Oxaloacetic acid (OAA) is a 3-oxocarboxylic
acid formed from the
oxidation of succinic acid. OAA and other 3-oxocarboxylic acids experience
a decarboxylation reaction in aqueous solutions, which can be catalyzed
by ammonium and amines. This catalysis has not been studied under
atmospherically relevant conditions despite previous interest in OAA
in the atmosphere. To address this, 1 mM solutions of OAA were prepared
with varying concentrations of ammonium sulfate, ammonium bisulfate,
ammonium chloride, and sodium sulfate to simulate various atmospheric
conditions. The extent of the decarboxylation was monitored using
UV–visible absorption spectroscopy. OAA’s uncatalyzed
decarboxylation lifetime was around 5 h. Under moderately acidic conditions
representative of aerosol particles (pH = 3–4), the decarboxylation
rate increased linearly with ammonium concentration up to about 2.7
M, after which additional ammonium had no effect. The effective lifetime
of OAA reduced to approximately 1 h under these conditions. Density
functional theory calculations support the proposed catalytic mechanism,
predicting the free energy barrier height for decarboxylation to be
approximately 21 kcal/mol lower after OAA has reacted with ammonium.
In more acidic solutions (pH < 1), OAA’s decarboxylation
was suppressed, with lifetimes of tens of hours, even in the presence
of ammonium. A comparison of the decarboxylation rate with the expected
rate of oxidation by OH suggests that decarboxylation will be the
dominant loss mechanism for OAA, and presumably other 3-oxocarboxylic
acids, in aerosol particles and cloud/fog droplets. This result explains
why OAA is hard to detect in field measurements even though it is
a known oxidation product of succinic acid.