By combining observations of the J = 1 --> 0 transitions of (CO)-O-18
and (HCO+)-C-13, and the J = 1 --> 0 and 2 --> 1 transitions of DCO+,
and a model of molecular cloud chemistry, we have obtained the electro
n abundance (X-e drop n(e)/n(H2)) in a sample of 20 low-mass and 7 hig
h-mass molecular cloud cores. We find that the electron abundances are
confined to a relatively narrow range of -7.5 < log(X-e)< -6.5 with v
ery little scatter about the mean values of < log(X-e)> = -7.04; sigma
= 0.22 (low-mass cores) and < log(X-e)> = -7.11; sigma = 0.15 thigh-m
ass cores). These values are consistent with the standard view that th
e ionization in dense cloud cores is dominated by cosmic rays, provide
d that zeta(H2) approximate to 5 x 10(-17) s(-1). These electron abund
ances also imply that the neutrals are only marginally coupled to the
magnetic field (W approximate to 5-8) with only ca. 10% the core radiu
s being cut off from magneto-hydrodynamic (MHD) wave propagation. The
coupling parameter (RI) also suggests that ambipolar diffusion timesca
les are about an order of magnitude larger than the freefall timescale
.