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chemical physics of discharges - Argonne National Laboratory

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about half the dlamcter <strong>of</strong> the jet (one fourth 345 the area) and that the nitrogen flowing /<br />

outside this core carries negligible enthalp . In this calculation is the unproven<br />

assumption carried over from the argon jet(9 J that the mass flux <strong>of</strong> nitrogen is constant (<br />

over the entire cross-section. Under the assumed core conditions the Set is 100%<br />

disssociated and the atoms 17% ianized. Tfie fluxes are then:<br />

atom flow: 1/4 X 2 X (1 - 0.17) X 0.0171 = 0.0071 moles sec-1<br />

ion flov: 1/b X 2 X 0.17 X 0.0171 = 0.00145 moles sec-1<br />

I<br />

The ion flw is thus seen to be in excellent agresment vith the 0.00171 moles sec-1<br />

production rate <strong>of</strong> HCN. To some extent this may be due to a fortunate choice <strong>of</strong> hot<br />

core temperature but is nevertheless a promising possibility.<br />

On the other hand there seems to be no good way to account for the reaction on the<br />

basis <strong>of</strong> nitrogen atoms, in this case present in large excess, suggesting that the<br />

nitrogen atoms are somehow deactivated before the carbonaceous species enters the hot<br />

core. Ins<strong>of</strong>ar M the hydrogen from the dissociation <strong>of</strong> methane must completely flll<br />

the reactor in a very short vhile, it seems probable that tha nitrogen at- u e<br />

deactivated fram this initial inmion, and that the carbonaceous species reacWwith<br />

the nitrogen ions (vhich might well be molecular ions by this time) or aome other<br />

species sometime later.<br />

CONCLUSION<br />

By systematic variation <strong>of</strong> 'reactor geometry it has been conclusively demonstrated<br />

that methane added through a peripheral slot to a nitrogen jet titrates, apparently<br />

in the true meaning <strong>of</strong> the word, some potential <strong>of</strong> the nitrogen Jet to react with the<br />

thermal decomposition products <strong>of</strong> methane to form HCN. It is further demonstrated<br />

that the potential to react is simply related to heat flow even far down the reactor<br />

and is therefore probably the consequence <strong>of</strong> some steady-state temperature and/or<br />

composition pr<strong>of</strong>lle in a flw with local thermal equilibrium.<br />

For their heuristic value, tvo superficially different explanations are proposed to<br />

explain the "potential to react." On the one hand, the experimental endotherm <strong>of</strong> the<br />

reaction at the equivalence point is ehom to be quite consistent vith the heat flov-<br />

ing in the hot core <strong>of</strong> the jet, for a jet model consistent with vhat ve light expect.<br />

On the other hand, for the same heat flov and jet model, the yield is shown to be con-<br />

sistent vfth the flw rate <strong>of</strong> e.g., ions at the point <strong>of</strong> mixing and it may equilly<br />

well be postulated that the ions or some other identifiable species are in fact an<br />

active ingredient being titrated.<br />

It is clearly pointless to attempt to conjecture further on t he mechanism invol-d<br />

in the titration vithout more direct evidence on the species and relocity pr<strong>of</strong>llee in<br />

the jet. A spectroscopic program currently undenqy in there laboratories dl1 pre-<br />

sumably help to flll this gap.<br />

Acknowledgement<br />

Usnp people have contributed in nome vay to the success <strong>of</strong> this work, but in pu-<br />

ticular the author wishes to express his appreciation to Mr. Charles Mentzer<br />

(Chemical Engineering Department, Princeton University) who helped perform some <strong>of</strong> the<br />

experiments , and to Pr<strong>of</strong>essor Hugh Hulburt (Chemical Engineering Department, Iorthvesfern '<br />

UnivCmity) and Dr. B~rrg R. Bronfln (United Nrcraf't <strong>Laboratory</strong>) for their invaluable<br />

di8cunsions and continuing Interest.<br />

1<br />

I<br />

I

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