| Abstract: | Summary It is pointed out here that instead of adjustment of the  g-values at theEötvös Torsion Balance measurements, it is better to adjust the gradients of gravity themselves by wich we can achieve uniformity between the gradients and the g-values i. e. isogammes, free of contradiction by the calculation from these gradients. The corrections are not to be attached to the total gradients, but to the measured gradients in directionx andy. Remarks to the choise of weight of adjust and to the rejection of systematic errors. Common correction of Torsion Balance and Gravimeter measurements. In appendix it is given an complety counted example.
Ungarischen Komitees der Union Géodésique et Géophysique Internationale, ord. Mitglied der Ung. Akademie der Wissenschaften Sopron, Technische Universität. |
