First Observation of Picosecond Kinetics of Hydrated Electrons in Supercritical Water

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Mingzhang Lin ◽  
Vincent de Waele ◽  
Yoshihiko Hatano ◽  
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...  
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Author(s):  
Steven F. Rice ◽  
Jefferson W. Tester ◽  
Kenneth Brezinsky

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Donghai Xu ◽  
Yang Guo ◽  
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Yuzhen Wang ◽  
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Won Bae Kong ◽  
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Jimoon Kang ◽  
Hwi-Sung Lee ◽  
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2007 ◽  
Vol 21 (5) ◽  
pp. 2840-2845 ◽  
Author(s):  
Anatoli A. Vostrikov ◽  
Sergey A. Psarov ◽  
Dmitri Yu. Dubov ◽  
Oxana N. Fedyaeva ◽  
Mikhail Ya. Sokol

Author(s):  
Sunuchakan Sanguanmith ◽  
Jintana Meesungnoen ◽  
David A. Guzonas ◽  
Craig R. Stuart ◽  
Jean-Paul Jay-Gerin

The temperature dependence of the rate constant (k) of the bimolecular reaction of two hydrated electrons (eaq−) measured in alkaline water exhibits an abrupt drop between 150°C and 200°C; above 250°C, it is too small to be measured reliably. Although this result is well established, the applicability of this sudden drop in k(eaq−+eaq−)) above ∼150°C to neutral or slightly acidic solution, as recommended by some authors, still remains uncertain. In fact, the recent work suggested that in near-neutral water the abrupt change in k above ∼150°C does not occur and that k should increase, rather than decrease, at temperatures greater than 150°C with roughly the same Arrhenius dependence of the data below 150°C. In view of this uncertainty of k, Monte Carlo simulations were used in this study to examine the sensitivity of the density dependence of the yield of eaq− in the low–linear energy transfer (LET) radiolysis of supercritical water (H2O) at 400°C on variations in the temperature dependence of k. Two different values of the eaq− self-reaction rate constant at 400°C were used: one was based on the temperature dependence of k above 150°C as measured in alkaline water (4.2×108  M−1 s−1), and the other was based on an Arrhenius extrapolation of the values below 150°C (2.5×1011  M−1 s−1). In both cases, the density dependences of our calculated eaq− yields at ∼60  ps and 1 ns were found to compare fairly well with the available picosecond pulse radiolysis experimental data (for D2O) for the entire water density range studied (∼0.15–0.6  g/cm3). Only a small effect of k on the variation of G(eaq−)) as a function of density at 60 ps and 1 ns could be observed. In conclusion, our present calculations did not allow us to unambiguously confirm (or deny) the applicability of the predicted sudden drop of k(eaq−+eaq−) at ∼150°C in near-neutral water.


Fuel ◽  
2013 ◽  
Vol 111 ◽  
pp. 574-583 ◽  
Author(s):  
J. Abelleira ◽  
J. Sánchez-Oneto ◽  
J.R. Portela ◽  
E.J. Martínez de la Ossa

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