Lead apatites : structural variations among Pb5(BO4)3Cl with B = P (pyromorphite), As (mimetite) and V (vanadinite)

The crystal structure of four Pb apatite samples, Pb5(BO4)3Cl, was refined with synchrotron high-resolution powder X-ray diffraction data, Rietveld refinements, space group P63/m and Z = 2. For this isotypic series, B = P5+ is pyromorphite, B = As5+ is mimetite and B = V5+ is vanadinite. The ionic r...

Ausführliche Beschreibung

Bibliographische Detailangaben
Veröffentlicht in:Journal of synchrotron radiation. - 1994. - 25(2018), Pt 1 vom: 01. Jan., Seite 214-221
1. Verfasser: Antao, Sytle M (VerfasserIn)
Weitere Verfasser: Dhaliwal, Inayat
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2018
Zugriff auf das übergeordnete Werk:Journal of synchrotron radiation
Schlagworte:Journal Article Rietveld refinement chemistry lead apatites mimetite pyromorphite structure synchrotron high-resolution powder X-ray diffraction (HRPXRD) vanadinite
LEADER 01000caa a22002652 4500
001 NLM279354398
003 DE-627
005 20250222200847.0
007 cr uuu---uuuuu
008 231225s2018 xx |||||o 00| ||eng c
024 7 |a 10.1107/S1600577517014217  |2 doi 
028 5 2 |a pubmed25n0931.xml 
035 |a (DE-627)NLM279354398 
035 |a (NLM)29271770 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Antao, Sytle M  |e verfasserin  |4 aut 
245 1 0 |a Lead apatites  |b structural variations among Pb5(BO4)3Cl with B = P (pyromorphite), As (mimetite) and V (vanadinite) 
264 1 |c 2018 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Revised 20.11.2019 
500 |a published: Print-Electronic 
500 |a Citation Status PubMed-not-MEDLINE 
520 |a The crystal structure of four Pb apatite samples, Pb5(BO4)3Cl, was refined with synchrotron high-resolution powder X-ray diffraction data, Rietveld refinements, space group P63/m and Z = 2. For this isotypic series, B = P5+ is pyromorphite, B = As5+ is mimetite and B = V5+ is vanadinite. The ionic radius for As5+ (0.355 Å) is similar to that of V5+ (0.335 Å), and this is twice as large as that for P5+ (0.170 Å). However, the c unit-cell parameter for mimetite is surprisingly different from that of vanadinite, although their unit-cell volumes, V, are almost equal to each other. No explanation was available for this peculiar c-axis value for mimetite. Structural parameters such as average 〈B-O〉 [4], 〈Pb1-O9〉 [9] and 〈Pb2-O6Cl2〉 [8] distances increase linearly with V (the coordination numbers for the cations are given in square brackets). Mimetite has a short Pb2-O1 distance, so the O1 oxygen atom interacts with the 6s2 lone-pair electrons of the Pb2+ cation that causes the Cl-Cl distance (= c/2) to increase to the largest value in the series because of repulsion, which causes the c-axis to increase anomalously. Although Pb apatite minerals occur naturally in ore deposits, they are also formed as scaly deposits in lead water pipes that give rise to lead in tap water, as was found recently in Flint, Michigan, USA. It is important to identify Pb-containing phases in water-pipe deposits 
650 4 |a Journal Article 
650 4 |a Rietveld refinement 
650 4 |a chemistry 
650 4 |a lead apatites 
650 4 |a mimetite 
650 4 |a pyromorphite 
650 4 |a structure 
650 4 |a synchrotron high-resolution powder X-ray diffraction (HRPXRD) 
650 4 |a vanadinite 
700 1 |a Dhaliwal, Inayat  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Journal of synchrotron radiation  |d 1994  |g 25(2018), Pt 1 vom: 01. Jan., Seite 214-221  |w (DE-627)NLM09824129X  |x 1600-5775  |7 nnns 
773 1 8 |g volume:25  |g year:2018  |g number:Pt 1  |g day:01  |g month:01  |g pages:214-221 
856 4 0 |u http://dx.doi.org/10.1107/S1600577517014217  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_40 
912 |a GBV_ILN_350 
912 |a GBV_ILN_2005 
951 |a AR 
952 |d 25  |j 2018  |e Pt 1  |b 01  |c 01  |h 214-221