Lecture 4: Diffusion and the Fokker-Planck equation Outline: • intuitive treatment • Diffusion as flow down a concentration gradient • Drift current and Fokker-Planck equation Lecture 4: Diffusion and the Fokker-Planck equation Outline: • intuitive treatment • Diffusion as flow down a concentration gradient • Drift current and Fokker-Planck equation • examples: • No current: equilibrium, Einstein relation • Constant current, out of equilibrium: Lecture 4: Diffusion and the Fokker-Planck equation Outline: • intuitive treatment • Diffusion as flow down a concentration gradient • Drift current and Fokker-Planck equation • examples: • No current: equilibrium, Einstein relation • Constant current, out of equilibrium: • Goldman-Hodgkin-Katz equation • Kramers escape over an energy barrier Lecture 4: Diffusion and the Fokker-Planck equation Outline: • intuitive treatment • Diffusion as flow down a concentration gradient • Drift current and Fokker-Planck equation • examples: • No current: equilibrium, Einstein relation • Constant current, out of equilibrium: • Goldman-Hodgkin-Katz equation • Kramers escape over an energy barrier • derivation from master equation Diffusion Fick’s law: J D P x Diffusion Fick’s law: J D P x cf Ohm’s law I g V x Diffusion Fick’s law: conservation: J D P x P J t x cf Ohm’s law I g V x Diffusion Fick’s law: conservation: => J D P x P J t x P 2 P D 2 t x cf Ohm’s law I g V x Diffusion Fick’s law: conservation: => J D P x P J t x P 2 P D 2 t x cf Ohm’s law I g diffusion equation V x Diffusion Fick’s law: J D conservation: => initial condition P x P J t x P 2 P D 2 t x P(x | 0) (x) cf Ohm’s law I g diffusion equation V x Diffusion Fick’s law: J D conservation: => initial condition solution: P x P J t x P 2 P D 2 t x cf Ohm’s law I g diffusion equation P(x | 0) (x) x 2 1 P(x | t) exp 4Dt 4Dt V x Diffusion Fick’s law: J D conservation: => initial condition solution: P x P J t x P 2 P D 2 t x cf Ohm’s law I g V x diffusion equation P(x | 0) (x) x 2 1 P(x | t) exp 4Dt 4Dt http://www.nbi.dk/~hertz/noisecourse/gaussspread.m Drift current and Fokker-Planck equation Jdrift (x,t) u(x)P(x,t) Drift (convective) current: Drift current and Fokker-Planck equation Drift (convective) current: Jdrift (x,t) u(x)P(x,t) Combining drift and diffusion: Fokker-Planck equation: P Jdrift Jdiff t x Drift current and Fokker-Planck equation Drift (convective) current: Jdrift (x,t) u(x)P(x,t) Combining drift and diffusion: Fokker-Planck equation: P J drift J diff t x P 2P u(x)P D u(x)P D 2 x x x x Drift current and Fokker-Planck equation Drift (convective) current: Jdrift (x,t) u(x)P(x,t) Combining drift and diffusion: Fokker-Planck equation: P J drift J diff t x P 2P u(x)P D u(x)P D 2 x x x x Slightly more generally, D can depend on x: Jdiff (x,t) D(x)P(x,t) x Drift current and Fokker-Planck equation Drift (convective) current: Jdrift (x,t) u(x)P(x,t) Combining drift and diffusion: Fokker-Planck equation: P J drift J diff t x P 2P u(x)P D u(x)P D 2 x x x x Slightly more generally, D can depend on x: Jdiff (x,t) D(x)P(x,t) x P 2 => u(x)P 2 D(x)P t x x Drift current and Fokker-Planck equation Drift (convective) current: Jdrift (x,t) u(x)P(x,t) Combining drift and diffusion: Fokker-Planck equation: P J drift J diff t x P 2P u(x)P D u(x)P D 2 x x x x Slightly more generally, D can depend on x: Jdiff (x,t) D(x)P(x,t) x P 2 => u(x)P 2 D(x)P t x x First term alone describes probability cloud moving with velocity u(x) Second term alone describes diffusively spreading probability cloud Examples: constant drift velocity http://www.nbi.dk/~hertz/noisecourse/gaussspreadmove.m Examples: constant drift velocity http://www.nbi.dk/~hertz/noisecourse/gaussspreadmove.m Solution (with no boundaries): u(x) u0 P(x,t) x u t 2 1 0 exp 4Dt 4Dt Examples: constant drift velocity http://www.nbi.dk/~hertz/noisecourse/gaussspreadmove.m Solution (with no boundaries): u(x) u0 P(x,t) Stationary case: x u t 2 1 0 exp 4Dt 4Dt Examples: constant drift velocity http://www.nbi.dk/~hertz/noisecourse/gaussspreadmove.m Solution (with no boundaries): u(x) u0 P(x,t) x u t 2 1 0 exp 4Dt 4Dt Stationary case: in gravitational field: u0 = μF = -μmg Gas of Brownian particles Examples: constant drift velocity http://www.nbi.dk/~hertz/noisecourse/gaussspreadmove.m Solution (with no boundaries): u(x) u0 P(x,t) x u t 2 1 0 exp 4Dt 4Dt Stationary case: in gravitational field: u0 = μF = -μmg Gas of Brownian particles μ =mobility Examples: constant drift velocity http://www.nbi.dk/~hertz/noisecourse/gaussspreadmove.m u(x) u0 Solution (with no boundaries): P(x,t) x u t 2 1 0 exp 4Dt 4Dt Stationary case: in gravitational field: u0 = μF = -μmg Gas of Brownian particles μ =mobility Boundary conditions (bottom of container, stationarity): P(x) 0, x 0; J(x) 0 Examples: constant drift velocity http://www.nbi.dk/~hertz/noisecourse/gaussspreadmove.m u(x) u0 Solution (with no boundaries): P(x,t) x u t 2 1 0 exp 4Dt 4Dt Stationary case: in gravitational field: u0 = μF = -μmg Gas of Brownian particles μ =mobility Boundary conditions (bottom of container, stationarity): P(x) 0, x 0; J(x) 0 drift and diffusion currents cancel Einstein relation m gP(x) D FP equation: dP 0 dx Einstein relation dP 0 dx FP equation: m gP(x) D Solution: m g m gx P(x) exp D D Einstein relation dP 0 dx FP equation: m gP(x) D Solution: m g m gx P(x) exp D D But from equilibrium stat mech we know m g m gx P(x) exp T T Einstein relation dP 0 dx FP equation: m gP(x) D Solution: m g m gx P(x) exp D D But from equilibrium stat mech we know So D = μT m g m gx P(x) exp T T Einstein relation dP 0 dx FP equation: m gP(x) D Solution: m g m gx P(x) exp D D But from equilibrium stat mech we know So D = μT Einstein relation m g m gx P(x) exp T T Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Voltage diff (“membrane potential”) between inside and outside of cell Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Voltage diff (“membrane potential”) between inside and outside of cell Can vary membrane potential experimentally by adding external field Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Voltage diff (“membrane potential”) between inside and outside of cell Can vary membrane potential experimentally by adding external field Question: At a given Vm, what current flows through the channel? Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Voltage diff (“membrane potential”) between inside and outside of cell Can vary membrane potential experimentally by adding external field Question: At a given Vm, what current flows through the channel? x=0 outside x=d inside x Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Voltage diff (“membrane potential”) between inside and outside of cell Can vary membrane potential experimentally by adding external field Question: At a given Vm, what current flows through the channel? x=0 x=d Vout= 0 inside outside x V(x) Vm Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Voltage diff (“membrane potential”) between inside and outside of cell Can vary membrane potential experimentally by adding external field Question: At a given Vm, what current flows through the channel? ρout x=0 x=d ρin x inside Vout= 0 outside V(x) Vm Constant current: Goldman-Hodgkin-Katz model of an (open) ion channel Pumps maintain different inside and outside concentrations of ions Voltage diff (“membrane potential”) between inside and outside of cell Can vary membrane potential experimentally by adding external field Question: At a given Vm, what current flows through the channel? ρout x=0 x=d ? ρin x inside Vout= 0 outside V(x) Vm Reversal potential If there is no current, equilibrium => ρin/ρout=exp(-βV) Reversal potential If there is no current, equilibrium => ρin/ρout=exp(-βV) This defines the reversal potential out Vr T log in at which J = 0. Reversal potential If there is no current, equilibrium => ρin/ρout=exp(-βV) This defines the reversal potential out Vr T log in at which J = 0. ForCa++, ρout>> ρin => Vr >> 0 GHK model (2) Vm< 0: both diffusive current and drift current flow in ρout x=0 x=d ? ρin x inside Vout= 0 outside V(x) Vm GHK model (2) Vm< 0: both diffusive current and drift current flow in Vm= 0: diffusive current flows in, no drift current ρout Vout= 0 outside x=0 x=d ? V(x) ρin x inside GHK model (2) Vm< 0: both diffusive current and drift current flow in Vm= 0: diffusive current flows in, no drift current Vm> 0: diffusive current flows in, drift current flows out ρout x=0 x=d ? V(x) Vout= 0 outside Vm ρin x inside GHK model (2) Vm< 0: both diffusive current and drift current flow in Vm= 0: diffusive current flows in, no drift current Vm> 0: diffusive current flows in, drift current flows out At Vm= Vr they cancel ρout x=0 x=d ? V(x) Vout= 0 outside Vm ρin x inside GHK model (2) Vm< 0: both diffusive current and drift current flow in Vm= 0: diffusive current flows in, no drift current Vm> 0: diffusive current flows in, drift current flows out At Vm= Vr they cancel Jdrift qE(x) q ρout dV qVm (x) (x), dx d x=0 outside d dx x=d ? V(x) Vout= 0 Jdiff D Vm ρin x inside Steady-state FP equation dJ d d qVm D 0 dx dx dx d Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const. dx d Steady-state FP equation Use Einstein relation: dJ d d qVm D 0 dx dx dx d d qVm J D const. dx d d qVm T dx d Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const. dx d d qVm Use Einstein relation: T dx d J d qVm , T dx d Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const . dx d d qVm Use Einstein relation: T dx d J d qVm , T dx d J J (x) (0) Solution: expx T T Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const . dx d d qVm Use Einstein relation: T dx d J d qVm , T dx d J J (x) (0) Solution: expx T T We are given ρ(0) and ρ(d). Use this to solve for J: Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const . dx d d qVm Use Einstein relation: T dx d J d qVm , T dx d J J (x) (0) Solution: expx T T We are given ρ(0) and ρ(d). Use this to solve for J: J 1 expd out expd (d), T Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const . dx d d qVm Use Einstein relation: T dx d J d qVm , T dx d J J (x) (0) Solution: expx T T We are given ρ(0) and ρ(d). Use this to solve for J: J 1 expd out expd (d), T (d) in out expqVr Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const . dx d d qVm Use Einstein relation: T dx d J d qVm , T dx d J J (x) (0) Solution: expx T T We are given ρ(0) and ρ(d). Use this to solve for J: J 1 expd out expd (d), T J T out expd (d) 1 expd (d) in out expqVr Steady-state FP equation dJ d d qVm D 0 dx dx dx d d qVm J D const . dx d d qVm Use Einstein relation: T dx d J d qVm , T dx d J J (x) (0) Solution: expx T T We are given ρ(0) and ρ(d). Use this to solve for J: J 1 expd out expd (d), T (d) in out expqVr T out expd (d) qVm out expqVm expqVr J 1 expd d 1 expqVm GHK current, another way Start from J D d qVm const. dx d GHK current, another way Start from d qVm const. dx d d T dx J D GHK current, another way Start from d qVm const. dx d d T dx d J expx T expx dx J D GHK current, another way Start from Note d qVm const. dx d d T dx d d J expx T expx T expx dx dx J D GHK current, another way Start from Note d qVm const. dx d d T dx d d J expx T expx T expx dx dx J D Integrate from 0 to d: GHK current, another way Start from Note d qVm const. dx d d T dx d d J expx T expx T expx dx dx J D Integrate from 0 to d: J expd 1 T in expd out GHK current, another way Start from Note d qVm const. dx d d T dx d d J expx T expx T expx dx dx J D Integrate from 0 to d: J expd 1 T in expd out J T in expd out expd 1 GHK current, another way Start from Note d qVm const. dx d d T dx d d J expx T expx T expx dx dx J D Integrate from 0 to d: J expd 1 T in expd out J T qVm in expqVm out in expd out expd 1 dexpqVm 1 GHK current, another way Start from Note d qVm const. dx d d T dx d d J expx T expx T expx dx dx J D Integrate from 0 to d: J expd 1 T in expd out J T qVm in expqVm out in expd out expd 1 d expqVm 1 qVm out expqVm expqVr L d1 expqVm (as before) GHK current, another way Start from Note d qVm const. dx d d T dx d d J expx T expx T expx dx dx J D Integrate from 0 to d: J expd 1 T in expd out J T qVm in expqVm out in expd out expd 1 d expqVm 1 qVm out expqVm expqVr L d1 expqVm Note: J = 0 at Vm= Vr (as before) GHK current is nonlinear (using z, Vr for Ca++) J V GHK current is nonlinear (using z, Vr for Ca++) J V Vm : qJ q 2 out Vm d GHK current is nonlinear (using z, Vr for Ca++) J V Vm : qJ q 2 out Vm E, E Vm /d, d GHK current is nonlinear (using z, Vr for Ca++) J V Vm : qJ q 2 out Vm E, E Vm /d, q 2 out d GHK current is nonlinear (using z, Vr for Ca++) J V Vm E, E Vm /d, q2 out d V Vm : qJ q 2 out exp(qVr ) m E, d Vm : qJ q 2 out GHK current is nonlinear (using z, Vr for Ca++) J V Vm E, E Vm /d, q 2 out d V Vm : qJ q 2 out exp(qVr ) m E, q2 out exp(qVr ) q2 in d Vm : qJ q 2 out GHK current is nonlinear (using z, Vr for Ca++) J V Vm E, E Vm /d, q 2 out d V Vm : qJ q 2 out exp(qVr ) m E, q2 out exp(qVr ) q2 in d q 3Vr out in Vm Vr: qJ (Vr Vm ) d out in Vm : qJ q 2 out Kramers escape Rate of escape from a potential well due to thermal fluctuations P2(x) P1(x) V1(x) V2(x) www.nbi.dk/hertz/noisecourse/demos/Pseq.mat www.nbi.dk/hertz/noisecourse/demos/runseq.m Kramers escape (2) V(x) a b c Kramers escape (2) V(x) J a b c Kramers escape (2) V(x) J a b c Basic assumption: (V(b) – V(a))/T >> 1 Fokker-Planck equation Conservation (continuity): P J u(x)P D(x)P t x x x Fokker-Planck equation Conservation (continuity): P J u(x)P D(x)P t x x x V P P D x x x Fokker-Planck equation Conservation (continuity): P J u(x)P D(x)P t x x x V P P D x x x (V ) P D P Use Einstein relation: x x x Fokker-Planck equation Conservation (continuity): P J u(x)P D(x)P t x x x V P P D x x x (V ) P D P Use Einstein relation: x x x Current: J DexpV (x) expV (x)P x Fokker-Planck equation Conservation (continuity): P J u(x)P D(x)P t x x x V P P D x x x (V ) P D P Use Einstein relation: x x x Current: J DexpV (x) expV (x)P x If equilibrium, J = 0, Fokker-Planck equation Conservation (continuity): P J u(x)P D(x)P t x x x V P P D x x x (V ) P D P Use Einstein relation: x x x Current: J DexpV (x) expV (x)P x If equilibrium, J = 0, P(x) expV (x) Fokker-Planck equation Conservation (continuity): P J u(x)P D(x)P t x x x V P P D x x x (V ) P D P Use Einstein relation: x x x Current: J DexpV (x) expV (x)P x J = 0, P(x) expV (x) Here: almost equilibrium, so use this P(x) If equilibrium, Calculating the current J expV (x) expV (x)P(x) D x (J is constant) Calculating the current J expV (x) expV (x)P(x) D x integrate: J D expV (x)dx expV (x)P(x)a c a c (J is constant) Calculating the current integrate: J D c a J expV (x) expV (x)P(x) D x (J is constant) expV (x)dx expV (x)P(x)a c expV (a)P(a) (P(c) very small) Calculating the current integrate: J D J expV (x) expV (x)P(x) D x expV (x)dx expV (x)P(x)a c a c expV (a)P(a) J (J is constant) DexpV (a)P(a) c a expV (x)dx (P(c) very small) Calculating the current integrate: J D J expV (x) expV (x)P(x) D x expV (x)dx expV (x)P(x)a c a (J is constant) c expV (a)P(a) J (P(c) very small) DexpV (a)P(a) c a expV (x)dx If p is probability to be in the well, J = pr, where r = escape rate Calculating the current integrate: J D J expV (x) expV (x)P(x) D x expV (x)dx expV (x)P(x)a c a (J is constant) c expV (a)P(a) J (P(c) very small) DexpV (a)P(a) c a expV (x)dx If p is probability to be in the well, J = pr, where r = escape rate p a a P(x)dx Calculating the current integrate: J D J expV (x) expV (x)P(x) D x expV (x)dx expV (x)P(x)a c a (J is constant) c expV (a)P(a) J (P(c) very small) DexpV (a)P(a) c a expV (x)dx If p is probability to be in the well, J = pr, where r = escape rate p a a P(x)dx P(a) a exp V (a) V (x)dx a Calculating the current integrate: J D J expV (x) expV (x)P(x) D x expV (x)dx expV (x)P(x)a c a (J is constant) c expV (a)P(a) J (P(c) very small) DexpV (a)P(a) c a expV (x)dx If p is probability to be in the well, J = pr, where r = escape rate p a a P(x)dx P(a) a a exp V (a) V (x)dx 2 2 2 P(a) exp 12 V (a)y dy P(a) V (a) 1 calculating escape rate In integral exp V (x)dx integrand is peaked near x = b c a calculating escape rate In integral a exp V (x)dx integrand is peaked near x = b expV (x)dx expV (b) exp 12 V (b) x b dx c a c 2 calculating escape rate In integral exp V (x)dx integrand is peaked near x = b c a a expV (x)dx expV (b) exp 12 V (b) x b dx c 2 2 2 expV (b) V (b) 1 calculating escape rate In integral exp V (x)dx integrand is peaked near x = b c a a expV (x)dx expV (b) exp 12 V (b) x b dx c r 2 2 2 expV (b) V (b) 1 J DexpV (a)P(a) p p cexpV (x)dx a calculating escape rate In integral exp V (x)dx integrand is peaked near x = b c a a expV (x)dx expV (b) exp 12 V (b) x b dx c r 2 2 2 expV (b) V (b) 1 J DexpV (a)P(a) p p cexpV (x)dx a DexpV (a)P(a) 2 2 2 P(a) expV (b) V (a) V (b) 1 2 1 calculating escape rate In integral exp V (x)dx integrand is peaked near x = b c a a expV (x)dx expV (b) exp 12 V (b) x b dx c r 2 2 2 expV (b) V (b) 1 J DexpV (a)P(a) p p cexpV (x)dx a DexpV (a)P(a) 2 2 2 P(a) expV (b) V (a) V (b) 1 D V (a) V (b) 2 exp V (b) V (a) 2 1 2 1 calculating escape rate In integral exp V (x)dx integrand is peaked near x = b c a a expV (x)dx expV (b) exp 12 V (b) x b dx c r 2 2 2 expV (b) V (b) 1 J DexpV (a)P(a) p p cexpV (x)dx a DexpV (a)P(a) 2 2 2 P(a) expV (b) V (a) V (b) 1 1 D 2 V (a) V (b) exp V (b) V (a) V (a) V (b) 2 expE b 2 2 1 2 1 calculating escape rate In integral exp V (x)dx integrand is peaked near x = b c a a expV (x)dx expV (b) exp 12 V (b) x b dx c r 2 2 2 expV (b) V (b) 1 J DexpV (a)P(a) p p cexpV (x)dx a DexpV (a)P(a) 2 2 2 P(a) expV (b) V (a) V (b) 1 1 D 2 V (a) V (b) exp V (b) V (a) V (a) V (b) 2 expE b ________ 2 2 1 2 1 More about drift current Notice: If u(x) is not constant, the probability cloud can shrink or spread even if there is no diffusion More about drift current Notice: If u(x) is not constant, the probability cloud can shrink or spread even if there is no diffusion (like density of cars on a road where the speed limit varies) More about drift current Notice: If u(x) is not constant, the probability cloud can shrink or spread even if there is no diffusion (like density of cars on a road where the speed limit varies) Demo: initial P: Gaussian centered at x = 2 u(x) = .00015x http://www.nbi.dk/~hertz/noisecourse/driftmovie.m Derivation from master equation P(x,t) t dx w(x x )P( x ,t) w( x x)P(x,t) w(x x ) r( x ;x x ) : Derivation from master equation P(x,t) t dx w(x x )P( x ,t) w( x x)P(x,t) w(x x ) r( x ;x x ) : (1st argument of r: starting point; 2nd argument: step size) Derivation from master equation P(x,t) t dxw(x x )P( x ,t) w( x x)P(x,t) w(x x ) r( x ;x x ) : (1st argument of r: starting point; 2nd argument: step size) dxr( x ;x x)P( x ,t) r(x; x x)P(x,t) x x s : Derivation from master equation P(x,t) t dx w(x x )P( x ,t) w( x x)P(x,t) w(x x ) r( x ;x x ) : (1st argument of r: starting point; 2nd argument: step size) dx r( x ;x x )P( x ,t) r(x; x x)P(x,t) dsr(x s;s)P(x s,t) r(x;s)P(x,t) x x s : Derivation from master equation P(x,t) t dx w(x x )P( x ,t) w( x x)P(x,t) w(x x ) r( x ;x x ) : (1st argument of r: starting point; 2nd argument: step size) dx r( x ;x x )P( x ,t) r(x; x x)P(x,t) dsr(x s;s)P(x s,t) r(x;s)P(x,t) x x s : Small steps assumption: r(x;s) falls rapidly to zero with increasing |s| on the scale on which it varies with x or the scale on which P varies with x. Derivation from master equation P(x,t) t dx w(x x )P( x ,t) w( x x)P(x,t) w(x x ) r( x ;x x ) : (1st argument of r: starting point; 2nd argument: step size) dx r( x ;x x )P( x ,t) r(x; x x)P(x,t) dsr(x s;s)P(x s,t) r(x;s)P(x,t) x x s : Small steps assumption: r(x;s) falls rapidly to zero with increasing |s| on the scale on which it varies with x or the scale on which P varies with x. x s Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) 2 x x Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) 2 x x x 2 sr(x,s)ds P(x,t) x 2 1 2 s2 r(x,s)ds P(x,t) L Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) 2 x x 2 sr(x,s)ds P(x,t) 2 12 s2 r(x,s)ds P(x,t) L x x 1 2 r1(x)P(x,t) r2 (x)P(x,t) L x 2 x 2 Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) 2 x x 2 sr(x,s)ds P(x,t) 2 12 s2 r(x,s)ds P(x,t) L x x 1 2 Kramers-Moyal expansion r1(x)P(x,t) r (x)P(x,t) L 2 2 x 2 x Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) 2 x x 2 sr(x,s)ds P(x,t) 2 12 s2 r(x,s)ds P(x,t) L x x 1 2 Kramers-Moyal expansion r1(x)P(x,t) r (x)P(x,t) L 2 2 x 2 x Fokker-Planck eqn if drop terms of order >2 Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) x x 2 2 sr(x,s)ds P(x,t) 2 12 s2 r(x,s)ds P(x,t) L x x 1 2 Kramers-Moyal expansion r1(x)P(x,t) r (x)P(x,t) L 2 2 x 2 x Fokker-Planck eqn if drop terms of order >2 rn (x) s r(x,s)ds n Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) x x 2 2 sr(x,s)ds P(x,t) 2 12 s2 r(x,s)ds P(x,t) L x x 1 2 Kramers-Moyal expansion r1(x)P(x,t) r (x)P(x,t) L 2 2 x 2 x Fokker-Planck eqn if drop terms of order >2 rn (x) s r(x,s)ds n rn(x)Δt = nth moment of distribution of step size in time Δt Derivation from master equation (2) expand: P(x,t) t dsr(x s;s)P(x s,t) r(x;s)P(x,t) 2 1 2 dsr(x;s)P(x,t) s r(x,s)P(x,t) 2 s r(x,s)P(x,t) L r(x;s)P(x,t) x x 2 2 sr(x,s)ds P(x,t) 2 12 s2 r(x,s)ds P(x,t) L x x 1 2 Kramers-Moyal expansion r1(x)P(x,t) r (x)P(x,t) L 2 2 x 2 x Fokker-Planck eqn if drop terms of order >2 rn (x) s r(x,s)ds n rn(x)Δt = nth moment of distribution of step size in time Δt r1 (x) u(x), r2 (x) 2D(x)