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I make art using a microscope and camera. I have heated ammonium sulphate that decomposes to ammonium hydrogen sulfate, melts, and then recrystalises to produce exceptionally beautiful birefiringent colours.

I am interested in its typical crystaline structure as perhaps other chemicals with similar structure may also be interesting artistically.

I have tried looking it up in ChemSpider, but no luck. I took some university courses in chemistry, so I have some (out of date) chemistry knowledge.

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    $\begingroup$ I looked up “polarized light microscopy art” and got hits, like this one: fineartamerica.com/art/polarized+light+microscopy. $\endgroup$
    – Ed V
    May 1 at 13:54
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    $\begingroup$ Crystal structure won't tell you much. Compounds with similar structure are not necessarily as good-looking, and moreover, the chemically related compounds do not necessarily have similar structure. $\endgroup$ May 1 at 13:56
  • $\begingroup$ Thanks for your answers/time. I occationally sell my images although I certainly need my day job. Good to know that maybe just structure might not best guide to crystals aesthetic qualities in polarised light...I would love to be able have a more systematic way of hunting for "good" crystals and thought this might have been a way forward. $\endgroup$
    – ben
    May 1 at 22:11
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Birefrigence is a result of structural anisotropy observed for crystals other than of the cubic Bravais class. Then, interaction of vectorial properties (e.g., light) with said material is anisotropic, too. It is a phenomenon seen both for inorganic, as well as organic materials (examples listed e.g., here). As seen e.g., by cooling films of molten polymers on a heat stage in polarization microscopy, local deviations from isotropy suffice to observe birefrigence, too (example). Thus, there is no «special functional group» which, if present, suddenly would switch on / switch off a sample to be birefrigent. It's observation and measurement by polarization microscopy allows to characterize the microstructure of e.g., minerals, and thus one of the elder tools in geology (still used today, e.g., Stoiber's «Crystal Identification with the Polarizing Microscope» by 1994 lists some in its freely available back matter). It may be used on organic samples, too (e.g., this tutorial).

The models to describe the crystal structure about ammonium sulfate, $\ce{(NH4)HSO4}$, depend on the temperature of the sample. This might increase or decrease birefrigence (I did not look out for a temperature-dependent recording of this about ammonium sulfate). The explored variation of sample temperature in the work below (at ambient pressure) however do not change the unit cell symmetry this much that birefrigence suddenly would be cancelled out for symmetry alone.

At room temperature ($\pu{293 K}$), the best description of this material that there two hydrogensulfate groups per unit cell which are described independently from each other:

enter image description here

(credit 2012JChemPhysChemA223, Fig. 1a / $\pu{293 K}$)

In the illustration, these are marked by O (ordered) and D (disordered). This is to say that the model describes the reality best assuming positions with $\ce{HSO^-4}$ with more than one orientation and local geometry. (Similar to sitting either forward, or backward on a chair.) This is, taking a different perspective on the sample (the representations omit hydrogen atoms):

enter image description here

(modified representation, based on 1972ActaCrystA445)

with ammonium ions, ordered and disordered $\ce{HSO^-4}$, the sites with the disordered would be either one of the following:

enter image description here

(credit 1972ActaCrystA445)

At lower temperatures, e.g. at $\pu{200 K}$ and at $\pu{125 K}$, it is energetically more favourable if both $\ce{NH^+4}$ and $\ce{HSO^-4}$ are in ordered position and orientation only, e.g.:

enter image description here

(credit 2012JChemPhysChemA223, Fig. 1b / $\pu{200 K}$)

This phase transitions and changes of unit cell symmetries (space group $P2_1/c$ (at $\pu{293 K}$) $\rightarrow$ $Pc$ (at $\pu{200 K}$) $\rightarrow$ $P1$ (at $\pu{125 K}$)) however will not cause a cancellation of birefrigence because of symmetry reasons.


You do not state (this much) why knowing the the spatial arrangement of the atoms, and hence a model of the crystal structure is important for you. However, because you mention to possess some command of chemistry and interest art, be aware among the crystallographers there are some equally with a sense for beauty. One of the low-level entries is IUCr's Crystal growing competition for school children (note the their brochure with examples in the later section) considerably newer than their teaching pamphlet.

On the more artistically appealing side, though, selectively dyeing crystals may be of interest for you. Work in this field was much popularized again by e.g. Bart Kahr:

enter image description here

(credit, includes protocol)

enter image description here

(credit 2001ChemRev893)

with protocols for chemicals easier to access (e.g., potassium dihydrogen phosphate [KDP] and amaranth dye, cf. here). Beside beauty, the selective incorporation of dyes provides insight into the growth mechanism of crystals. You may find additional inspiration in other works by him, e.g., in 1996AdvMat941, 2001ChemRev893 including a 20 page long table of examples («reported during the past 147 years»), or 2002CrystEngComm514 about «painting crystals» by an easy-to-follow protocol.

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  • $\begingroup$ Nice answer. But I'd like to see an explanation of the birefringence given the crystal structure. $\endgroup$
    – matt_black
    May 1 at 16:50
  • $\begingroup$ Thanks for the time you put into your answer including the actual structure and helpful guidance for me when I want to look up further structures. The crystals of interest to me have to be interesting under a microscope through crossed polaroids. I was interested in the structure as I had hoped that structure is guide to birefrigence which it appears it is only loosely. Thanks also commenters. What would be useful (to me and other microscopists) would be catalogue of crystals that are strongly birefrigent. Minerals are interesting but petrographic sildes are hard to make. $\endgroup$
    – ben
    May 1 at 22:20
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From considering crystal symmetry, we can only say if birefringence must be zero, not how strong it may be. Consider a wave propagating along an axis about which the crystal structure has a four-fold rotation symmetry. It should be clear that there can be no birefringence, since two waves that differ only by a 90-degree rotation of polarization will each see exactly the same crystal structure. This kind of thinking shows, for example, that a cubic crystal cannot be birefringent for any direction of propagation, while an orthorhombic crystal will have one direction with zero birefringence.

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    $\begingroup$ Thanks for this. Certainly I have found that sodium chloride has no birefringent properties.... $\endgroup$
    – ben
    May 1 at 22:13

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