An IsoFind extension is a method that runs. It carries the name of whoever wrote it and its version number, installs offline from a signed archive, and replays identically. That is exactly what a paper rarely describes precisely enough to be reproduced.
At the heart of the suite, two flagship extensions bring the full power of R and PHREEQC directly into IsoFind, with no installation and no connection.
A complete R environment, running locally
The full power of R, embedded in IsoFind through WebR. Your code runs on your machine, with no R install and no connection, with direct access to your samples.
Geochemical modelling, offline
PHREEQC, the USGS reference code, embedded in IsoFind. Speciation, saturation indices and process interpretation, directly on your samples.
Search, filter by category and sort. The download provides a .isplugin archive, to open in IsoFind to install it.
An extension is a folder of scripts and a manifest. Download IsoFind to install the ones in the catalogue, or start from the documentation to publish your own.
The full power of the R language, embedded in IsoFind through WebR. Your code runs entirely on your machine, with no R installation and no connection, with direct access to your samples and analyses. You keep full control of your data, from computation to plot.
PHREEQC, the reference geochemical code from the USGS, embedded in IsoFind and compiled to WebAssembly. The console computes aqueous speciation, mineral equilibria and saturation indices, then turns it all into a readable interpretation, directly on your samples. All computation stays on your machine.
pH, pe and temperature via sliders, element list, then compute.
Raw PHREEQC input, full control of the blocks.
Vary a condition and track the evolution.
Vary pH, pe or temperature over a range, and track how the species and the saturation indices of the chosen minerals evolve. The console detects the crossover thresholds by interpolation and reports them, for example the exact pH at which goethite becomes oversaturated. This is the direct answer to the threshold at which a precipitation or dissolution process kicks in.
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