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chemical physics of discharges - Argonne National Laboratory

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33<br />

velocity <strong>of</strong> the reacting partn rs is sufficie tl y great. Giese and Maier (60) have<br />

f shown that for the reaction Ar + CO 4 Ar + C + 0, which is endothermic by 6.62<br />

+<br />

and 6.44 e\’ for the 2p state <strong>of</strong> Ar , the threshold for the<br />

“co<br />

Their measured values were in agreement with this relation.<br />

(60) C. F. Giese and W. B. Plaier, J. X m . a. 39, 197 (1963)<br />

(61)<br />

(62)<br />

(63)<br />

React ion<br />

1<br />

112<br />

Table 11<br />

Some Second-Order Rate Constants<br />

10 10 k, cc/molecule sec Reference<br />

D2 -3 D3 + D 14.5 4,11<br />

+<br />

CH4 + CH4 + CH<br />

5+ + m3<br />

10 61,62,63<br />

H20 + H20 --f H30 + OH 12.7 1,2,13<br />

+ +<br />

C H + C H + C H +CH4 14.5 9<br />

2 6 3+5<br />

2+3<br />

+ C H + ~ CH o + n 0.126 22<br />

O2 + 33<br />

CH4 + O2 + CH30 + OH<br />

0.257 22<br />

V. L. Tal’roze and E. L. Frankevich, J. Phys. Chem. USSR 34, 1275 (1960)<br />

C. W. Hand and H. von Weyssenh<strong>of</strong>f, Can. J. Chem., 42, 195, 2385 (1964)<br />

J. L. Franklin, Y.<br />

2353 (1966)<br />

Wada, P. Natalis and P. M. Hierr J. Phys. Chem. 70, -<br />

All reaction rate studies have not been limited to extremely low pressures.<br />

When the pressure in the ion source becomes sufficiently great the reactions follow<br />

the psuedo first order rate laws over rather wide ranges <strong>of</strong> pressure, unless subse-<br />

quent reactions interfere. Thus, Field et al. (51) found the disappearance <strong>of</strong> CH4<br />

in methane to obey first law kinetics over a pressure range <strong>of</strong> about 0.1 to 400 Torr.<br />

However, as the pressure is raised, in certain systems, reactions <strong>of</strong> a higher order<br />

do occur. Field, (37) studying ethylene, has reported some reactions having apparent<br />

orders as high as about 6. These, <strong>of</strong> course, are not truly 6th order reactions, but<br />

simply represent a succession <strong>of</strong> perhaps five secondary reactions which show dependence<br />

upon the 6th power <strong>of</strong> the pressure. Rates <strong>of</strong> reactions <strong>of</strong> such high order do<br />

not yield satisfactory rate constants, but it has been possible to determine rate<br />

constants for reactions <strong>of</strong> 3rd order, and Field and several others have made approximate<br />

measurements <strong>of</strong> the rate constants for such third order processes. As is the<br />

case with the second order processes, these reaction rates are relatively high. For<br />

example, in ethylape eld deter ined several third order rate constants to be<br />

F3 2 -1<br />

in the order <strong>of</strong> molecule- sec .<br />

Although most <strong>of</strong> the measurements <strong>of</strong> rate constants in the literature were<br />

obtained with the source operating in a continuous mode employing a variation in<br />

pressure to establish the rate, some studies have been made in which retention time<br />

in the source was varied.<br />

Such measurements were originally made by Tal’roze and<br />

Frankevitch (61), but subsequent measurements have been made by Hand and von Weissenh<strong>of</strong>f<br />

(62) and Franklin, Natalis, Wada, and Hierl (63). In order to obtain a satisfactory<br />

variation <strong>of</strong> time, a pulsed mode is employed. In such an operation a pulse<br />

<strong>of</strong> electrons is fired through the gas. After it is stopped, the resulting ions<br />

can be retained in the source for a controlled period <strong>of</strong> time and then rapidly<br />

extracted by a pulse <strong>of</strong> high energy. By varying the delay time, the time <strong>of</strong> retention<br />

in the source is varied, and rate constants determined in the manner more usually<br />

employed by chemists in rate studies. Results obtained in this way generally agree<br />

-<br />

I<br />

+

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