Author: Hans OeschgerPublisher:
ISBN:
Category : Ice
Languages : en
Pages : 452
Book Description
Isotopes Et Impuretés Dans Les Neiges Et Glaces
Author: Hans OeschgerIsotopes Et Impuretes Dans Les Neiges Et Glaces
Author: Isotopes et Impuretés dans les Neiges et Glaces
Author: Isotopes and Impurities in Snow and Ice
Author: ISOTOPES AND IMPURITIES IN SNOW AND ICE. SYMPOSIUM. ISOTOPES ET IMPURETES DANS LES NEIGES ET GLACES. PROCEEDINGS OF THE GRENOBLE SYMPOSIUM, AUGUST/SEPTEMBER 1975. ACTES DU COLLOQUE DE GRENOBLE, AOUT/SEPTEMBER 1975
Author: The Journal of Glaciology
Author: Arctic Ocean
Author: Louis ReyPublisher: Springer
ISBN: 1349059196
Category : Science
Languages : en
Pages : 430
Book Description
Proceedings of conference held in March 1980, at the Royal Geographical Society to examine the effect of pollutants from Europe, America and Asia on the Arctic Ocean environment.
IAHS-AISH Publication
Author: International Association of Hydrological SciencesPublisher:
ISBN:
Category : Hydrology
Languages : en
Pages : 616
Book Description
U.S. Geological Survey Water-supply Paper
Author: Chemistry of Multiphase Atmospheric Systems
Author: Wolfgang JaeschkePublisher: Springer Science & Business Media
ISBN: 3642706274
Category : Science
Languages : en
Pages : 773
Book Description
Rapidly increasing interest in the problems of air pollution and source-receptor relationships has led to a significant expansion of knowledge in the field of atmospheric chemistry. In general the chemistry of atmospheric trace constituents is governed by the oxygen content of the atmosphere. Upon entering the atmosphere in a more or less reduced state, trace substances are oxidized via various pathways and the generated products are often precursors of acidic compounds. Beside oxidation processes occurring in the gas phase, gaseous compounds are often converted into solid aerosol particles. The various steps within gas-to-particle conversion are constantly interacting with condensation processes, which are caused by the tropospheric water content. Thus in addition to the gaseous state, a liquid and solid state exists within the troposphere. The solid phase consists of atmospheric conversion products or fly ash and mineral dust. The liquid phase consists of water, conversion products and soluble compounds. The chemistry occurring within this system is often referred to as hydrogeneous chemistry. The chemist interprets this term, however, more strictly as reactions which occur only at an interphase between phases. This, however, is not always what happens in the atmosphere. There are indeed heterogeneous processes such as reactions occurring on the surface of dry aerosol particles. But apart from these, we must focus as well on reactions in the homogeneous phase, which are single steps of consecutive reactions running through various phases.