1951
DOI: 10.1002/zaac.19512660604
|View full text |Cite
|
Sign up to set email alerts
|

Strukturuntersuchung der Monoklinen Arsenikmodifikation Claudetit

Abstract: Claudetiteinkristalle werden bei Temperaturen oberhalb des Umwandlungspunktes Arsenolith‐Claudetit aus Arsenolith gezüchtet. Die Identität mit dem natürlichen Claudetit wird sichergestellt. Bei den Züchtungsversuchen wird noch eine weitere bisher unbekannte kristalline Modifikation erhalten, deren Existenz durch Röntgenaufnahmen gesichert werden kan. Drehkristall‐, Schwenk‐ und Weissenberg‐Aufnahmen um verschiedene Achsen ergeben die monokline Raumgruppe C 2h5‐P21/ mit den Daten: a1 = 5,25 Å; a2 = 12,90 Å; a3 … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
7
0
1

Year Published

1951
1951
2021
2021

Publication Types

Select...
8
1
1

Relationship

0
10

Authors

Journals

citations
Cited by 37 publications
(8 citation statements)
references
References 5 publications
0
7
0
1
Order By: Relevance
“…In As 2 O 3 , three of the dynamically stable defective fluorite structures ( 100 -LS, 111 -LS, and valentinite-LS arrangements) exhibit relative energies of less than 0.1 eV/f.u. Although arsenolite-As 2 O 3 is the low-temperature phase according to an experimental report, 34 the corresponding arrangement, 111 -LS, has 0.05 eV/f.u. higher energy than the claudetite-As 2 O 3 -type arrangement.…”
Section: A Symmetry Breaking From Ideal Defective Fluorite Structuresmentioning
confidence: 98%
“…In As 2 O 3 , three of the dynamically stable defective fluorite structures ( 100 -LS, 111 -LS, and valentinite-LS arrangements) exhibit relative energies of less than 0.1 eV/f.u. Although arsenolite-As 2 O 3 is the low-temperature phase according to an experimental report, 34 the corresponding arrangement, 111 -LS, has 0.05 eV/f.u. higher energy than the claudetite-As 2 O 3 -type arrangement.…”
Section: A Symmetry Breaking From Ideal Defective Fluorite Structuresmentioning
confidence: 98%
“…Polymorphism of arsenic­(III) oxide has attracted attention for years. There are two minerals of As 2 O 3 : cubic arsenolite containing adamantoid As 4 O 6 molecules packed in a three-dimensional (3D) diamond network , and monoclinic claudetite I consisting of highly corrugated As 2 O 3 layers. In the late 1940s, another monoclinic modification was discovered and called claudetite II because of its extended layers that resembled those of claudetite I. , Well-known also is a glassy As 2 O 3 modification. There have been a few studies of arsenic­(III) oxide polymorphs under high pressure.…”
Section: Introductionmentioning
confidence: 99%
“…These two secondary polymorph phases range in color from white to bluish and pale yellow, depending on the levels of impurities. Arsenolite's crystal structure was investigated by Bozorth (1923), Pertlik (1978a), Treacy and Taylor (1981) and Ballirano and Maras (2002) while that of claudetite was studied by Becker et al (1951Becker et al ( , 1954, Frueh (1951), Pertlik (1975 and1978b) and Treacy and Taylor (1981).…”
Section: Arsenolite and Claudetite (As 2 O 3 )mentioning
confidence: 99%