Ilya Bindeman's stable isotope lab
Jim Watkins' or one of the other second floor labs
TSA's various shops, hanging with mi paesani

• SOLTHERM.XPT  —  Now with tourmaline and latest basis set component #66^† univalent lithium. Sweet, sweet, lithium  —  Based on internally consistent mineral and gas phase data from Holland and Powell 2011, and updated Supcrt92 aqueous species data.
  
• XPT-LogK - a utility for extracting and interpolating log K's in Soltherm
  
• SOLPRINT-2011-XPT.txt - distilled from SOLTHERM as a user reference, showing balanced reactions and log K's at liquid-vapor saturation from 25 to 350 °C
• SolthermBRGM.xpt | SolprintBRGM.txt - *BRGM *Thermoddem data, reformatted from the ToughReact *version.  For the Martians, and other low temperature peoples
• Gas.sto - gas stoichiometry data for programs GEOCAL and VOLCAL | Minox.dat - reactant stoichiometry data for CHIM-XPT
• Manuals: SOLVEQ-XPT and CHIM-XPT
  

• Delicious water, what are thine properties? So too ethereal vapor phase thereof - Steam Tables - pdf, csv
  
• Fugacity coefficients in mixtures of H₂O, CO₂, and NaCl at high P and T. Program Fugco, with a worked example as in the cited reference, and included as subroutines in CHIM-XPT

• GASTHERM.DAT - for programs GASWORKS, SOLVGAS, and VOLCAL. The principles of operation of these programs are similar to those of CHIM-XPT, SOLVEQ, and VOLCAL, except the mobile phase that carries all of the components is the gaseous phase rather than aqueous. The software was developed to assess how gas exsolved from magma reacts with host rock, and so in compilation of the data there was a bias toward gases that are observed in fumaroles or might occur there or beneath. Similarly, minerals, solids, and liquids compiled within GASTHERM are focused on those same environments. And yet, many entries suggest compilation of anything that was available at the time. A significant issue is the absence of most digital records of the enthalpy, entropy, and heat capacity data that were used to compute the log K's for the gases. The situation is only slightly better for the minerals and solids. On the up side, the sources of data are well documented, and it is clear already that improved data exist. Since there is some interest in resurrecting this collection, good times are afoot.
  

• Supcrt92.zip - the original distribution from Johnson et al. 1992 using Maier-Kelly heat capacity: C_p = a + b T + c T^-2
• Supcrt96 | Source | Win32 - derived from Supcrt92 to use Maier-Kelly heat capacity, and adding Powell and Holland 1990: C_p = a + b T + c T^-2 + d T^-0.5
• Cprons96 | Source | Win32- derived from Cprons92. Converts any (including any of those for Supcrt92) properly formatted sequential access database to direct access, suitable for use with Supcrt96
  
• Data
• The most current Supcrt92 data might be found at the Gitlab ENKI portal, in Everett Shock's Geopig workgroup space, file Slop16.dat. This group has done phenomenal work in adding data for organic compounds. Changes in slop16 relative to 07 include the addition of many new organic compounds, now for the first time including crystalline solids(!); changes to inorganic aqueous species are minimal and not yet adopted in SOLTHERM. Related, if a naturally occurring gas or liquid H-C compound, with or without additional N, O, S, etc., is properly cooled by nature so that it is crystalline, is it not a mineral? Looking at you, Sol system outer planets
  
• *Thermocalc- for phase equilibria computations - application and data from Tim *Holland.  The primary application for which the Holland and Powell 2011 compiled their data
  
• SPRONS and DPRONS - Sequential- and Direct-access PROperties of Natural Substances, as per Johnson et al 1992. The sequential access file is for data addition and editing, which is then processed by Cprons into the direct access version for increased Supcrt execution speed
  
• SPRONS92.DAT - The original masterpiece
• SpronsHP2011.dat - The most recent sequential access version contains aqueous species from Slop07.dat and SpronsAqs, and minerals and gases from SpronsH&P2011minerals, from Slop07 those that are not already present in SpronsH&P2011, and Sprons96Misc
• dpronshp.dat -  The above file piped through Cprons96 and ready to use with Supcrt96
  
• SpronsH&P2011minerals.dat - Mineral and gas phase data derived from Holland and Powell 2011 in the format for which Supcr96 and Cprons96 were originally hacked in 1996. The data is *updated and revised occasionally by Holland and Powell; the 2011 version can be found here
  
• Sprons96Misc.dat - Bonus mineral and gas phase data from other sources, also properly formatted for Supcrt96
• SpronsAqs.dat - Bonus aqueous phase data too, properly formatted for any version of Supcrt. In particular, H₄SiO₄,aq. from Stefánsson 2001; rarely does so very much hinge upon so very little
• Locally kept are two Sprons versions, Slop16.dat from Shock et al. with only added H₄SiO₄,aq. from Stefánsson, and SpronsHP2011.dat with identical aqueous species, all of SpronsH&P2011minerals.dat, and the other miscellaneous items from Sprons96Misc.dat and SpronsAqs.dat.
  

Experimental petrology

• CSPV North - LabVIEW v.2012sp1/WinXP
  
• CSPV South - LabVIEW v.2018/Win10-64
• Related items
  

Isotope ratio mass spectrometry

• Reference info, mostly
  

• Some photos of the setup, before it was boxed up
  

• Geologic map [A, B, L] of Muddy Ranch - aka Rajneeshpuram, aka Washington Family Ranch - and vicinity, north of Currant and Muddy Creeks, Wasco, Wheeler, and Jefferson Counties, Oregon (1993)
  
• Streetcar map of Eugene, OR, 1907-1928. Exposed track may still be seen on Moss, Columbia, and University Streets. Modified from a map published in Eugene Weekly in 2008
• Some photographs of the I-5 Whilamut Passage Bridge replacement and related construction, near milepost OR 192
• Related items
  

The data

•  It wants to be free

^† Bringing us to 55 of 82^‡ stable elements in the Soltherm basis set. The other items being metastable acetate, oxalate, succinate, malonate, CH₄, H₂, N₂, and NH₃, radioactive UO₂⁺ and Pm⁺³, and alternate redox component O₂ - redox state is defined by either paired sulfate-sulfide or H₂O-O₂. A legacy from the era of 16-bit operating systems, when use of sulfide for an oxidizing system, or O₂ for a reducing system, might cause an array underflow. Since water must be present and sulfate is so common, basis components sulfide and O₂ are hard coded to be mutually exclusive. Pick one.
^‡ Bismuth-209 undergoes α-decay to ²⁰⁵Tl with a half-life of 2.01x10¹⁹ years, or, ~1.46x10⁰⁹ times the 1.38*10¹⁰ or so year age of our observable universe. To not be a pedant but only in this one case, bismuth is deemed stable. So 82 rather than 81.