Dermal Heat Transport Analysis for Transcutaneous O2 Measurement
Abstract
Heat from a transcutaneous oxygen electrode is transmitted locally to the blood beneath it causing a shift in the HbO2 dissociation curve. This increases the local PO2, and allows a measurable PO2, at the skin surface. The temperature effect on the HbO2, curve must be accounted for in in vivo calibration of Ptco2, data. To do this, the capillary blood temperature beneath the electrode must be known. A heat balance is written around the capillary blood with heat being conducted in from the electrode and carried out by two means: conduction to deep tissue; and transport away by the flowing capillary blood. The following equation is the steady state solution of the heat transport problem:
T8 = ±
where Z = ± = 0.17
T8, = capillary blood temperature
T1 = electrode temperature
To = body temperature
ρ = blood density
P = cutaneous perfusion
δ = dermal capillary depth
k = thermal conductivity of skin
C± = heat capacity of blood
This solution shows the capillary blood temperature may be calculated if the T1 and To are measured and the physiologic constants in 2 are known. 2 is a dimensionless heat transport number which represents the relative importance of perfusion to conduction effects on the deterring T8, and may be used as a data correlating parameter. Z = 0.17 is obtained using literature values for the physiological constants. This analysis used in conjunction with a mass transport analysis for oxygen will produce a theoretically based correlation scheme for in vivo calibration of heated transcutaneous oxygen electrodes.