Quote: | Originally posted by neutrino
One I accidentally discovered: mixing calcium chloride and magnesium sulfate solutions, then heating the resulting paste to decomposition releases
HCl. It goes something like this:
Ca<sup>2+</sup><sub></sub> + SO<sub>4</sub><sup>2-</sup> --> CaSO<sub>4</sub>
Drying, we get solid MgCl<sub>2</sub> . 6H<sub>2</sub>O. Finally,
2MgCl<sub>2</sub> . 6H<sub>2</sub>O --heat --> Mg<sub>2</sub>OCl<sub>2</sub> +
H<sub>2</sub>O + HCl |
Good point: some chlorides decompose a significant amount. Alkaline earth and transistion metal chlorides (and especially aluminum chloride hydrate)
decompose, giving off HCl fumes with some amount of H2O, allowing muriatic acid to be distilled directly in low yield.
Sulfuric acid of course is had in higher yield from anhydrous iron, copper, or to a lesser extent zinc, sulfates.
Cinnabar is the primary mercury ore, you just have to find it -- mercury isn't very common in the Earth's crust after all, but just like silver, it's
there. Mercury (elemental) and I think the oxide are also present to some extent.
Chalk, limestone and dolomite: all the calcium oxide and carbon dioxide you could hope for, most formations are several feet thick (up to a few
hundred) and span thousands of miles. After calcining to yellow heat for an hour or three (big pieces may need days, cleaving into 1" slabs would
help here) you're left with CaO and a lot of CO2 out the stack, which can be pumped and compressed, or bubbled into a solution for collection: read up
on the Solvay process, which produces CaCl2 as a byproduct for well, given the materials CaCO3 + NaCl, I think you can guess why.
Oh, and let's not forget CaO is also the primordial alkali. Why?
The magnesium ought to be leachable, perhaps by dissolving a block of dolomite and precipitating CaCO3 with MgCO3 (from more dolomite? Dunno) to give
seperate Ca and Mg (salt) products.
But this is kind of off the direction... a great conversation as well but I was thinking more what you do with it. (Or maybe I'm wasting my time
explaining; this is an interesting enough angle, at least.) Like, my oxidizer example: besides oxygen in air, about the only natural thing you have
is MnO2, which can oxidize Cl- to Cl2. The MnCl2 can be precipitated and reoxidized with oxygen and fire or weathering and time (as happens
naturally). That Cl2 gas can go on to do just about anything, up to and including things like permanganate (which can also be made from pyrolusite
and a caustic fusion, in air), perchlorate, ferrate and so on.
And heck, primordial electrochemistry is worth thinking about, too. It's a lot of effort to mine, roast, smelt, distill and cast zinc anodes, but it
can be done. Copper can be mined, roasted and smelted with a bit more ease, though it needs more fire to cast it (not a problem for a firetender such
as myself ). Electrolyte, well that can be made from whatever, be it acid, base
or a salt. Given enough surface area and a few cells, you can do all the standard electrochemistry, well assuming you can isolate platinum, and make chlorates, persulfates and the ever most venomous fluorine, as well as the
strongest reducers, the alkali metals (which can in fact be isolated by carbothermic processes!).
Organic chemistry of course all starts with organic chemicals, since it's a waste to start with CO2 and there's so much plant and animal life
available to the desperate Mad Scientist. Finding the source of reagents (oh my, and glassware! ) for these synthesis might prove an interesting angle however.
Tim |