TITLE nap : Persistent Na-current nu v en ko afhankelijk : boltzman met halfmaximale concentratie = 7mM : en activatie bij 3.5mM (1%) : simple, with no inactivation-gate : tau_activation = constant, 6ms : tau_inactivation = very slow; 50000 keer trager dan tau_inact_m^3*h : : Activation from -60mV, peak at -10 mV : : Tweede poging door toevoeging inactivation gate met : zelfde voltage gevoeligheid als Traub's m^3*h kanaal : maar dan 100 keer langzamer. : : door aanpassing van het model CaChan. : A Molecular Model of Low-Voltage-Activated Calcium Conductance : van Wang? UNITS { (molar) = (1/liter) (mV) = (millivolt) (mA) = (milliamp) (mM) = (millimolar) } INDEPENDENT {t FROM 0 TO 1 WITH 100 (ms)} NEURON { SUFFIX nap USEION k READ ko USEION na READ nai, nao, ena WRITE ina GLOBAL ina_p_h, tau_act, conc_half, helling RANGE gnabar, ina } UNITS { :FARADAY = (faraday) (coulomb) FARADAY = 96485.309 (coul) R = (k-mole) (joule/degC) } PARAMETER { celsius (degC) gnabar=1e-6 (mho/cm2) : Maximum Permeability .2e-3*5 hans helling=-.765 (mM) : K-slope of boltzman conc_half=7 (mM) : conc. for halfmax. activation ina_p_h = 25000 (ms) :taufactor tov snelle na-stroom tau_act = 6 (ms) } ASSIGNED { ina (mA/cm2) ena (mV) v (mV) nai (mM) : <-vanwege deze nao (mM) : <-en deze regel. ko (mM) } STATE { ma mb ha hb } : fraction of states, m=fraction in open state. BREAKPOINT { SOLVE nastate METHOD sparse :boltzman() ina = gnabar*ma*ma*ha*kdep(ko)*(v-ena) :*ghk(v,nai,nao) :ma = 1 - mb :ha = 1 - hb } INITIAL { :SOLVE nastate STEADYSTATE sparse ma=m_inf(v) mb=1-ma ha=h_inf(v) hb=1-ha ina = gnabar*ma*ma*ha*kdep(ko)*(v-ena) :*ghk(v,nai,nao) } LOCAL a1,a2,b1,b2 KINETIC nastate { a1 = m_a(v) a2 = m_b(v) b1 = h_a(v) b2 = h_b(v) ~ mb <-> ma (a1, a2) ~ hb <-> ha (b1, b2) CONSERVE ma + mb = 1 CONSERVE ha + hb = 1 } FUNCTION kdep(ko (mM)) { TABLE DEPEND conc_half, helling FROM 0 TO 150 WITH 150 kdep=1+ 2/(1+exp((ko-conc_half)/helling)) } FUNCTION m_a(v(mV)) { :LOCAL m_inf TABLE FROM -150 TO 150 WITH 200 :if (v<=-70) { : m_inf=0 :}else{ : m_inf=1/(1+(exp(-(v+39.7)/7.0))) :} m_a = m_inf(v)/tau_act } FUNCTION m_inf(v) { TABLE FROM -150 TO 150 WITH 200 m_inf=1/(1+(exp(-(v+39.7)/7.0))) } FUNCTION m_b(v(mV)) { :LOCAL m_inf TABLE FROM -150 TO 150 WITH 200 :m_inf=1/(1+(exp(-(v+39.7)/7.0))) m_b = (1-m_inf(v))/tau_act } FUNCTION h_a(v(mV)) { TABLE FROM -150 TO 150 WITH 200 h_a = (1/ina_p_h)*(0.128*exp((7-v-70)/18)) } : 37 was 17 FUNCTION h_b(v(mV)) { TABLE FROM -150 TO 150 WITH 200 h_b = (1/ina_p_h)*4/(1+exp((30-v-70)/5)) } : 60 was 40 FUNCTION h_inf(v) { TABLE FROM -150 TO 150 WITH 200 h_inf=h_a(v)/(h_a(v)+h_b(v)) } FUNCTION ghk(v(mV), ci(mM), co(mM)) (.001 coul/cm3) { LOCAL z, eci, eco z = (1e-3)*1*FARADAY*v/(R*(celsius+273.11247574)) : *1* -> valentie kalium eco = co*efun(z) eci = ci*efun(-z) :high nao charge moves inward, mogelijke fouten vanwege oorsprong Ca(2+)! :negative potential charge moves inward ghk = (.001)*1*FARADAY*(eci - eco) } FUNCTION efun(z) { if (fabs(z) < 1e-4) { efun = 1 - z/2 }else{ efun = z/(exp(z) - 1) } }