Abstract:
It has been a longstanding issue in the radiation chemistry of water
that, even though H2 is a molecular product, its “escape” yield g(H2)
increases with increasing temperature. A main source of H2 is the
bimolecular reaction of two hydrated electrons (e-aq).
The temperature
dependence of the rate constant of this reaction (k1), measured under
alkaline conditions, reveals that the rate constant drops abruptly above
~150°C. Recently, it has been suggested that this temperature
dependence should be regarded as being independent of pH and used in
high-temperature modeling of near-neutral water radiolysis. However,
when this drop in the e-aq self-reaction rate constant is included in
low (isolated spurs) and high (cylindrical tracks) linear energy
transfer (LET) modeling calculations, g(H2) shows a marked downward
discontinuity at ~150°C which is not observed experimentally. The
consequences of the presence of this discontinuity in g(H2) for both low
and high LET radiation are briefly discussed in this communication. It
is concluded that the applicability of the sudden drop in k1 observed at
~150°C in alkaline water to near-neutral water is questionable and that
further measurements of the rate constant in pure water are highly
desirable.
Keyword: Water radiolysis; High temperature; Self-reaction of the hydrated
electron; Rate constant; Yield of H2; Linear energy transfer (LET);
Monte Carlo track chemistry calculations
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