ABSTRACTis low (ri = 1-2 sec cml). When Tleaf-Tup = 5 C, the ratio drops below 0.5. Under high leaf resistance conditions (rz = 10-50 sec cm-') the comparable ratios are approximately 0.9 and 0.7, respectively. sensor which is sensitive over a narrow range of relative humidity at the low end of the relative humidity range. In operation, the cup is dried by air from a silica gel dehydrator. It is then placed over the leaf. Transpiration proceeds, the humidity in the cup increases, and the time required for the sensor to respond over a narrow, prescribed (usually 1-2%) range is determined.Since the relative humidity at the sites of evaporation within the leaf is close to 100% (it is generally assumed to be the saturation vapor pressure at the leaf temperature [7]), and since the humidity sensor is observed over a narrow range at the low end of the relative humidity scale (say, 18-20%), the water vapor concentration difference from leaf to air is assumed to be constant during the period of measurement. Consequently, the transpiration rate (E) can be assumed to be steady during the period of measurement and inversely proportional to the time-lapse (At) which occurs as the sensor responds over the measurement range.Calibration is based on the frequently used transpiration equation:During the past few years the water vapor diffusion porometer (1,4,8,9) has become a widely used tool for field studies of stomatal resistance, replacing, to a considerable degree, other types of porometers which measure viscous air flow or some other parameter.The attraction of the diffusion porometer is that it measures the actual diffusive resistance of the leaf to water vapor movement, and the transfer processes and pathways that are involved are essentially the same as in natural transpiration. These where eleaf (mm Hg) is the saturation vapor pressure at Tleaf and ecup (mm Hg) is the actual vapor pressure at the mid-point of the measurement range, and at Tcup; Cleaf and ccup (g cm-') are the corresponding water vapor concentrations. The coefficient a converts vapor pressure in mm Hg to water vapor concentration in g cm73. (It has the value 2.89 X 104 e/T when T is in degrees Kelvin). The term ra (sec cm7l) is the diffusive resistance external to the leaf (i.e., of the porometer cup itself) and r1 (sec cm-l) is the diffusive resistance of the leaf. Since E = k/At, where k is a coefficient of proportionality, this expression can be rewritten asAt any one level of Tleaf and T,u,X the right hand side of equation (2) is a constant, so (ra + rl) can be uniquely determined, for any one porometer system, by measurements of At. Calibration is generally carried out by determining At when the porometer is located over a range of perforated Plexiglas plates, the diffusive resistance of which is calculated from diffusion theory (4). At the base of each plate is a layer of wet blotting paper to simulate the sites of evaporation within the leaf.Since water vapor must diffuse from the sites of evaporation through the perforations in each plate, and...