alike as possible, except that they are placed in different solutions. The electrode holders are now pressed against the ends of the roll of disks, the block, M, is firmly fastened by means of the set screw, N, and the screw, F, is turned until the electrode holders are tightly clamped against the roll of disks. The pressure used in this operation should be fairly uniform.T he apparatus is now lifted out of the sea water• It was at first thought necessary to use a dynamometer, but it was found that the operator soon becomes so proficient as to make it unnecessary. The resistance is very little affected by vuriations in pressure. 'In the earlier experiments the resistance was taken with the cylinder submerged in sea water, and this may be preferable in special cases. MEASURING ELECTRICAL CONDUCTIVITY 27 and allowed to drain^for a definite time (not over one minute) after which the resistance becomes practically constant. The current passes for a short distance through sea water before reaching the disks. There is a film of sea water between each pair of disks and likewise a film around the cut edges. Otherwise the current passes only through the tissue. As soon as the resistance has been measured the apparatus is replaced in sea water; the set screw, N, is loosened so that the electrode holders can be moved apart and the disks separated from each other by means of forceps. After standing for a few minutes in sea water the resistance is again determined. The disks are then separated as before and allowed to stand in sea water. This procedure is continued until it becomes evident that the resistance is practically stationary.T he apparatus is then transferred to another solution (e, g., NaCl 0.52 M) having the same conducti\dty (and temperature^^) as the sea water. There should be at least 1,500 cc. of solution, contained in a shallow dish of glass or enameled ware. The disks are at once separated by means of forceps and thoroughly rinsed ' Each support rests on a block of paraffin. Care must be taken that there is no conduction between the blocks; e.g., along the wet surface of ihe tabla 'For the literature see Robertson, T. B. (1906, 1910, pp. 238, 311). Also Szucs (1912). "All the solutions had the same conductivity as sea water. 225 Bugarsky, 21, 225 Burgess, 176 Cadmium, effect on conductivity, 46 Caesium, penetration of, 203, 214 Caffeine, antagonism of, 171 ff effect on conductivity, 171 ff, 194