770 36 Thermography to Measure Water Relations of Plant
Leaves
The transfer velocity kheat can be defined as the ratio of
the diffusion coefficient D to the diffusion length
∆x:
∆cwv is the difference between water vapor concentrations
inside the leaf and in the surrounding turbulent air. The concentrations
can be ex-pressed as relative humidities (fractions of the water vapor
saturation concentration at the given temperature):
Equation (36.2) can now be expressed by the individual contributing
terms:
A |
leaf |
dt |
|
(36.15)
|
+2kleaf heatρ cp (Tair −
Tleaf) + kwv λ cwv (hleaf − hair)
|
� |
C
A |
+ 2αleaf IRσ�T4 ref− T 4
leaf�+ 2ρcp�kleaf heat−αleaf
αref IR IRkref heat�Tair
+ 2ρcp�αleaf αref IR
IRkref heatTref − kleaf
heatTleaf�+ jlat
|
|