70
I I I
q V I R
AKT
0
0
1
ª
¬
«
º
¼
»
®
°
¯ °
½
¾
°
¿ °
g
s at
o
s
exp
(4.25)
where A represents the dimensionless factor, K represents the kinetic energy, T is
the standard temperature at kelvin, q represents the charges, V represents the volts,
and R represents the resistance under varying weather conditions.
Then the incremental conductance (IC) is calculated to determine the maximum
volts which is configured in accordance to the MPP volts by determining the conductance values of V–I circuit (dI/dV and I/V, calculatively) (Fig. 4.9). Thus, this
result suggests overcoming the limitations of IC to calculate the sign of dP/dV to
deliver net current flow from the geothermal energy of dP/dV = 0, and is expressed
as follows:
Fig. 4.8 The functional block diagram of net energy functional current and min-volt reaction current formation from the generator
4 Geothermal Energy
I I I
q V I R
AKT
0
0
1
ª
¬
«
º
¼
»
®
°
¯ °
½
¾
°
¿ °
g
s at
o
s
exp
(4.25)
where A represents the dimensionless factor, K represents the kinetic energy, T is
the standard temperature at kelvin, q represents the charges, V represents the volts,
and R represents the resistance under varying weather conditions.
Then the incremental conductance (IC) is calculated to determine the maximum
volts which is configured in accordance to the MPP volts by determining the conductance values of V–I circuit (dI/dV and I/V, calculatively) (Fig. 4.9). Thus, this
result suggests overcoming the limitations of IC to calculate the sign of dP/dV to
deliver net current flow from the geothermal energy of dP/dV = 0, and is expressed
as follows:
Fig. 4.8 The functional block diagram of net energy functional current and min-volt reaction current formation from the generator
4 Geothermal Energy