@johnsoevans Thank-you for your response.
Yes, there is a chance that the intensity mismatch is due to texture and/or preferred orientation effects because the sample was gently packed into a quartz capillary tube. I have dabbled with the Spherical Harmonics command in conjunction with individual phase peak_types:
`str
phase_name Cu9Ni1
space_group "Fm-3m"
Cubic( = lp_Cu9Ni1; )
scale Cu9Ni1_scale 0.00001
r_bragg 0
site Cu9Ni1_site x 0 y 0 z 0 occ Cu 0.9 beq = Cu_beq; occ Ni 0.1 beq = Ni_beq;
weight_percent wt_Cu9Ni1 5
TCHZ_Peak_Type(pku1, 0.00039,pkv1, -0.00221,pkw1, -0.00146,!pkz1, 0.0000,pkx1, 0.00957, pky1, 0.0001)
str
phase_name Cu8Ni2
space_group "Fm-3m"
Cubic( = lp_Cu8Ni2; )
scale Cu8Ni2_scale 0.00001
r_bragg 0
site Cu8Ni2_site x 0 y 0 z 0 occ Cu 0.8 beq = Cu_beq; occ Ni 0.2 beq = Ni_beq;
weight_percent wt_Cu8Ni2 5
TCHZ_Peak_Type(pku2, 0.00039,pkv2, -0.00221,pkw2, -0.00146,!pkz2, 0.0000,pkx2, 0.00957, pky2, 0.0001)
...
for strs {
PO_Spherical_Harmonics(sh,8)
scale_pks = Max(sh,0);
}
`
where lp_Cu9Ni1, lp_Cu8Ni2, Cu_beq and Ni_beq are all fixed values.
In combination, these commands fix the intensity mismatches for the (111) and (200) peaks (see here) but don't rectify other smaller mismatches highlighted here .
This leaves me with a few questions. Is there something I am fundamentally missing in the analysis? If not, is it worth trying out some of the other preferred orientation commands such as March-Dollase? Or is this about as good of a fit as I can expect using several phase_groups as opposed to fitting individual peaks, etc.?!