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Autor:
J D W Abernethy
Publikováno v:
Physics Bulletin. 24:591-593
Suppose that one were given the task of measuring the magnetism of a rock sample in the presence of the unavoidable and much larger magnetic field of the earth, or of measuring a weak infrared signal in a warm laboratory. In both cases the signal of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::515dbf709eada64276ee1a57cbe170c9
https://doi.org/10.1088/0031-9112/24/10/012
https://doi.org/10.1088/0031-9112/24/10/012
