| Автор | Koenigsberger, J. G. |
| Дата выпуска | 1936 |
| dc.description | The accuracy of variometric magnetic measurements is not often checked as such observations of different decades are not comparable. The question arises—similarly as now found by comparison of observations with the pendulum and gravity‐variometer—if the magnetic variometer may give also for greater distances results of the same accuracy as absolute methods. There is an opportunity for such a comparison in Switzerland. For 1931.5 W. Brückmann<sup>1</sup> has made absolute measurements, designated as 1, below, of the magnetic elements, his results being published late in 1932, and for 1930.5 the author has measured the horizontal and vertical components H and Z with a variometer, designated as 2, below, on a profile 200 km long through the same country from Chiasso to Basel, published early in 1932<sup>2</sup>. |
| Формат | application.pdf |
| Копирайт | Copyright 1936 by the American Geophysical Union. |
| Название | A comparison between absolute and variometric magnetic measurements |
| Тип | article |
| DOI | 10.1029/TE041i004p00353 |
| Electronic ISSN | 0096-8013 |
| Print ISSN | 0096-8013 |
| Журнал | Terrestrial Magnetism and Atmospheric Electricity |
| Том | 41 |
| Первая страница | 353 |
| Последняя страница | 354 |
| Выпуск | 4 |
| Библиографическая ссылка | , Erdmagnetische Vermessung der Schweiz, Ann. Schweiz. Met. Centralanst., 68Nr. 6, 1932. |
| Библиографическая ссылка | , Beitr. angew. Geophysik,2,374–400 (1932); see also Terr. Mag., 36, 243–249, 374 (1931). The average volume‐susceptibility K of 200 rocks on the Alpine tract of the profile Luzern‐Bellinzona is +6×10<sup>−6</sup>, taking account of the area occupied by the single rocks. |
| Библиографическая ссылка | See p.377,Beitr. angew. Geophysik,2 (1932). |
