The Department of Materials Science and Engineering has generously licensed Crystal Maker, including CrystalDiffract and SingleCrystal, under a campus agreement, allowing any Drexel student or researcher to use it for academic or research purposes.

Installation♯

CrystalMaker, CrystalDiffract, and SingleCrystal are available to install on all Engineering computers attached to the Drexel domain via Software Center.

Crystalmaker Software Ltd

CrystalMaker homepage. User's guide - available under the Help menu in the software (Help CrystalMaker User's Guide) Additional crystal libraries; Video tours; Support main page. Visualization and analysis of crystal structures using CrystalMaker software.

The license codes are also available in the Software share on the COE File Server and can be accessed by any Drexel.edu account. The file also includes download locations to obtain the latest versions of the software installers for Windows and macOS.

The license is renewed annually around the end of September, so please refer back to that location on the file server for new codes once the software requests them.

• Excuse me, Do you have an alternative program for CrystalMaker? I mean a free program to build a crystal of an inorganic material such as TiO2, ZnO, Fe3O4.etc which can be an alternative.
• CrystalMaker provides a collection of applications for exploring crystal lattices and their diffractions. Thayer School has purchased a departmental site license (all applications, all users, all purposes) for all these applications which will need to be renewed each year, at which time we will evaluate whether we should renew this annual license or not.

CrystalMaker

To assist our understanding of the diverse structural characteristics of sour corrosion products, the interactive crystal structure visualization software package CrystalMaker 1.4.4 was recently purchased. Lattices are generated from inputted structural data, usually as “Crystal Information Files” (CIFs) from online databases. CIFs are a standard method of reporting crystallographic data for individual structures, i.e., unit cell information, atomic coordinates and space group. The benefit of using CrystalMaker is that generated crystal structures can be manipulated, coordination environments displayed and basic measurements performed (bond lengths/angles, density). The software is user friendly and enables generation of crystal structure images for use in reports, papers, presentations, proposals, etc. Most importantly, CrystalMaker gives the researcher a “feel” for the structures with which they are working; this has proved useful for visualizing, and helping develop an understanding of, corrosion products such as siderite (FeCO₃), mackinawite (FeS), troilite (FeS), pyrrhotite (Fe_1-xS), smythite (Fe_3+xS₄), greigite (Fe₃S₄) and pyrite (FeS₂). Mackinawite and troilite/pyrrhotites are routinely observed in sour corrosion systems, as well as in our on-going research at the ICMT. Stoichiometric versions of each phase would have the formula FeS, with a pyrrhotite that is not deficient in iron possessing the troilite lattice. Structurally, the lattices of mackinawite and troilite are completely different. Each phase tends to form under particular conditions.

Mackinawite is a layered iron sulfide, often written with the formula Fe_1+xS as it is usually found with a non-stoichiometric composition. It is readily formed at temperatures of less than 100°C at relatively short times in sour corrosion systems. Mackinawite has a tetragonal unit cell: a = b = 3.6735 Å, c = 5.0328 Å, c = 5.0328 Å; α = β = γ = 90°. Consequently, it is frequently referred to as “tetragonal iron sulfide”. A single unit cell is shown in Figure 1 (brown = iron, yellow = sulfur). The iron atoms are at the apices and at the center of the square faces on opposite sides of the unit cell. The sulfurs are positioned on the elongated sides of the unit cell. The long axis of the cell corresponds to the direction in which the iron sulfide layers within the mackinawite structure stack, multiple unit cells are shown in Figure 2; its 2-dimensional structure is now obvious. A close-up of the crystal structure reveals that the iron atoms are essentially embedded within each layer, tetrahedrally coordinated to sulfurs. The sulfurs are similarly 4-coordinate, but in more of a pyramidal geometry, Figure 3. Mackinawite layers depicted with Shannon radii (Fe²⁺ radius set to 0.63 Å, S^2- to 1.84 Å), which more accurately reflect the actual/relative sizes of the atoms in the lattice, see Figure 4, reveal that the layers are sufficiently far apart for species to reside/diffuse “between the sheets”. Wolthers et al. have hypothesized that water molecules intercalate into the mackinawite lattice during its hydrothermal formation.

Troilite and the pyrrhotites essentially possess the niccolite, or nickel arsenide, characteristic crystal structure; albeit with distortions and, in the case of pyrrhotites, iron deficiency. In corrosion systems, these phases typically occur at temperatures in excess of 100°C, although their formation over long periods of time at lower temperatures may also be possible. The hexagonal arrangement of iron and sulfur atoms in the troilite lattice, viewed perpendicular to the xy-plane, is shown in Figure 5. Troilite can be described as an expanded/distorted hcp anion array with cations in the octahedral holes, or vice versa. Its unit cell parameters are a = b = 5.9650 Å, c = 11.7570 Å; α = β = 90°, γ = 120°. Unlike mackinawite, troilite possesses a 3-dimensional framework. It is worth noting that troilite is of significantly higher density than mackinawite, 4.835 g/cm³ versus 4.298g/cm³. Figure 6 depicts a view of its lattice after it has undergone rotation to illustrate the alternating nature of the iron and sulfur within the crystal structure. Inspection of the figure reveals the stoichiometric nature of troilite, with Fe:S = 1:1. The 6-coordinate, distorted octahedral character of the irons and sulfurs within the lattice is clear from Figure 7. Pyrrhotite has essentially the same framework architecture as troilite, except that irons are systematically absent from the lattice. Pyrrhotite formulae tend to be written as Fe_1-xS, where x < 0.20, or Fe_yS_z. The non-stoichiometry results from replacement of Fe²⁺ in the lattice with Fe³⁺, fewer of which are required for charge balance of the S^2- anions.

A long term goal of the CC-JIP is to study the formation and interconversion of iron sulfides under conditions where localized corrosion occurs.

References
(1) Lennie, A.R.; Redfern, S. A. T.; Schofield, P.F.; Vaughan, D.J. Synthesis and Rietveld Crystal Structure Refinement of Mackinawite, Tetragonal FeS. Mineralogical Magazine 1995, 59, 677-683.
(2) Wolthers, M.; Van der Gaast, S.J., Rickard, D. The Structure of Disordered Mackinawite, American Mineralogist, 2003, 88(11), 2007-2015.
(3) Skala, R.; Cisarova, I.; Drabek, M. Inversion Twinning in Troilite. American Mineralogist, 2006, 91, 917-921.

Crystalmaker Mac

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