Toward the Avogadro constant-preliminary results on the molar volume of silicon

1989 ◽  
Vol 38 (2) ◽  
pp. 200-205 ◽  
Author(s):  
A. Sacconi ◽  
A.M. Peuto ◽  
W. Pasin ◽  
R. Panciera ◽  
G. Lenaers ◽  
...  
1988 ◽  
Author(s):  
Sacconi ◽  
Peuto ◽  
Lenaers ◽  
Valkiers ◽  
De Bievre

1987 ◽  
Vol IM-36 (2) ◽  
pp. 161-165 ◽  
Author(s):  
Peter Seyfried ◽  
Reiner Balhorn ◽  
Manfred Kochsiek ◽  
Andrzej F. Kozdon ◽  
H.-J. Rademacher ◽  
...  

Metrologia ◽  
1999 ◽  
Vol 36 (5) ◽  
pp. 455-464 ◽  
Author(s):  
K Fujii ◽  
M Tanaka ◽  
Y Nezu ◽  
K Nakayama ◽  
H Fujimoto ◽  
...  

2001 ◽  
Vol 50 (2) ◽  
pp. 593-597 ◽  
Author(s):  
P. De Bievre ◽  
S. Valkiers ◽  
R. Kessel ◽  
P.D.P. Taylor ◽  
P. Becker ◽  
...  

1997 ◽  
Vol 46 (2) ◽  
pp. 592-595 ◽  
Author(s):  
P. De Bievre ◽  
S. Valkiers ◽  
R. Gonfiantini ◽  
P.D.P. Taylor ◽  
H. Bettin ◽  
...  

2003 ◽  
Vol 52 (2) ◽  
pp. 646-651 ◽  
Author(s):  
K. Fujii ◽  
A. Waseda ◽  
N. Kuramoto ◽  
S. Mizushima ◽  
M. Tanaka ◽  
...  

1999 ◽  
Vol 173 ◽  
pp. 185-188
Author(s):  
Gy. Szabó ◽  
K. Sárneczky ◽  
L.L. Kiss

AbstractA widely used tool in studying quasi-monoperiodic processes is the O–C diagram. This paper deals with the application of this diagram in minor planet studies. The main difference between our approach and the classical O–C diagram is that we transform the epoch (=time) dependence into the geocentric longitude domain. We outline a rotation modelling using this modified O–C and illustrate the abilities with detailed error analysis. The primary assumption, that the monotonity and the shape of this diagram is (almost) independent of the geometry of the asteroids is discussed and tested. The monotonity enables an unambiguous distinction between the prograde and retrograde rotation, thus the four-fold (or in some cases the two-fold) ambiguities can be avoided. This turned out to be the main advantage of the O–C examination. As an extension to the theoretical work, we present some preliminary results on 1727 Mette based on new CCD observations.


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