The London, Edinburgh and Dublin Philosophical Magazine and Journal of ScienceTaylor & Francis, 1904 - English periodicals |
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Results 1-5 of 100
Page 5
... taken to be a normal one , and there can be no intrinsic difference between the bands seen in this case and those observed when a grating of the same resolving power is used . It has been shown by Lord Rayleigh that in all questions ...
... taken to be a normal one , and there can be no intrinsic difference between the bands seen in this case and those observed when a grating of the same resolving power is used . It has been shown by Lord Rayleigh that in all questions ...
Page 9
... taken . This latter consideration was one of which he not infrequently made use ; I recall that he once em- ployed it to reconcile conflicting views as to the interpretation of Fourier's series in a discussion which arose in the columns ...
... taken . This latter consideration was one of which he not infrequently made use ; I recall that he once em- ployed it to reconcile conflicting views as to the interpretation of Fourier's series in a discussion which arose in the columns ...
Page 10
... ( taken with the negative sign ) corresponds to the entropy of any body which the ensemble is capable of representing , and we are no more concerned about the 7 of a single system ( except in so far as a knowledge of it may be necessary ...
... ( taken with the negative sign ) corresponds to the entropy of any body which the ensemble is capable of representing , and we are no more concerned about the 7 of a single system ( except in so far as a knowledge of it may be necessary ...
Page 16
... taken 268 , to agree with the value used in Physics of the Earth's Crust , ' but the discrepancy is immaterial . C My calculations give the deflexions in a direction perpen- dicular to the range , and not in the meridian , and it is not ...
... taken 268 , to agree with the value used in Physics of the Earth's Crust , ' but the discrepancy is immaterial . C My calculations give the deflexions in a direction perpen- dicular to the range , and not in the meridian , and it is not ...
Page 17
... taken to represent the mountain , agree with those of the actual highlands as regards their horizontal attraction , we may reduce the deflexions thus obtained to the meridian by multi- plying them by cosine 45 ° , and compare the ...
... taken to represent the mountain , agree with those of the actual highlands as regards their horizontal attraction , we may reduce the deflexions thus obtained to the meridian by multi- plying them by cosine 45 ° , and compare the ...
Contents
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Common terms and phrases
absorption æther aggregate Aleph alternating current ampere angle anode antenna apparatus arrangement atom basalt calculated canal rays cardinal number cathode rays cell cent charge colours conductivity connexion constant corpuscles corresponding curve cylinder Dattenberg deflexion density diameter direct current direction distance doublet electric electrodes electrometer emanation emission energy equal equation excited activity experiments galvanometer gases given glass heating effect hydrogen increase ionization ions isostacy J. J. Thomson length light liquid magnetic maximum means measured mercury mercury vapour metal method molecules negative number of corpuscles observed obtained ordinal oscillations paper particles Phil plane plate platinum polarization position potential pressure produced Prof radiation radioactivity radium radium bromide reflecting-power resistance ring rotation selenide selenium shown surface temperature theory thickness tube velocity vibration volts wave-length waves wire