scholarly journals Probing zeolites by vibrational spectroscopies

2015 ◽  
Vol 44 (20) ◽  
pp. 7262-7341 ◽  
Author(s):  
Silvia Bordiga ◽  
Carlo Lamberti ◽  
Francesca Bonino ◽  
Arnaud Travert ◽  
Frédéric Thibault-Starzyk

This review addresses the most relevant aspects of vibrational spectroscopies (IR, Raman and INS) applied to zeolites and zeotype materials: acidity, basicity and site accessibility investigated by probes molecules; precise determination of the IR absorption coefficients; thermodynamic aspects of molecular adsorption; space and time resolved experiments.

1995 ◽  
Vol 13 (2) ◽  
pp. 183-190 ◽  
Author(s):  
W. Laux ◽  
J. Jacoby ◽  
D.H.H. Hoffmann

Plasmas with solid-state density at temperatures of a few eV will be produced in the near future at GSI by high-energy heavy ions. To diagnose these plasmas, novel methods–based on hard X-ray diagnostics–have to be applied. An investigation of the hydrodynamic expansion of the target requires a space- and time-resolved measurement of the plasma density. The determination of the target density independently of its temperature is obtained by a special X-ray pinhole camera enabling a selective registration of the target K-shell emission in combination with space- and time-resolved beam intensity measurements.


2005 ◽  
Vol 10 (5) ◽  
pp. 054004 ◽  
Author(s):  
R. L. P. van Veen ◽  
H. J. C. M. Sterenborg ◽  
A. Pifferi ◽  
A. Torricelli ◽  
E. Chikoidze ◽  
...  

2010 ◽  
Vol 46 (4) ◽  
pp. 411-417 ◽  
Author(s):  
Yang MENG ◽  
Lin GU ◽  
Wenzheng ZHANG

1968 ◽  
Vol 12 ◽  
Author(s):  
R. Goossens

A precise method for the determination of the increment of the  basal area using the PressIer bore. Refering to  previous research showing that the basal area of the corsica pine could be  characterized by an ellips, we present in this paper a precise method for the  determination of the increment of the basal area. In this method we determine  the direction of the maximum diameter, we measure this diameter and we take a  core in one of the points of tangency of the caliper with the measured tree.  The determination of the diameter perpendicular to the maximum diameter  finishes the work wich is to be done in the forest. From the classical  measurements effectuated on the core and from the measured diameters we can  then determine the form (V) and the excentricity (e). Substituting these two  parameters in the formula 2 or 2', we can also calculate the error of a  radius measured on the core with respect to the representative radius, This  error with them allow us to correct the measured value of the minimum or the  maximum radius and we will be able to do a precise determination of the  increment.


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