Epidotes

The solid solution is treated as a ternary solution of clinozoisite, Fe-epidote and an ordered epidote solid solution, using the approach outlined in Holland & Powell (1996 Am Min). Here, Al and Fe3 are assumed to mix on only the M1 and M3 sites, with a strong tendency for Fe3 to order onto the M3 site. The model used is an extension of that used by Bird & Helgeson (1980) to incorporate non-ideal mixing.

M1

M3

cz

Al

Al

ep

Al

Fe

fep

Fe

Fe

The ideal activities of the three end-members are written

where pcz is the proportion of the cz end-member etc. The activity coefficients arefound from the simple regular solution expressions for the ternary solid solution among cz, fep and ep end-members. The degree of order, given by Q = XFeM3 - XFeM1 = pep is found by substituting the activities into the equilibrium constant for the internal equilibrium cz + fep = 2ep. The enthalpy of this reaction is -26.1 kJ, and the values for Wcz-fep, Wcz-ep and Wfep-ep are 15.4, 0.0 and 3.0 kJ/mol respectively, derived from the known values of the order parameter Q from Dollase (1973) and the experimental reversals of Liou (1973), Holdaway (1972), Jenkins et al. (1983) as well as consideration of natural zoisite-clinozoisite partitioning data. While the derived enthalpies of ep and fep depend on this mixing model, that of cz does not.

The calculated activities at 400 and 600°C are given below.

Coded up for THERMOCALC:

% ==================   Epidotes   ========================
epi 3
x(ep) 0.5
N(ep) 0.015 range 0 0.5 % where N = Q/2

%-------------------------------------------------------------------

p(cz) 1 1 1 2 -1 x -1 N
p(ep) 1 1 0 2 1 x 1 N
p(fep) 1 1 0 1 2 N

% --------------------------------------------------
sf

W(czep) 0 0 0
W(czfep) 15.4 0 0
W(almpy) 3 0 0

% --------------------------------------------------
4 % 4 "site fractions"

xFeM1 1 1 0 2 1 x 1 N

xAlM1 1 1 1 2 -1 x -1 N

xFeM3 1 1 0 2 1 x -1 N

xAlM3 1 1 1 2 -1 x 1 N

% --------------------------------------------------
% ideal mixing activities

cz 1 2 xAlM1 1 xAlM3 1 % may only involve "site fractions"

ep 1 2 xFeM1 1 xAlM3 1

fep 1 2 xFeM1 1 xFeM3 1


%__________________________________________________________________
 

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