Ilya Bindeman's stable isotope lab
Jim Watkins' & Mark Reed's lab area
TSA's various shops, hanging with mi paesani

• SOLTHERM-2011.XPT  —  Now with tourmaline and latest basis 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. Additional items from many sources include minerals and aqueous species added to the local Supcrt database e.g. tourmaline, or log K's added directly to Soltherm which are always limited to conditions of liquid-vapor saturation e.g. florencite. See below for more on Supcrt.  
  
• 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
• A provisional version of SOLTHERM with updated Al-bearing aqueous species data from Tagirov and Schott 2001, and attendant SOLPRINT
  
• 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
  

• GASTHERM.DAT - for programs GASWORKS, SOLVGAS, and VOLCAL

• 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

• 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
  
• Supcrt3000 - derived from Supcrt96  to use either Maier-Kelly or Holland-Powell heat capacity, and adding Robie et al. 1979: C_p = a + b T + c T^-2 + d T^-0.5 + e T²
  
• Formulation of these bits of code is left as a worthy exercise for an enterprising or conscripted young graduate student. If other terms were under consideration for addition, e.g. Berman and Brown T^-1 and T^-3, this would be the iteration in which to add those. Also, extend to minerals with phase transitions. Also, and too, add an option and switch for output in SI units, ha ha ha ha ha.
  
• 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
• The generalized strategery is to keep two versions of the database. One version is simply the latest version from Shock et al., Slop16.dat, with a single addition of H₄SiO₄,aq. from Stefánsson as mentioned above, and the other version contains identical aqueous species data, all the Holland and Powell data, and all other miscellaneous additions, in SpronsHP2011.dat.
  

Experimental petrology

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

Isotope ratio mass spectrometry

• CTC GC PAL maintenance guide. So much win in this one
  
• Related items

• Related items

• Geologic map [A, B, L] of Big 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
• For sale, but in no particular hurry to sell - 1984 Trek 720 touring bicycle. Make me an offer I can not refuse.
  
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The data

•  It wants to be free.

^† Bringing us to 57 of 82^‡ stable elements in our basis set. 
^‡ 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 single case, bismuth is deemed stable. So 82 rather than 81.