ Π»ΡΠ΄ΠΎΠΌ; 4)Β ΠΎΠ»Π΅Π΄Π΅Π½Π΅Π½ΠΈΠ΅ ΠΠΠ Π½Π° ΠΎ.Β ΠΠΈΠ½Π³ ΠΠΆΠΎΡΠ΄ΠΆ Π±ΡΠ»ΠΎ ΠΌΠ°Π»ΠΎΠΌΠΎΡΠ½ΡΠΌ, ΠΌΠ°Π»ΠΎΠΏΠΎΠ΄Π²ΠΈΠΆΠ½ΡΠΌ (Β«Ρ
ΠΎΠ»ΠΎΠ΄Π½ΠΎΠ³ΠΎΒ» ΡΠΈΠΏΠ°) ΠΈ, Π²Π΅ΡΠΎΡΡΠ½ΠΎ, Π±ΡΠ»ΠΎ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½ΠΎ Π½Π΅ΡΠΊΠΎΠ»ΡΠΊΠΈΠΌΠΈ Π»Π΅Π΄Π½ΠΈΠΊΠ°ΠΌΠΈ Ρ Π½ΠΈΠ·ΠΊΠΈΠΌΠΈ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΠΎΠΌ ΡΠΊΠ·Π°ΡΠ°ΡΠΈΠΈ ΠΈ ΡΠΏΠΎΡΠΎΠ±Π½ΠΎΡΡΡΡ Β«ΠΊΠΎΠ½ΡΠ΅ΡΠ²ΠΈΡΠΎΠ²Π°ΡΡΒ» Π΄ΡΠ΅Π²Π½ΠΈΠ΅ ΠΎΡΠ»ΠΎΠΆΠ΅Π½ΠΈΡ