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  • Composition of the soil gas phase. Permanent gases and hydrocarbons
  • The emission of gaseous hydrocarbons (CH4, C2H4, C2H5 and C3H8) and the permanent gases, O2 and CO2 from soils, has been measured during several weeks. Therefore, eighteen soil samples from different regions in Belgium were selected. The gas samples
  • Liquified energy gases in the UK: what price public safety?
  • Magmatic gases extracted and analysed from ocean floor volcanics
  • Simulation of the effects of CO and other trace gases in the atmosphere on climate and the environment
  • C/C and S/S ratios in magmatic gases from ridge volcanism in Afar
  • Measurements of concentration of the trace gases active in the greenhouse effect
  • In this paper the gas chromatograph for the tropospheric measurements of the trace gases active in the greenhouse effect and the ozone layer destruction are described. For the measurements of the CO, CH4 and CO2 an automatic gas chromatograph
  • Biomass burning as a source of atmospheric gases CO, H, NO, NO, CHCl and COS
  • Biomass burning can contribute extensively to the budgets of several gases which are important in atmospheric chemistry. In several cases the emission is comparable to the technological source. Most burning takes place in the tropics in the dry
  • Human activities in creating and controlling emissions of the most important greenhouse gase
  • Hydrometeorological changes due to increasing atmospheric CO2 and associated trace gases
  • Isotopic identification of gases of a deep origin in French thermomineral waters in Hydrogeothermal studies. 26th International geological congress.
  • On the damage caused by volcanic eruptions with special reference to tephra and gases in Volcanic activity and human ecology.
  • Atmospheric transport of aerosols and trace gases over southern Africa
  • In this paper, the recent research will be reviewed. An assessment will be made of the tropospheric thermodynamic structure and atmospheric transport fields that govern the large-scale horizontal and vertical regional transfer of air, trace gases
  • Interactions between the Earth's surface, atmospheric greenhouse gases and clouds
  • This review traces the theory as far back as 1827, highlighting new directions and significant advances over that time. Four main themes can be discerned : 1) certain radiatively active gases are responsible for warming the planet| 2) that humans
  • can inadvertently influence this warming| 3) climate models are designed to permit prediction of the climatic changes in the atmospheric loadings of these gases but they have not yet achieved this goal of prediction| and 4) many scenarios of changes
  • Effect of gases, aerosols and clouds on the atmospheric absorption of solar radiation
  • C 14 dating of trapped gases in massive ground ice, Western Canadian Arctic
  • Assessment of the importance of forests in reducing global climatic change (counteracting and mitigating the impacts of greenhouse gases)
  • Modelling the distal impacts of past volcanic gas emissions. Evidence of Europe-wide environmental impacts from gases emitted during the eruption of Italian and Icelandic volcanoes in 1783
  • A 30,000 yr continental paleotemperature record derived from noble gases dissolved in groundwater from the San Juan Basin, New Mexico
  • Tranfer of SO and other reactive gases across the air-sea interface