Agardite-(Y), Cu(2+) 6Y(AsO4)3(OH)6·3H2O
Shaunna M Morrison1, Kenneth J Domanik2, Marcus J Origlieri1
1Department of Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, Arizona 85721-0077, USA.
Acta Crystallographica. Section E, Structure Reports Online
|January 16, 2014
Summary
This study details the crystal structure of agardite-(Y), a mineral in the mixite group. Researchers used X-ray diffraction to reveal its unique chain-like structure of copper, yttrium, and arsenate polyhedra.
Area of Science:
- Mineralogy
- Crystallography
- Geochemistry
Background:
- Agardite-(Y) is a mineral belonging to the mixite group, with the general formula Cu(2+) 6 A(TO4)3(OH)6·3H2O.
- The A-site typically contains rare earth elements, Al, Ca, Pb, or Bi, while the T-site contains P or As.
Purpose of the Study:
- To present the first structure determination of agardite-(Y).
- To analyze the structural characteristics of agardite-(Y) using single-crystal X-ray diffraction.
Main Methods:
- Single-crystal X-ray diffraction was performed on a natural sample of agardite-(Y).
- The sample was sourced from the Jote West mine, Pampa Larga Mining District, Copiapo, Chile.
Main Results:
- The refined formula for agardite-(Y) is Cu(2+) 5.70(Y0.69Ca0.31)[(As0.83P0.17)O4]3(OH)6·3H2O.
- The structure features infinite chains of edge-sharing CuO5 square pyramids along the c axis.
- These chains are linked by edge-sharing YO9 polyhedra and corner-sharing AsO4 tetrahedra in the ab plane.
- Tubular channels containing lattice water molecules are present, with walls formed by CuO5 and AsO4 polyhedra.
Conclusions:
- This study provides the first detailed structural analysis of agardite-(Y).
- The findings elucidate the complex arrangement of polyhedra and channels within the agardite-(Y) structure.
- The research contributes to the understanding of the mixite mineral group's crystallography.
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