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Mathematical simulation of gas bubble moving in central region of the short vortex chamber

100%

Syomin D., Rogovyi A.

Teka Komisji Motoryzacji i Energetyki Rolnictwa

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2012

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tom 12

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nr 4

2

Computer modeling of destructive fire hazards dynamics

100%

Michaylov D.

Teka Komisji Motoryzacji i Energetyki Rolnictwa

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2013

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tom 13

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nr 3

3

Convective heat exchange in optopneumatic cell

84%

Kaljuzhnyj G., Kovalenko A., Lyshtvan E.

Teka Komisji Motoryzacji i Energetyki Rolnictwa

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2010

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tom 10A

4

Matematicheskoe modelirovanie napr'jazhennogo sostojanija ploda tomata pri vertikal'nom sdavlivanii

84%

Melnik V.

Motrol. Motoryzacja i Energetyka Rolnictwa

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2013

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tom 15

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nr 7

5

Three-dimensional elasto-plastic soil modelling and analysis of sauropod tracks

84%

Sanz E., Arcos A., Pascual C., Pidal I. M.

Acta Palaeontologica Polonica

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2016

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tom 61

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nr 2

This paper reports the use of FEA (Finite Element Analysis) to model dinosaur tracks. Satisfactory reproductions of sauropod ichnites were simulated using 3D numerical models of the elasto-plastic behaviour of soils. Though the modelling was done of ichnites in situ at the Miraflores I tracksite (Soria, Spain), the methodology could be applied to other tracksites to improve their ichnological interpretation and better understand how the type and state of the trodden sediment at the moment the track is created is a fundamental determinant of the morphology of the ichnite. The results obtained explain why the initial and commonly adopted hypothesis—that soft sediments become progressively more rigid and resistant at depth—is not appropriate at this tracksite. We explain why it is essential to consider a more rigid superficial layer (caused by desiccation) overlying a softer layer that is extruded to form a displacement rim. Adult sauropods left trackways behind them. These tracks could be filled up with water due to phreatic level was close to the ground surface. The simulation provides us with a means to explain the differences between similar tracks (of different depths; with or without displacement rims) in the various stratigraphic layers of the tracksite and to explain why temporary and variable conditions of humidity lead to these differences in the tracks. The simulations also demonstrate that track depth alone is insufficient to differentiate true tracks from undertracks and that other discrimination criteria need to be taken into account. The scarcity of baby sauropod tracks is explained because they are shallow and easily eroded.

6

Power characteristics of superchargers with vortex work chamber

84%

Syomin D., Rogovoy A.

Teka Komisji Motoryzacji i Energetyki Rolnictwa

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2010

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tom 10B

7

Studies of meteorological factors influence upon air agrophysical characteristics in canopy on the base of physical and mathematical simulation

84%

Gak E. Z., Smolyar E. I., Gak M. Z.

International Agrophysics

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1994

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tom 08

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nr 1

8

Mathematical simulation of soil cloddiness

67%

Chertkov V. Y.

International Agrophysics

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1995

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tom 09

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nr 3

Ograniczanie wyników

4 Teka Komisji Motoryzacji i Energetyki Rolnictwa

2 International Agrophysics

1 Acta Palaeontologica Polonica

1 Motrol. Motoryzacja i Energetyka Rolnictwa

2 Syomin D.

1 Arcos A.

1 Chertkov V. Y.

1 Gak E. Z.

1 Gak M. Z.

1 Kaljuzhnyj G.

1 Kovalenko A.

1 Lyshtvan E.

1 Melnik V.

1 Michaylov D.

1 Pascual C.

1 Pidal I. M.

1 Rogovoy A.

1 Rogovyi A.

1 Sanz E.

1 Smolyar E. I.

1 2016

2 2013

1 2012

2 2010

1 1995

1 1994

Mathematical simulation of gas bubble moving in central region of the short vortex chamber

Computer modeling of destructive fire hazards dynamics

Convective heat exchange in optopneumatic cell

Matematicheskoe modelirovanie napr'jazhennogo sostojanija ploda tomata pri vertikal'nom sdavlivanii

Three-dimensional elasto-plastic soil modelling and analysis of sauropod tracks

Power characteristics of superchargers with vortex work chamber

Studies of meteorological factors influence upon air agrophysical characteristics in canopy on the base of physical and mathematical simulation

Mathematical simulation of soil cloddiness