|
|
|
|
| LEADER |
01000caa a22002652 4500 |
| 001 |
NLM110040589 |
| 003 |
DE-627 |
| 005 |
20250202085617.0 |
| 007 |
tu |
| 008 |
231222s2000 xx ||||| 00| ||eng c |
| 028 |
5 |
2 |
|a pubmed25n0367.xml
|
| 035 |
|
|
|a (DE-627)NLM110040589
|
| 035 |
|
|
|a (NLM)11088595
|
| 040 |
|
|
|a DE-627
|b ger
|c DE-627
|e rakwb
|
| 041 |
|
|
|a eng
|
| 100 |
1 |
|
|a Poschel
|e verfasserin
|4 aut
|
| 245 |
1 |
0 |
|a Onset of fluidization in vertically shaken granular material
|
| 264 |
|
1 |
|c 2000
|
| 336 |
|
|
|a Text
|b txt
|2 rdacontent
|
| 337 |
|
|
|a ohne Hilfsmittel zu benutzen
|b n
|2 rdamedia
|
| 338 |
|
|
|a Band
|b nc
|2 rdacarrier
|
| 500 |
|
|
|a Date Revised 20.11.2019
|
| 500 |
|
|
|a published: Print
|
| 500 |
|
|
|a Citation Status PubMed-not-MEDLINE
|
| 520 |
|
|
|a When granular material is shaken vertically one observes convection, surface fluidization, spontaneous heap formation, and other effects. There is a controversial discussion in the literature as to whether there exists a threshold for the Froude number Gamma=A(0)omega(2)(0)/g, below which these effects cannot be observed anymore. By means of theoretical analysis and computer simulation we find that there is no such single threshold. Instead, we propose a modified criterion that coincides with the critical Froude number Gamma(c)=1 for small driving frequency omega(0)
|
| 650 |
|
4 |
|a Journal Article
|
| 700 |
1 |
|
|a Schwager
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Saluena
|e verfasserin
|4 aut
|
| 773 |
0 |
8 |
|i Enthalten in
|t Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics
|d 1993
|g 62(2000), 1 Pt B vom: 27. Juli, Seite 1361-7
|w (DE-627)NLM098226002
|x 1063-651X
|7 nnns
|
| 773 |
1 |
8 |
|g volume:62
|g year:2000
|g number:1 Pt B
|g day:27
|g month:07
|g pages:1361-7
|
| 912 |
|
|
|a GBV_USEFLAG_A
|
| 912 |
|
|
|a SYSFLAG_A
|
| 912 |
|
|
|a GBV_NLM
|
| 912 |
|
|
|a GBV_ILN_350
|
| 951 |
|
|
|a AR
|
| 952 |
|
|
|d 62
|j 2000
|e 1 Pt B
|b 27
|c 07
|h 1361-7
|