TITLE Potassium Ih channel for STh
COMMENT
Ih from Huguenard & McCormick 92 LGN relay
Magee (1998) shows Ih to have a reversal potential that is ionic non
specific with a reversal potential of around -30mV.
Huguenard recordings at 35.5degC.
How the q10 works: There is a q10 for the rates (alpha and beta's)
called Q10 and a Q10 for the maximum conductance called gmaxQ10. The
q10s should have been measured at specific temperatures temp1 and
temp2 (that are 10degC apart). Ideally, as Q10 is temperature
dependant, we should know these two temperatures. We used to
follow the more formal Arrhenius derived Q10 approach. The
temperature at which this channel's kinetics were recorded is tempb
(base temperature). What we then need to calculate is the desired
rate scale for now working at temperature celsius (rate_k). This was
given by the empirical Arrhenius equation, using the Q10, but now is
using the quick Q10 approximation.
ENDCOMMENT
UNITS {
(mV) = (millivolt)
(mA) = (milliamp)
}
INDEPENDENT {t FROM 0 TO 1 WITH 1 (ms)}
NEURON {
SUFFIX Ih
NONSPECIFIC_CURRENT ih
RANGE gk
GLOBAL eih,activate_Q10,Q10,gmaxQ10,rate_k,gmax_k,temp1,temp2,tempb
}
PARAMETER {
v (mV)
dt (ms)
gk = 0.001 (mho/cm2)
eih = -5.611047394e+01 (mV)
celsius
activate_Q10 = 1
Q10 = 2.0
gmaxQ10 = 2.0
temp1 = 25.0 (degC)
temp2 = 35.0 (degC)
tempb = 35.5 (degC)
}
STATE {
f
}
ASSIGNED {
ih (mA/cm2)
finf
ftau (ms)
rate_k
gmax_k
}
BREAKPOINT {
SOLVE integrate METHOD cnexp
ih = (gk*gmax_k)*f*(v-eih)
}
UNITSOFF
INITIAL {
LOCAL ktemp,ktempb,ktemp1,ktemp2
if (activate_Q10>0) {
rate_k = Q10^((celsius-tempb)/10)
gmax_k = gmaxQ10^((celsius-tempb)/10)
}else{
rate_k = 1.0
gmax_k = 1.0
}
setinf(v)
f = finf
}
DERIVATIVE integrate {
setinf(v)
f' = (finf - f)/ftau
}
PROCEDURE setinf(v) {
:Voltage shift (for temp effects) of 5.0.
TABLE finf, ftau DEPEND celsius FROM -100 TO 100 WITH 400
finf = 1.0/(1+exp((v + 80 )/ 5.5))
ftau = (1.0/(exp(-15.02 - 0.086*v)+exp(-1.5195 + 0.0701*v))) /rate_k
}
UNITSON