(...) is the fact that this concentration doesn't appear in the calculation of Keq = (C) / (A) x (B).
I don't know how you possibly could come to this expression.
for example, a well known constant is about the esterification of acetic acid with ethanol:
C
2H
5OH + CH
3COOH
CH
3COOC
2H
5 + H
2O
where of course the water does show up in the respective LMA expression:
K ≈ 4 = [CH
3COOC
2H
5] * [
H2O] / ( [C
2H
5OH] * [CH
3COOH] )
hence, in a waterbased environment, with let's say c
0 (ethanol, acetic acid) = 0.1 M and water at a ~ constant 55 M , you'd have like 7.2 * 10
-4 M of ester in equilibrium
as you see, this reaction
is feasible - though the net gain is small.*
)However, talking about the origin of life / the "chemical evolution" part , all these considerations about condensation at / near room temperature might well be beside the point, as for example the
Miller/Urey experiment teaches us.
It may well be that those fundamental molecules of life didn't come into being in a lukewarm pool of water, but with thunder and lightning, erupting volcano's lava meeting the sea, and in the
superheated brine in black smokers, instead.
... and
this changes
everythingThus ΔG is independent of water concentrations.
as shown above, it isn't
regards
Ingo
*
)however, at times even small concentrations might well be high enough to create a protective environment. think about soap, and how little soap is required to produce
micelles