would be changed by about twice the quoted uncertainties. The values given should thus be regarded as uncertain to about this degree.In view of the necessary choice of weights for the various measurements of the proton gyromagnetic ratio and the preliminary nature of the present result, it does not seem desirable to calculate improved values for the atomic constants at this time. It is interesting to note, however, that the present value of the gyromagnetic ratio, when combined with the average of the available proton cyclotron resonance results, 13 gives a value for the Faraday which is about half-way between the values obtained from the iodine and the silver voltameters. 11 ' 12 A new complete adjustment of the constants should be delayed until a number of relevant experiments now under way are completed. At that time the value of the ampere as maintained by the national laboratories will probably be one of the quantities to be adjusted.We would like to express our thanks to the many people at NBS who have contributed to this experiment. In particular we would like to thank L. Costrell who designed the electronic apparatus and R. D. Cutkosky and L. M. Branscomb who collaborated on the early part of the experiment. We are very much indebted to the U. S. Coast and Geodetic Survey for permission to carry out the experiment at the Fredericksburg Magnetic Observatory, and to Mr. R. E. Gebhardt and the members of the Observatory staff for their active cooperation. We should also like to thank M. Packard and A. L. Bloom of Varian Associates for valuable information on freeprecession measurements in the earth's field. ! E. L. Hahn, Phys. iJev. 77, 297 (1950). 2 M. Packard and R. Varian, Phys. Rev. 93, 941 (1954). 3 N. Bloembergen and R. V. Pound, Phys. Rev. 9j>, 8 (1954). 4 P. L. Bender (to be published). 5 This solenoid has also been used in a recent determination of the ampere.