Interstellar scintillation (ISS), fluctuations in the amplitude and ph
ase of radio waves caused by scattering in the interstellar medium, is
important as a diagnostic of interstellar plasma turbulence. ISS is a
lso of interest because it is noise for other radio astronomical obser
vations. The unifying concern is the power spectrum of the interstella
r electron density. Here we use ISS observations through the nearby (l
ess than or similar to 1 kpc) ISM to estimate the spectrum. From measu
rements of angular broadening of pulsars and extragalactic sources, de
correlation bandwidth of pulsars, refractive steering of features in p
ulsar dynamic spectra, dispersion measure fluctuations of pulsars, and
refractive scintillation index measurements, we construct a composite
structure function that is approximately power law over 2 x 10(6) m <
scale < 10(13) m. The data are consistent with the structure function
having a logarithmic slope versus baseline less than 2; thus there is
a meaningful connection between scales in the radiowave fluctuation f
ield and the scales in the electron density field causing the scatteri
ng. The data give an upper limit to the inner scale, l(0), less than o
r similar to 10(8) m and are consistent with much smaller values. We c
onstruct a composite electron density spectrum that is approximately p
ower law over at least the approximate to 5 decade wavenumber range 10
(-13) m(-1) < wavenumber < 10(-8) m(-1) and that may extend to higher
wavenumbers. The average spectral index of the electron density over t
his wavenumber range is approximate to 3.7, very close to the value ex
pected for a Kolmogorov process. The outer scale size, L(0), must be g
reater than or similar to 10(13) m (determined from dispersion measure
fluctuations). When the ISS data are combined with measurements of di
fferential Faraday rotation angle, and gradients in the average electr
on density, constraints can be put on the spectrum at much smaller wav
e numbers. The composite spectrum is consistent with a Kolmogorov-like
power law over a huge range (10 or more decades) of spatial wavenumbe
r with an inferred outer scale, L(0) greater than or similar to 10(18)
m. This power-law subrange-expressed as ratio of outer to inner scale
s-is comparable to or larger than that of other naturally occurring tu
rbulent fluids, such as the oceans or the solar wind. We outline some
of the theories for generating and maintaining such a spectrum over th
is huge wavenumber range.