Artioli G, Kvick A
European Journal of Mineralogy 2 (1990) 749-759
Synchrotron X-ray Rietveld study of perlialite, the natural counterpart of synthetic zeolite-L
Sample: data collected with synchrotron radiation
18.5432 18.5432 7.5310 90 90 120 P6/mmm
atom x y z occ Uiso
KA 1/3 2/3 0 .39 .07
KB 1/3 2/3 .5 .38 .015
KB1 1/3 2/3 .427 .31 .015
KD .297 0 0 .52 .046
TlD1 .315 0 0 .48 .046
KE .5 0 .5 .70 .041
TlE .5 0 .5 .30 .044
Si1 .0924 .3546 .5 2/3 .032
Al1 .0924 .3546 .5 1/3 .032
Si2 .1672 .4975 .215 2/3 .062
Al2 .1672 .4975 .215 1/3 .062
O1 0 .272 .5 .01
O2 .158 .316 .5 .06
O3 .260 .520 .288 .07
O4 .1038 .4125 .326 .023
O5 .4092 .8184 .213 .06
O6 .156 .483 0 .015
WatF .11 0 0 .40 .09
WatH .134 0 .37 .91 .09
WatI .28 .14 0 .25 .03
WatJ .28 .14 .26 .19 .10
WatK 0 0 .172 .70 .10
WatN .560 .280 0 .66 .10
Sample: data collected with conventional diffractometer radiation
KA 1/3 2/3 0 .13 .11
KB 1/3 2/3 .5 .60 .023
KB1 1/3 2/3 .443 .20 .023
KD .299 0 0 .521 .0403
TlD1 .3150 0 0 .479 .0403
KE .5 0 .5 .687 .044
TlE .5 0 .5 .313 .044
Si1 .0918 .3522 .5 2/3 .031
Al1 .0918 .3522 .5 1/3 .031
Si2 .1703 .4976 .2172 2/3 .056
Al2 .1703 .4976 .2172 1/3 .056
O1 0 .276 .5 .03
O2 .1622 .3244 .5 .02
O3 .2650 .530 .283 .05
O4 .1075 .4149 .331 .027
O5 .4181 .8362 .263 .06
O6 .160 .489 0 .045
WatF .12 0 0 .10 .10
WatH .1351 0 .364 .83 .11
WatI .288 .144 0 .53 .09
WatJ .274 .137 .24 .42 .10
WatK 0 0 .19 .37 .10
WatN .553 .277 0 .31 .10
Multiple datasets can be concatenated into a single downloadable file by selecting the datasets and then hitting the "Download Selected Data" button.
Total number of retrieved datasets: 2 View in amc, download in amc
Return to AMCSD Home Page
