The coherent neutron scattering length density is atomic number density times scattering length:
The density was converted to to match the molar mass in grams per mole, and .
Use the water data to determine the common oxygen contribution rather than assume identical molar volumes. Ordinary water has molecular number density
so . Therefore and
The assumptions are isotopically pure waters, additive nuclear scattering lengths, the same oxygen isotope contribution, and molar masses approximately and . Equal molar volumes would give the rougher estimate .
Assuming additive liquid volumes, the scattering length density is linear in DO volume fraction :
where all scattering length densities are in . The of heavy water occupies about . The required ordinary-water volume is
Thus add approximately of HO. Volume fraction, rather than mass fraction, enters this contrast-matching equation. Isotope exchange to form HDO does not change the total nuclear scattering-length balance in the additive-volume approximation.
Without the film, a sharp silicon-water boundary gives the usual Fresnel-like reflectivity governed by its scattering-length-density contrast. If the contrast-matched mixture from part (iii) is used, that ideal interface signal is strongly suppressed.
Polyethylene has a different scattering length density from both matched media. Its two interfaces generate interference oscillations, or Kiessig fringes, in reflectivity versus normal momentum transfer . Their approximate spacing is
for . Fit several fringes, with refraction, roughness and instrument resolution included if necessary, to determine the thickness accurately. Even with unmatched water the film changes the reflection envelope and adds thickness-dependent interference.

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