Source: Hedderich, Sachs and Reynarowych, Applied Statistics: Methods Using R,
section 8.4.4, printed page 834, equation (8.63): log psi(a, b) = beta1 (b -
a), so psi(a, b) = exp(beta1 (b - a)). The intercept cancels, so the odds
ratio for moving the predictor from a to b depends on beta1 and the span alone.
Details
A Wald interval is supplied when se is given: the log odds
ratio is beta1 (b - a) with standard error
abs(b - a) se(beta1), which is (8.56) transported through the
same linear map.
Book worked example, same page: from the Challenger data the book
estimates beta1 = -0.2322; a temperature rise of 10 degF gives
psi(10) = exp(-2.322) = 0.098 and a drop of 10 degF gives
psi(-10) = exp(2.322) = 10.2.
