Values larger than 1 are not compatible with ITERATE-ALPHA, this setting is overruled by the SWITCH option.
This option can only be used with ANALYTIC-INTEGRATION integration.
[Default: n=2, equivalent to SECOND-ORDER-TERMS.]
SWITCH overrules this selection.
HIGH-PRECISION is synonymous to SECOND-ORDER-TERMS.
This option can only be used with ANALYTIC-INTEGRATION integration, available only in Garfield version \ and earlier.
[This is the default order, but is overruled by SWITCH.]
LOW-PRECISION is synonymous to FIRST-ORDER-TERMS.
This option can only be used with ANALYTIC-INTEGRATION integration, available only in Garfield version\ 7 and earlier.
[The default is SECOND-ORDER-TERMS.]
This option can only be used with ANALYTIC-INTEGRATION integration, available only in Garfield version\ 7 and earlier.
[This is not default.]
If \α/pressure is smaller than the threshold, the quantities are computed with SECOND-ORDER-TERMS, NOITERATE-ALPHA
Otherwise, they are computed with FIRST-ORDER-TERMS, ITERATE-ALPHA.
This guarantees that the drift velocity, diffusion and Lorentz angle are accurate at low field values, which is where they matter most, whereas the Townsend coefficient is accurate at higher field values, at the price of a somewhat reduced accuracy for the other quantities.
This option can only be used with ANALYTIC-INTEGRATION integration, available only in Garfield version\ 7 and earlier.
[This option is default, \α/pressure is set to 50/pressure.]
These formulae are only valid when the approximation that the longitudinal and transverse diffusion are equal is true. This is of course never true, but one can get a correction to the longitudinal diffusion from the ratio of the longitudinal to transverse diffusion without the magnetic field in the given gas at the E-field of interest. [from Steve Biagi]
These diffusion coefficients are obtained when you specify F0-TRANSVERSE-DIFFUSION, H1-TRANSVERSE-DIFFUSION, F0-LONGITUDINAL-DIFFUSION and H1-LONGITUDINAL-DIFFUSION. The correction to the longitudinal diffusion is applied, using the G0 estimate of the longitudinal diffusion.
F0-TRANSVERSE-DIFFUSION is default.
These options can only be used with ANALYTIC-INTEGRATION integration, available only in Garfield version\ 7 and earlier.
Formatted on 21/01/18 at 16:55.