On the determination of dynamic errors for rise time measurement with an oscilloscope

1999 ◽  
Vol 48 (6) ◽  
pp. 1103-1107 ◽  
Author(s):  
C. Mittermayer ◽  
A. Steininger
2009 ◽  
Vol 156-158 ◽  
pp. 487-492 ◽  
Author(s):  
M.V. Zamoryanskaya

In this paper the new method for determination of luminescent centers concentration are discussed. While the possibility of electron traps determination and definition of its activation energy are suggested. The cathodoluminescent (CL) method was used. The determination of luminescent centers concentration in silicon oxide is based on the measurements of dependences of CL intensity on electron beam current. The presence and energy of activation of electron traps were studied by measurement of rise time and decay of luminescent band during the stationary irradiation of silica by electron beam.


1973 ◽  
Vol 63 (2) ◽  
pp. 599-614 ◽  
Author(s):  
M. E. O'Neill ◽  
J. H. Healy

abstract A simple method of estimating source dimensions and stress drops of small earthquakes is presented. The basic measurement is the time from the first break to the first zero crossing on short-period seismograms. Graphs relating these measurements to rise time as a function of Q and instrument response permit an estimate of earthquake source parameters without the calculation of spectra. Tests on data from Rangely, Colorado, and Hollister, California, indicate that the method gives reasonable results.


1996 ◽  
Vol 32 (5) ◽  
pp. 3521-3523 ◽  
Author(s):  
T.C. Arnoldusse ◽  
C. Vo ◽  
M. Burleson ◽  
J.-G. Zhui

1996 ◽  
Vol 43 (3) ◽  
pp. 1626-1628
Author(s):  
M. Kuwata ◽  
H. Maeda ◽  
K. Husimi ◽  
S. Ohkawa ◽  
M. Iwasaki ◽  
...  
Keyword(s):  

1997 ◽  
Vol 45 (2) ◽  
pp. 95 ◽  
Author(s):  
J. D. Roberts

I analysed geographic variation in advertisement call of tetraploid forms of Neobatrachus. Comparing five regional samples spanning the range of N. kunapalari, there was significant geographic variation in pulses per call but not in dominant frequency, pulse rate, pulse duration or percentage rise time. The call of N. kunapalari was significantly different from four other samples covering the geographic range of tetraploid forms across Australia in all but percentage rise time. Calls of frogs from Mt Magnet in Western Australia (WA) differed from calls from Port Hedland (WA) in pulse duration and in multivariate descriptions but were similar in pulse rate. Pulse rates of calls from N. centralis on Eyre Peninsula in South Australia (SA) were distinct from all other populations sampled but in multivariate space these calls were similar to calls of N. sudellifrom eastern Australia. There may be an eastwest cline in call from N. sudelli to calls of N. aquilonius and N. centralis in WA. Call data support the recognition of two tetraploid species: N. kunapalari and N. sudelli. N. sudelli exhibits geographic variation in call, but the status of N. aquilonius and N. centralis as possible synonyms of N. sudelli was not resolved.


1987 ◽  
Vol 23 (5) ◽  
pp. 249-250 ◽  
Author(s):  
A. Blacha ◽  
R. Clauberg ◽  
H.K. Seitz ◽  
H. Beha
Keyword(s):  

1956 ◽  
Vol 76 ◽  
pp. 105-105
Author(s):  
A. Wasserstein

In Vol. LXXV (1955) of the JHS I suggested that the determination of the angular diameters of the sun and the moon ascribed to Thales (Diog. Laertius I. 24) may have been obtained by angular measurement, not as is generally supposed by time-measurement. However, the question of the precise technical method that may have been employed was left open. To measure a very small angle with any degree of accuracy is obviously not easy; and a combination of actual measurement with calculation is probably necessary. In what follows I describe a method of measuring very small angles: whether this was the method employed in obtaining the result ascribed to Thales I do not know; all I can claim is that it presupposes neither mathematical knowledge nor mathematical techniques which could not have been at the disposal of an early Greek philosopher-mathematician.


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