We report on a recent determination of the Newtonian constant of gravity, G
, using a new 'free fall' method. This method uses a freely falling test ob
ject to sense the gravitational field of a ring-shaped mass placed alternat
ely above and below the drop region. The measurement of the changes in acce
leration of the test object allow determination of G. Because the test mass
is unsupported, systematic errors associated with the free fall method are
significantly different from those of the traditional torsion experiments
that constitute the great majority of G measurements. This characteristic m
akes this method potentially valuable in the context of today's uncertainty
about the value of G.
The raw data have been examined in a variety of ways. We describe our metho
ds which allow us to extract, besides G, information about various experime
ntal parameters and possible systematic errors. A number of sources of syst
ematic errors have been investigated, including magnetic and vibratory sign
als arising from the dropping action of our apparatus. We outline the steps
we have taken to ascertain the magnitude of errors introduced by these eff
ects.
Using the free fall method, we have completed a determination of G, obtaini
ng a result of G = (6.6873 +/- 0.0094) x 10(-11) m(3) kg(-1) s(2).