The conserved-vector-current theory of the strangeness-conserving weak decays predicts that Gv, the vector coupling constant in nuclear beta decay, should be equal to G>, the coupling constant in the muon decay. To make possible a more precise comparison of Gv and G>, the ft value of O 14 has been remeasured. The endpoint energy of the positron decay has been determined by measuring the Q values of the reactions C 12 (He»0 14 and C 12 (He 3 ,^)N 14 * (2.311-MeV state), using the same techniques and equipment where possible in order to minimize the uncertainty in the difference of the Q values. The results of these measurements are Q n = -1148.8±0.6 keV and &=2468.4=b 1.0 keV, which yield £max(0 + ) = 1812.6±1.4 keV, all energies relative to the Li 7 (M) Be7 threshold assumed as 1880.7d=0.4 keV. The half-life of O 14 has also been remeasured as 71.00±0.13 sec, which implies a partial halflife of 7l.43±0.15 sec for the transition to the 2.311-MeV state of N 14 . Averaged with the recent half-life measurement of Hendrie and Gerhart, we obtain an ft value of 3075±10 sec for the O 14 decay, after correcting for nuclear form factors, electron screening, and if-capture competition. With the radiative corrections of Kinoshita and Sirlin, the value obtained for G v is (1.4025 ±0.0022) X 10~4 9 erg-cm 3 , where the quoted error is experimental in origin. This is to be compared with the value computed from recent muon decay measurements, G>= (1.4312=1=0.0011) X10~4 9 erg-cm 3 , which is (2.0=1=0.2)% larger. As there appear to be several possible theoretical explanations for this small discrepancy, the present results are consistent with the conserved-vector-current hypothesis.