Hydropascoite, Ca (sub 3) (V (sub 10) O (sub 28) ).24H (sub 2) O, a new decavanadate mineral from the Packrat Mine, Mesa County, Colorado

Hydropascoite, Ca (sub 3) (V (sub 10) O (sub 28) ).24H (sub 2) O, is a new mineral species (IMA2016-032) discovered in the Packrat mine, near Gateway, Mesa County, Colorado. It occurs as blades up to 2 mm in length on asphaltum associated with montroseite- and corvusite-bearing sandstone. Hydropascoite is dark yellow green, with a pistachio green streak, vitreous luster, Mohs hardness of ca 11/2, brittle tenacity, irregular fracture, and one perfect cleavage on {001}. Density (meas.) is 2.38(2) g/cm (super 3) . Hydropascoite is biaxial (-), with alpha 1.730(5), beta 1.780(5), gamma 1.790(5) (white light); 2V (meas.) = 54.1(6) degrees , and extreme dispersion. The optical orientation is X^a nearly equal 10 degrees , Z^c* nearly equal 20 degrees . Hydropascoite is pleochroic, with X = bluish green, Y = orange, Z = yellowish green; X > Z > Y Electron probe microanalysis gave the empirical formula (Ca (sub 2.69) Na (sub 0.30) ) (sub Sigma 2.99) (H (sub 0.31) V (super 5+) (sub 10) O (sub 28) ).24H (sub 2) O, based on O = 52. Hydropascoite is triclinic, P1, a 10.08700(19), b 11.0708(2), c 21.8112(15) A, alpha 94.112(7) degrees , beta 96.053(7) degrees , gamma 116.398(8) degrees , V 2150.2(2) A (super 3) , and Z = 2. The strongest four lines in the diffraction pattern are [d in A(I)(hkl)]: 8.92(100)(110), 10.70(31)(002), 9.77(28)(010), and 7.4539(22)(102). The atomic arrangement of hydropascoite was solved and refined to R (sub 1) = 0.0488 for 8187 independent reflections with F > 4sigma F. The structural unit in hydropascoite is the [V (sub 10) O (sub 28) ] (super 6-) decavanadate group; charge balance in the structure is maintained by the [Ca (sub 3) .24H (sub 2) O] (super 6+) interstitial complex. The three Ca polyhedra in the interstitial complex are not polymerized. Linkage between the structural unit and the components of the interstitial complex is principally by hydrogen bonding. In addition to the extensive hydrogen bonding, three oxygen atoms of the structural unit bond directly to calcium atoms of the interstitial complex. The mineral is named to recognize its chemical and structural similarity to pascoite, Ca (sub 3) (V (sub 10) O (sub 28) ).17H (sub 2) O, and its higher H (sub 2) O content.