Laboratory and theoretical investigation of chemical release experiment Final report, 8 Oct. 1965 - 10 Nov. 1966
Chemical release experiments in upper atmosphere
CHEMILUMINESCENCE↗
Engineering topics
Warneck, P.
Publications and source records attributed to Warneck, P..
Reactions of super 1 D oxygen atoms. III.
Ozone formation in photolysis of oxygen and oxygen-helium mixture as function of pressure and temperature
HELIUM↗
Studies of ion-neutral reactions by a photoionization mass-spectrometer technique. I.
Photoionization mass spectrometer for ion-molecule reaction studies, determining ion residence times, drift velocities, diffusion coefficients and ion temperatures
DIFFUSION COEFFICIENT↗
Studies of ion-neutral reactions by a photoionization mass-spectrometer technique. II.
Photoionization mass spectrometer for charge transfer reaction analysis
PHOTOIONIZATION↗
Ion-molecule reaction rates in an oxygen- nitrogen atmosphere Final report
Photoionization mass spectrometer studies of ion-molecular reactions in oxygen-nitrogen atmosphere, and McLeod gauge measurements of ion source pressures
PHOTOIONIZATION↗
Gas analysis by photo-ionization mass spectrometry.
Photoionization mass spectrometer with 180-degree magnetic analyzer with inclined pole faces, applicability to gas analysis
GAS ANALYZER↗
CO sub 2 actinometer for argon source.
Quantum yield of CO formation from photolysis of carbon dioxide at wavelengths of argon lines
CARBON MONOXIDE↗
Physics of planetary atmospheres. IV - Gas analysis by photoionization mass spectrometry
Photoionization mass spectrometer with 180 deg magnetic analyzer and use as gas analyzer
MAGNETIC INSTRUMENT↗
Chemiluminescent reactions of cs sub 2, cos, and h sub 2 s with atomic oxygen.
Chemiluminescent reactions of carbon disulfide, carbonyl sulfide and hydrogen sulfide with atomic oxygen
CHEMILUMINESCENCE↗
Planetary physics viii- reactions of 1d oxygen atoms in the photolysis of carbon dioxide. ii
Ozone formation in vacuum ultraviolet photolysis of carbon dioxide in closed system
PHOTOLYSIS↗
Planetary Aeronomy: NO2 In the Martian Atmosphere - 2
The transmission curve of the Martian atmosphere derived by Opik is compared with transmission curves of an atmosphere containing various amounts of nitrogen dioxide. It is found that the amount of 6 x l0(exp 18) sq cm column NO2 (or even less) given by Sinton as an upper limit for the Martian NO2 content could adequately explain the phenomenon of the blue haze. This finding made it worthwhile to investigate the effect of the temperature and pressure sensitive equilibrium 2 NO2 reversibly yields N204 upon the total NO2 content and the altitude-number density distributions of NO2 and N204. Computations were carried out for surface temperatures of 273 K, 243 K, 213 K, and 183 K and for three different temperature distributions. The discussion of the results leads to the suggestion of several important new experiments.
Warneck, P.↗
PLANETARY AERONOMY XIV- ULTRAVIOLET ABSORPTION OF SO SUB 2- DISSOCIATION ENERGIES OF SO SUB 2 AND SO
Planetary aeronomy - ultraviolet absorption of sulfur dioxide - dissociation energies of sulfur dioxide and sulfur oxide
ULTRAVIOLET SPECTROSCOPY↗
PLANETARY AERONOMY II- NO SUB 2 IN THE MARTIAN ATMOSPHERE
Planetary aeronomy - nitrogen dioxide in martian atmosphere
AERONOMY↗
PLANETARY ATMOSPHERE STUDIES II- A MICROWAVE POWERED HYDROGEN LAMP FOR VACUUM ULTRAVIOLET PHOTOCHEMISTRY
Instrumentation for planetary atmosphere studies - a microwave hydrogen lamp for vacuum ultraviolet photochemistry
VACUUM↗
PLANETARY ATMOSPHERE STUDIES IV- PHOTOCHEMISTRY OF CARBON-OXYGEN SYSTEMS
Planetary atmosphere studies iv - photochemistry of carbon-oxygen systems
CARBON MONOXIDE↗
PLANETARY ATMOSPHERE STUDIES V- PHOTOCHEMISTRY OF SULFUR-OXYGEN SYSTEMS
Planetary atmosphere studies v - photochemistry of sulfur-oxygen systems
OXYGEN↗