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Ammonia evolution from western and eastern oil shales

Conference ·
OSTI ID:6433177
The study of nitrogen (N) species released during oil shale processing is an important research area because both oil shale and shale oil are rich in N. Combustion of N-bearing fuels can produce nitrogen oxides (NO/sub x/). Ammonia is a major N by-product in oil shale processing. The retort water and pyrolysis gases carry 4% and 0.2% of the total N, respectively, and ammonia accounts for most of the N in these product streams. Ammonia also accounts for half of N in the combustion gas stream, and NO/sub x/ for the other half. The concentrations of HCN and molecular nitrogen (N/sub 2/) in the combustion gas stream were not determined, so they were not included in the balance. The total N balance is poor, probably due to species not measured and to the lack of accuracy in determination of the N content in solids. We studied ammonia evolution by pyrolyzing oil shale under a given time-temperature history and measuring the total yield of ammonia by an ammonia electrode. In this paper, we summarize the on-line ammonia evolution rates for two Green River Formation oil shales and one Eastern oil shale under inert gas (argon) and also under steam. We analyze the contribution of the organic/inorganic sources of N to the NH/sub 3/ yield at different pyrolysis temperatures and show oil shale N-chemistry during pyrolysis. We also compare the kinetics of ammonia evolution with that of other pyrolysis gases. 29 refs., 5 figs., 2 tabs.
Research Organization:
Lawrence Livermore National Lab., CA (USA)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
6433177
Report Number(s):
UCRL-99703; CONF-8804239-2; ON: DE89006733
Country of Publication:
United States
Language:
English