32
SYSTEM
so:
Equation17
g
s
=
ρ
D
vapor
e
s
(T
a1
)(1− h
r1
)
⎡
⎣
⎤
⎦
d
2
h
e
(T
) − h
e
(T
)
− d
1
Therefore, g
s
is a function of the distances between RH sensors, temperature, and the two
RHreadings.
When the conductance is small, the humidities are nearly the same, and the denominator of
the denominator of Equation18 goes to 0, causing problems. Multiplying top and bottom by
the denominator gives
Equation18
g
s
=
ρ
D
vapor
h
r1
e
s
(T
a1
) − h
r 2
e
s
(T
a2
)
⎡
⎣
⎤
⎦
e
(T
)(1− h
)
⎡
⎤
d
− h
e
(T
) − h
e
(T
)
⎡
⎤
d
NOTE: The resulting g
s
is in units of mol/m
2
s.
For this theory to accurately predict the stomatal conductance using the steady-state
diffusion technique, true steady-state conditions must exist in the diffusion path.
The amount of time necessary to reach steady-state conditions is proportional to the
conductance. At conductances <20 mmol/(m
2
s), steady-state conditions are generally
reached in <5 min. At higher conductances, steady-state conditions can take up to 30 min
and can become inaccurate.