Jim Palandri
Research Associate
Department of Earth Sciences
1272 University of Oregon
Eugene, Oregon 97403-1272
Jim might be found in:
Ilya
Bindeman's stable isotope lab
Somewhere in one of the second floor labs
TSA's various shops, hanging
with mi paesani
Handy links to mostly local items, and
some off-site items(*) commonly with broken links
Items related to local applications CHIM-XPT, SOLVEQ-XPT, and GEOCAL
- 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
Supcrt-related items for computing log K's in SOLTHERM
- Supcrt92.zip
- the original distribution from Johnson et al. 1992
using Maier-Kelly heat capacity: Cp = a + b T + c T-2
- Supcrt96 | Source
| Win32
- derived from Supcrt92 to use Maier-Kelly heat capacity, and
adding Powell and Holland 1990:
Cp = 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 we keep 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 reference items
Isotope ratio mass spectrometry
- More reference info, also
mostly local
Fluid inclusions
Just for fun
- 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 photos
of the I-5 Whilamut
Passage Bridge replacement and related construction, near
milepost OR 192
The data
† 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.
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.