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Hallimondite |
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Locock A J, Burns P C, Flynn T M |
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American Mineralogist 90 (2005) 240-246 |
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The role of water in the structures of synthetic hallimondite, Pb2[(UO2)(AsO4)2](H2O)n |
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and synthetic parsonsite, Pb2[(UO2)(PO4)2](H2O)n, 0 < n < 0.5 |
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7.1153 10.4780 6.8571 101.178 95.711 86.651 P-1 |
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atom x y z occ Uiso U(1,1) U(2,2) U(3,3) U(1,2) U(1,3) U(2,3) |
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U1 .6186 .8400 .0988 .010 .016 .007 .008 .001 .003 .001 |
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Pb1 .3090 .5416 .2785 .016 .018 .019 .012 -.001 .003 .002 |
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Pb2 .0451 .7776 .7170 .018 .021 .012 .022 .001 .006 .000 |
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As1 .5365 .8167 .6206 .009 .013 .007 .007 .000 .002 .000 |
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As2 .8238 .5494 .2763 .010 .011 .009 .009 .001 .001 .002 |
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O1 .0022 .6340 .4155 .018 .012 .022 .018 -.005 -.002 .000 |
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O2 .3486 .4738 .5851 .014 .013 .019 .013 .000 .005 .007 |
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O3 .3859 .7840 .0731 .021 .019 .025 .019 -.004 .002 .005 |
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O4 .6811 .7288 .7623 .015 .022 .015 .007 .003 .000 .002 |
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O5 .7149 .6298 .1057 .020 .034 .011 .013 .006 -.001 .004 |
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O6 .3323 .7477 .5346 .017 .014 .017 .017 -.004 .002 -.003 |
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O7 .5018 .0540 .1927 .019 .040 .009 .008 .008 .002 .001 |
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O8 .8504 .8978 .1144 .021 .022 .022 .021 -.009 .005 .002 |
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O9 .6524 .8562 .4429 .019 .022 .023 .013 -.002 .004 .005 |
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O10 .9230 .4099 .1582 .021 .029 .014 .019 .009 .009 .002 |
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Wat11 .0500 .9720 .4740 .29 .073 |
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