The mole fraction x2 of (H2)2 in equilibrium mixture with H2 under the atmospheric conditions of Jupiter is evaluated from the dimerization equilibrium constant calculated by quantum-chemical treatments and also from the Lennard-Jones potential. The treatments are of an ab initio type with the ...
oceanographic regions/ atmospherechemical compositionoceanAD 1986 06 to 08partial pressuretropical Atlantic surface seawatermole fractionundersaturatedContinuous monitoring of oceanic and atmospheric CO2 during periods of 8 to 12 days in two particular locations of the tropical Atlantic was carried out during...
What is the volume of 1.40 moles of nitrogen gas at 20.0 degrees C and 770 torr? What is the volume, in L, occupied by 3.260 moles of NO_2 gas at STP conditions? What is the pressure of 1.56 moles of nitrogen gas confined to a volume of 0.260 L at 39 degr...
the mole-rats exhale high levels of carbon dioxide, which becomes acid when it touches skin and mucous tissue in the nose, eyes and mouth. But the mole-rats have evolved to become desensitized to the stinging pain of acid.
The seasonal cycle of CO2 mole fraction is damped with elevation. While the amplitude of the seasonal cycle is 28.5 μmol mol 1 at 10 m above the ground, it is only 10.7 μmol mol 1 in the layer of 2500–3000 m corresponding to the lower free atmosphere above the well-mixed boundary...
Significance of Ci estimated from leaf gas exchange. Plant Physiology . 1998Meyer S, Genty B (1998) Mapping intercellular CO2 mole fraction (Ci) on Rosa rubiginosa leaves fed with abscisic acid by using chloro- phyll fluorescence imaging. Significance of Ci estimated from leaf gas exchange. ...
CO2CO2 Isotopes(CO2)-C-12-O-16(CO2)-C-13-O-16The precision of optically based techniques for long term CO2 monitoring in the atmosphere is approaching the +/- 0.02 mu mol mol(-1 )level, however biases of potentially up to fifteen times greater than this can arise due to differences ...
There is a widely recognized need to improve our understanding of biosphere-atmosphere carbon exchanges in areas of complex terrain including the United States Mountain West. CO2 fluxes over mountainous terrain are often difficult to measure due to unusual and complicated influences associated with ...
The computed dimerization equilibrium constant is combined with observed height profiles of temperature and pressure in the Jupiter atmosphere in order to derive the dimeric mole fraction x2 in the partial thermodynamic equilibrium with the monomer. In all the treatments considered, it is found that ...
This study systematically examines the regional uncertainties and biases in carbon dioxide (CO2) mole fractions from two of the state‐of‐the‐art global CO2 analysis products, namely, the Copernicus Atmosphere Monitoring Service (CAMS) real‐time atmospheric analysis from the European Centre for ...