Lumsdenite, NaCa3Mg2(As3+V4+2V5+10As5+6O51)·45H2O, a new polyoxometalate mineral from the Packrat mine, Mesa County, Colorado, USA

2020 ◽  
Vol 58 (1) ◽  
pp. 137-151 ◽  
Author(s):  
Anthony R. Kampf ◽  
John M. Hughes ◽  
Barbara P. Nash ◽  
Joe Marty ◽  
Timothy P. Rose
Keyword(s):  
Powder Diffraction ◽  
White Light ◽  
Structural Unit ◽  
Close Association ◽  
The Novel ◽  
Secondary Minerals ◽  
Atomic Arrangement ◽  
Greenish Yellow ◽  
Greenish Blue ◽  
Dark Green

ABSTRACT Lumsdenite (IMA 2018–092), ideally NaCa3Mg2(As3+V4+2V5+10As5+6O51)·45H2O, is a rare new polyoxometalate mineral from the Packrat mine, Gateway district, Mesa County, Colorado, USA. Crystals of lumsdenite occur as blades up to 0.2 mm in length, commonly growing in sprays. The crystals are dark green blue, with a green-blue streak. The mineral occurs on asphaltum, associated with montroseite- and corvusite-bearing sandstone. Other secondary minerals found in close association with lumsdenite are gypsum, huemulite, rösslerite, and at least two other potentially new minerals. Lumsdenite is optically biaxial (–), with α 1.617(2), β 1.651(5), and γ 1.675(5) in white light. The pleochroism scheme for lumsdenite is X = greenish yellow, Y = dark greenish blue, Z = greenish blue; X << Z < Y. The mineral is triclinic, , with a 10.3490(5), b 17.6263(9), c 23.2556(16) Å, α 82.208(6), β 88.351(6), γ 81.702(6)°, V 4158.8(4) Å3, and Z = 2. The strongest four powder diffraction lines for lumsdenite are [dobs Å(I)(hkl)]: , 14.86(80)(011), 17.30(44)(010), and 10.22(32)(100). The atomic arrangement of lumsdenite contains the novel polyoxometalate heteropolyanion [As3+V4+,5+12As5+6O51] structural unit in lumsdenite, [As3+V4+25+10As5+6O51]11−, which has previously been found in four other minerals from the Packrat mine. The charge of the structural unit is balanced by the charge of the [NaCa3Mg2(H2O)31·14H2O]11+ interstitial complex. The name lumsdenite is for the location of the mine at the head of Lumsden Canyon.

scholarly journals Dipcadi krishnadevarayae (Asparagaceae), a new plant species from Andhra Pradesh, India

2016 ◽  
Vol 8 (13) ◽  
pp. 9562 ◽  
Author(s):  
Boyina Ravi Prasad Rao ◽  
Kothareddy Prasad ◽  
Dasari Veeranjaneyulu ◽  
Mudavath Chennakesavulu Naik ◽  
Sugali Salamma ◽  
...  
Keyword(s):  
New Species ◽  
Plant Species ◽  
Andhra Pradesh ◽  
Novel Species ◽  
The Novel ◽  
University Campus ◽  
Green Band ◽  
Greenish Yellow ◽  
Dark Green ◽  
A New Species

Dipcadi krishnadevarayae B.R.P.Rao (Asparagaceae), a new species from the Sri Krishnadevaraya University campus, Anantapuramu of Andhra Pradesh, India, is described and illustrated.  The novel species is distinct from all other species of Dipcadi in having distinctly 6-lobed stigma and shows close affinity to D. serotinum (L.) Medik. and D. montanum (Dalzell) Baker.  It differs from both allies in having a combination of up to 50cm long linear leaves, 85cm long 16–24 flowered scapes, greenish-yellow flowers, dark green band outside the outer tepals, distinctly 6-lobed stigma and up to 10 seeds in each locule.  

scholarly journals The Preferences of Different Cultivars of Lettuce Seedlings (Lactuca sativa L.) for the Spectral Composition of Light

Agronomy ◽  
2021 ◽  
Vol 11 (6) ◽  
pp. 1211
Author(s):  
Barbara Frąszczak ◽  
Monika Kula-Maximenko
Keyword(s):  
Chlorophyll Content ◽  
Blue Light ◽  
White Light ◽  
Leaf Shape ◽  
Red Light ◽  
Spectral Composition ◽  
Fresh Weight ◽  
Light Spectrum ◽  
Dark Green ◽  
Relative Chlorophyll Content

The spectrum of light significantly influences the growth of plants cultivated in closed systems. Five lettuce cultivars with different leaf colours were grown under white light (W, 170 μmol m−2 s−1) and under white light with the addition of red (W + R) or blue light (W + B) (230 μmol m−2 s−1). The plants were grown until they reached the seedling phase (30 days). Each cultivar reacted differently to the light spectrum applied. The red-leaved cultivar exhibited the strongest plasticity in response to the spectrum. The blue light stimulated the growth of the leaf surface in all the plants. The red light negatively influenced the length of leaves in the cultivars, but it positively affected their number in red and dark-green lettuce. It also increased the relative chlorophyll content and fresh weight gain in the cultivars containing anthocyanins. When the cultivars were grown under white light, they had longer leaves and higher value of the leaf shape index. The light-green cultivars had a greater fresh weight. Both the addition of blue and red light significantly increased the relative chlorophyll content in the dark-green cultivar. The spectrum enhanced with blue light had positive influence on most of the parameters under analysis in butter lettuce cultivars. These cultivars were also characterised by the highest absorbance of blue light.

The Structure of Amorphous Platinum Disulfide as Studied by Anomalous X-ray Scattering

1994 ◽  
Vol 49 (11) ◽  
pp. 1031-1036 ◽  
Author(s):  
Masatoshi Saito ◽  
Makoto Wakeshima ◽  
Nobuaki Sato ◽  
Takeo Fujino ◽  
Yoshio Waseda ◽  
...  
Keyword(s):  
Variational Method ◽  
Least Squares ◽  
Absorption Edge ◽  
Structural Unit ◽  
Precipitation Process ◽  
Interference Function ◽  
X Ray ◽  
Atomic Arrangement ◽  
X Ray Scattering ◽  
Ray Scattering

Abstract Anomalous X-ray scattering (AXS) has been applied to study the structure of amorphous plati­ num disulfide, Pt1-xS2, prepared by the precipitation process. The local atomic arrangement in amorphous Pt1-xS2 was determined by the least-squares variational method so as to reproduce the experimental differential interference function at the Pt Lm absorption edge by the AXS method as well as the ordinary interference function by Mo K α. The structural unit in amorphous Pt1-xS2 is found to be a PtS6 octahedron, similar to that in crystalline PtS2. These octahedra share both their corners and edges, while only edge-sharing linkages occur in crystalline PtS2

Imayoshiite, Ca3Al(CO3)[B(OH)4](OH)6·12H2O, a new mineral of the ettringite group from Ise City, Mie Prefecture, Japan

2015 ◽  
Vol 79 (2) ◽  
pp. 413-423 ◽  
Author(s):  
D. Nishio-Hamane ◽  
M. Ohnishi ◽  
K. Momma ◽  
N. Shimobayashi ◽  
R. Miyawaki ◽  
...  
Keyword(s):  
Single Crystal ◽  
Powder Diffraction ◽  
White Light ◽  
New Mineral ◽  
Structural Refinement ◽  
Single Crystal Diffraction ◽  
Ettringite Group ◽  
Mohs Hardness ◽  
White Streak

AbstractImayoshiite, Ca3Al(CO3)[B(OH)4](OH)6·12H2O, occurs in cavities in the altered gabbro xenolith in the sepentinized dunite exposed at Suisho-dani, Ise City, Mie Prefecture, Japan. Imayoshiite is colourless and transparent with a vitreous lustre and its aggregates are white with a silky lustre. Imayoshiite has a white streak. Its Mohs hardness is 2–3. It is brittle, the cleavage is distinct on {100} and the fracture is uneven. The mineral is uniaxial (–) with the indices of refraction ω = 1.497(2) and ε = 1.470(2) in white light. Imayoshiite is hexagonal, P63, a = 11.0264(11), c = 10.6052(16) Å by powder diffraction and a = 11.04592(2), c = 10.61502(19) Å by single-crystal diffraction. The structural refinement converged to R1 = 2.35%. Imayoshiite is the first member of the ettringite group with both CO3 and B(OH)4 anions.

Lucius or a New Io

Mnemosyne ◽  
2017 ◽  
Vol 70 (1) ◽  
pp. 94-114
Author(s):  
Olga L. Levinskaya
Keyword(s):  
Close Association ◽  
The Novel ◽  
Important Link ◽  
Solid Foundation ◽  
Prometheus Bound ◽  
The One

InMetamorphosesApuleius used a highly exquisite technique of literary casting. This technique implies exploitation of different literary models or molds, both Greek and Roman, which help to hold the novel together on various levels. The story of Io the cow in its dramatic, tragic version (Prometheus BoundandSuppliant Women)has been chosen as one of the basic molds. Io’s story was exploited by Apuleius for shapingboththe ‘inset’ plot about the adventures of Psyche and the main, principal plot—the one about the adventures of Lucius. More than that: the close association between Io and Isis in the Roman tradition provides an important link between the first ten books and the final one. We may consider Io’s story not only as the plot-forming matrix that links together ten books of the novel with its 11th, concluding book, but also as the solid foundation of the unity of the entire novel.

Clarithromycin form I determined by synchrotron X-ray powder diffraction

2012 ◽  
Vol 68 (2) ◽  
pp. o41-o44 ◽  
Author(s):  
Shuji Noguchi ◽  
Keiko Miura ◽  
Sadahiro Fujiki ◽  
Yasunori Iwao ◽  
Shigeru Itai
Keyword(s):  
Powder Diffraction ◽  
Crystal Packing ◽  
Diffraction Method ◽  
Molecular Replacement ◽  
The Novel ◽  
Intermolecular Hydrogen Bonds ◽  
Rietveld Refinements ◽  
Replacement Method ◽  
Metastable Form ◽  
Molecular Replacement Method

The structure of the metastable form I polymorph of the macrolide antibiotic clarithromycin, C38H69NO13, was determined by a powder diffraction method using synchrotron radiation. The space group of form I isP21212. The initial model was determined by a molecular replacement method using the structure of clarithromycin form 0 as a search model, and the final structure was obtained through Rietveld refinements. In the form I crystal structure, the clarithromycin molecules are aligned parallel along theaaxis in a head-to-tail manner with intermolecular hydrogen bonds between the hydroxy O atoms. The dimethylamine groups of the clarithromycin molecule interdigitate between neighbouring head-to-tail clarithromycin alignments. The novel crystal packing found in form I provides a mechanism that describes the transformation of form 0 to form I.

scholarly journals Fluoro-aluminoleakeite, NaNa2(Mg2Al2Li)Si8O22F2, a new mineral of the amphibole group from Norra Kärr, Sweden: description and crystal structure

2009 ◽  
Vol 73 (5) ◽  
pp. 817-824 ◽  
Author(s):  
R. Oberti ◽  
F. Cámaraite ◽  
F. C. Hawthorne ◽  
N. A. Ball
Keyword(s):  
Crystal Structure ◽  
Structure Refinement ◽  
Polarized Light ◽  
Crystal Structure Analysis ◽  
New Mineral ◽  
Monoclinic Space Group ◽  
Calculated Density ◽  
Greenish Blue ◽  
Dark Green ◽  
Pale Green

AbstractFluoro-aluminoleakeite, ideally , is a new mineral of the amphibole group from Norra Kärr, Sweden (IMA-CNMMNC 2009-012). It occurs in a proterozoic alkaline intrusion that mainly comprises a fine-grained schistose agpaitic nepheline-syenite (grennaite). Fluoro- aluminoleakeite occurs as isolated prismatic crystals 0.10–2 mm long in a syenitic matrix. Crystals are light greenish-blue with a greenish-blue streak. It is brittle, has a Mohs hardness of 6 and a splintery fracture; it is non-fluorescent with perfect {110} cleavage, no observable parting, and has a calculated density of 3.14 g cm–3. In plane-polarized light, it is pleochroic, X = pale green, Y = dark green, Z = pale green; X ^ a = 62.9° (in β obtuse), Y || b. Fluoro-aluminoleakeite is biaxial negative, α = 1.632(1), β = 1.638(1), γ = 1.643(1); 2Vobs. = 98.0(4)°, 2Vcalc. = 95.5°.MFluoro-aluminoleakeite is monoclinic, space group C2/m, a = 9.7043(5) Å, b = 17.7341(8) Å, c = 5.2833(3) Å, β = 104.067(4)°, V = 882.0(2) Å3, Z = 2. The eight strongest X-ray diffraction lines in the powder-diffraction pattern are [d in Å, (I), (hkl)]: 2.687, (100), (31, 151); 4.435, (80), (021, 040); 3.377, (80), (131); 2.527, (60), (02); 8.342, (50), (110); 3.096, (40), (310); 2.259, (40), (71, 12) and 2.557, (30), (002, 061). Analysis, by a combination of electron microprobe and crystal-structure refinement, gives SiO2 58.61, Al2O3 7.06, TiO2 0.32, FeO 3.27, Fe2O3 6.05, MgO 8.61, MnO 0.73, ZnO 0.43, CaO 0.05, Na2O 9.90, K2O 2.43, Li2O 1.62, F 3.37, H2Ocalc. 0.50, sum 101.08 wt.%. The formula unit, calculated on the basis of 24 (O,OH,F,Cl) p.f.u. with (OH) + F = 2 a.p.f.u., is A(Na0.65 O22W(F1.47OH0.53)Σ=2.00. Crystal-structure analysis shows CLi to be completely ordered at the M(3) site, and provided reliable site populations. Fluoro-aluminoleakeite is related to the end-member leakeite, , by the substitutions CFe3+ → CAl and WF → W(OH).

scholarly journals Ab InitioDetermination of the Novel Perovskite-Related Structure of La7Mo7O30from Powder Diffraction

1999 ◽  
Vol 142 (1) ◽  
pp. 228-235 ◽  
Author(s):  
F Goutenoire ◽  
R Retoux ◽  
E Suard ◽  
P Lacorre
Keyword(s):  
Powder Diffraction ◽  
Related Structure ◽  
The Novel

Multiple pituitary hormone gradients from inferior petrosal sinus sampling in Cushing's disease

1988 ◽  
Vol 119 (1) ◽  
pp. 75-80 ◽  
Author(s):  
Patricia A. Crock ◽  
Richard G. Pestell ◽  
Anthony J. Calenti ◽  
Eric J. Gilford ◽  
J. Keith Henderson ◽  
...  
Keyword(s):  
Cushing’S Disease ◽  
Anterior Pituitary ◽  
Close Association ◽  
Pituitary Hormones ◽  
Cushing's Disease ◽  
Pituitary Hormone ◽  
Inferior Petrosal Sinus ◽  
The Novel ◽  
Inferior Petrosal Sinus Sampling ◽  
Left And Right

Abstract. Pre-operative bilateral simultaneous inferior petrosal sinus sampling with assessment of ACTH levels in the left and right sinuses and the periphery was performed in 9 patients with pituitary dependent Cushing's disease who were subsequently found at surgery to have basophil microadenomata. The novel observation of this study was the pattern of secretion of other pituitary hormones so that significant inter-sinus gradients ≥ 1.4:1 were seen for β-endorphin (2.8 ± 1.3, mean ± sem), PRL (4.2 ± 1.3) and GH (6.9 ± 2.4) as well as for ACTH (5.1 ± 1.1). There was no inter-sinus gradient for LH, FSH and TSH. In these 9 patients with adenomata, the correlations between the inter-sinus gradients for ACTH and β-endorphin were r = 0.95 (P <0.01), ACTH and PRL r = 0.90 (P < 0.01) and for ACTH and GH r = 0.89 (P <0.05). This close association between the gradients for ACTH and other anterior pituitary hormones could be due either to cosecretion of β-endorphin, PRL and GH by the ACTH-producing pituitary adenomata or to a paracrine effect of β-endorphin from the tumours on adjacent pituitary tissue. By reflecting the central pituitary hormone milieu, petrosal sinus sampling can give information about pituitary function unobtainable from peripheral hormone levels.

Bobcookite, NaAl(UO2)2(SO4)4·18H2O and wetherillite, Na2Mg(UO2)2(SO4)4·18H2O, two new uranyl sulfate minerals from the Blue Lizard mine, San Juan County, Utah, USA

2015 ◽  
Vol 79 (3) ◽  
pp. 695-714 ◽  
Author(s):  
Anthony R. Kampf ◽  
Jakub Plášil ◽  
Anatoly V. Kasatkin ◽  
Joe Marty
Keyword(s):  
Hydrogen Bonds ◽  
White Light ◽  
Empirical Formula ◽  
San Juan ◽  
Uranyl Sulfate ◽  
Secondary Alteration ◽  
Pale Yellow ◽  
Conchoidal Fracture ◽  
Greenish Yellow ◽  
San Juan County

AbstractThe new minerals bobcookite (IMA 2014-030), NaAl(UO2)2(SO4)4·18H2O and wetherillite (IMA 2014-044), Na2Mg(UO2)2(SO4)4·18H2O, were found in the Blue Lizard mine, San Juan County, Utah, USA, where they occur together as secondary alteration phases in association with boyleite, chalcanthite, dietrichite, gypsum, hexahydrite, johannite, pickeringite and rozenite.Bobcookite descriptive details: lime green to greenish-yellow massive veins and columnar crystals; transparent; vitreous lustre; bright greenish-white fluorescence; pale greenish yellow streak; hardness (Mohs) 2½; brittle; conchoidal fracture; no cleavage; moderately hygroscopic; easily soluble in cold H2O; densitycalc= 2.669 g cm–3. Optically, biaxial (–), α = 1.501(1), β = 1.523(1), γ = 1.536(1) (white light); 2Vmeas.= 78(1)°; 2Vcalc.= 74°; dispersionr<v, moderate. Pleochroism:Xcolourless,Yvery pale yellow-green,Zpale yellow-green;X<Y<Z. EDS analyses yielded the empirical formula Na0.97Al1.09(U1.02O2)2(S0.98O4)4(H2O)18. Bobcookite is triclinic,P1,a= 7.7912(2),b= 10.5491(3),c= 11.2451(8) Å , α = 68.961(5), β = 70.909(5), γ = 87.139(6)°,V= 812.79(8) Å3andZ= 1. The structure (R1= 1.65% for 3580Fo> 4σF) contains [(UO2)(SO4)2(H2O)] chains linked by NaO4(H2O)2octahedra to form layers. Hydrogen bonds to insular Al(H2O)6 octahedra and isolated H2O groups hold the structure together. The mineral is named for Dr Robert (Bob) B. Cook of Auburn University, Alabama, USA.Wetherillite descriptive details: pale greenish-yellow blades; transparent; vitreous lustre; white streak; hardness (Mohs) 2; brittle; two cleavages, {101} perfect and {010} fair; conchoidal or curved fracture; easily soluble in cold H2O; densitycalc= 2.626 g cm–3. Optically, biaxial (+), α = 1.498(1), β = 1.508(1), γ = 1.519(1) (white light); 2Vmeas.= 88(1)°, 2Vcalc.= 87.9°; dispersion isr<v, distinct; optical orientation:Z=b,X∧a= 54° in obtuse β; pleochroism:Xcolourless,Ypale yellow-green,Zpale yellow-green;X<Y≈Z. EDS analyses yielded the empirical formula Na1.98(Mg0.58Zn0.24Cu0.11Fe0.092+)Σ1.02(U1.04O2)2(S0.98O4)4(H2O)18. Wetherillite is monoclinic,P21/c,a= 20.367(1),b= 6.8329(1),c= 12.903(3) Å, β = 107.879(10)°,V= 1709.0(5) Å3andZ= 2. The structure (R1= 1.39% for 3625Fo> 4σF) contains [(UO2)(SO4)2(H2O)] sheets parallel to {100}. Edge-sharing chains of Na(H2O)5O polyhedra link adjacent uranyl sulfate sheets forming a weakly bonded three-layer sandwich. The sandwich layers are linked to one another by hydrogen bonds through insular Mg(H2O)6octahedra and isolated H2O groups. The mineral is named for John Wetherill (1866–1944) and George W. Wetherill (1925–2006).

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