Inspection of
Figure 3 demonstrates that semilogarithmic linear behavior emerges only at a later time. Therefore, to obtain the corneal oxygen-consumption rate constant, we evaluate Equation 8 at later time, where the measured partial pressure approaches the final steady state
in Equation 9 is the longest time constant in Equation 8 and, therefore, controls long-time behavior. Appendix A (see Supplementary Material and Supplementary
Appendix A) demonstrates that
P(∞,0)/
P(
t,0) < 1 so
P(∞,0) can safely be neglected in Equation 9 or
This result indicates that at long times, a semilogarithmic graph of the polarographic-measured partial pressure versus time yields a straight line with negative slope α
1.
Figure 4 confirms this assertion and illustrates typical best eye-fit straight lines whose slopes give α
1 for each repeat experiment. Given the experimentally determined value of α
1, the metabolism rate constant is available in
Appendix A (see Eq. A16 for
n = 1; see Supplementary Material and Supplementary
Appendix A and Eq. A16)
where
b1 is established by trial-and-error from (see Eq. A15 for
n = 1; see Supplementary Material and Supplementary Eq. A15)
where
β = DkLm/(
DmkmL) is the ratio of diffusion resistance in the membrane to that in the cornea. Hence, to establish the metabolic rate constant, the diffusive properties of both the cornea and the probe membrane must be known. In
Table 1, we adopt an average value of
D and
k characteristic of the stroma
1–3,71 and reported literature values for
Dm and
km.
40,68–70 Resulting values for
β and
b1 are also listed in Table 1. Different polarographic probes may be fitted with differing membrane materials and with differing thicknesses, so
β must be determined for each instrument. Once φ and
b1 are calculated from Equations 11 and 12, oxygen uptake follows from Equation 7. Thus, from the measured linear semilogarithmic slope of the tension decline at later times, α
1, oxygen uptake follows from application of Equations 7, 11, and 12.