EVANSITE

 


Chemical formula: Al3(PO4)(OH)6 6H2O (?)

Family: Phosphates, Arseniates, Vanadates

Status: IMA-GP

Crystal system : Amorphous

Display mineral: NON

Associated names (luminescent varieties, discredited names, synonyms, etc.): BOLIVARITE

 

Luminescence:

Longwave UV (365nm) colors:

              


Greenish white , Bluish White , Yellowish White ,

Midwave UV (320nm) colors:

              


Greenish white , Bluish White , Yellowish White ,

Shortwave UV (254nm) colors:

                   


Yellowish Green , Bluish White , Greenish , Greenish white ,


Daylight picture


CALCITE (improperly labeled EVANSITE), Richelle, Visé, Province de Liège, Belgique;
Daylight
Col. G.Barmarin; Photo: G. Barmarin

Longwave (365nm) picture


CALCITE (improperly labeled EVANSITE), Richelle, Visé, Province de Liège, Belgique;
UVLW
Col. G.Barmarin; Photo: G. Barmarin

Shortwave (254nm) picture


CALCITE (improperly labeled EVANSITE), Richelle, Visé, Province de Liège, Belgique;
UVSW
Col. G.Barmarin; Photo: G. Barmarin

 

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Phosphorescence (in the common sense of the term) observable with the naked eye:

No data

Comments:

Rik Dillen and Axel Emmermann have shown (2021) that evansite samples from a deposit along a road in Richelle (Belgium) and presenting a globular crust facies on a schistose rock (see picture), sold for decades on Belgian mineral fairs with the label evansite, are in fact mainly made of calcite (see also Philippo, 2019). An analysis by Raman spectrometry on several points of a sample of this type in my collection unambiguously indicates the presence of calcium carbonate and not of evansite (aluminum phospate). The fluorescence is also quite similar to that of many calcites.

 

In some amateur collections, other samples of Richelle's evansite on a completely different matrix (breccia) also appear to be fluorescent as mentionned by Van Tassel in his paper (1959, see bibliography), but their exact nature needs to be confirmed (green crandallite?). The morphology of the samples described by Van Tassel in the gray breccia of Argenteau (white to gray nodules not exceeding one millimeter but showing fuorescence in blue-white tints) still does not correspond to these samples. In the book 'Les minéraux de Belgique' (Fransolet et al., 1974) evansite is not on the list of minerals from the locality of Richelle, but that of Argenteau (Philippo, 2019).

 

The fluorescence of real evansite samples from Belgium therefore remains to be studied.

Activator(s) and spectrum:

Activator(s): (UO2)2+ (ion Uranyle) en impureté, ST (Singlet-triplet)-Matière organique en impureté,  

Peaks in the spectrum (nm):

Organic impurities: Broad band centered around 500-550nm (not related to evansite but calcite from Richelle)


Col. G. Barmarin; Spectre: G. Barmarin

Comments on spectrum and activators:

The spectrum shape of classic samples from Richelle combined with strong phosphorescence lets think that the fluorescence is due to organic impurities (but finally those samples seem to be only common calcite!);

Green fluorescence is clearly due to uranium in impurities (see bibliography).

Best localities for fluorescence (*):

 

(*)The data are not exhaustive and are limited to a few remarkable localities for fluorescence

Bibliographic reference for luminescence:

Reference for luminescence on the Internet:

Mineralogical reference on the Internet:

  http://www.mindat.org/show.php?name=Evansite

  http://webmineral.com/data/Evansite.shtml

Internet Search:

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