2005
Formation of nitrate and sulfate in the plume of Berlin
LAMMEL, Gerhard a Adrian LEIPZákladní údaje
Originální název
Formation of nitrate and sulfate in the plume of Berlin
Název česky
Formation of nitrate and sulfate in the plume of Berlin
Autoři
LAMMEL, Gerhard a Adrian LEIP
Vydání
Environmental Science and Pollution Research, Heidelberg, Springer, 2005, 0944-1344
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10511 Environmental sciences
Stát vydavatele
Německo
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 1.518
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/05:00039046
Organizační jednotka
Přírodovědecká fakulta
UT WoS
Klíčová slova česky
Atmospheric chemistry; nitrate; particulate matter; secondary inorganic aerosol; sulphur dioxide oxidation; urban plume
Klíčová slova anglicky
Atmospheric chemistry; nitrate; particulate matter; secondary inorganic aerosol; sulphur dioxide oxidation; urban plume
Změněno: 23. 2. 2010 17:41, prof. Gerhard Lammel, PhD.
V originále
The near-ground aerosol chemical composition was studied at two stationary sites in the vicinity of Berlin during a field campaign in the summer of 1998. By means of analysis of the wind field, two episodes were identified which allow one to study changes within individual air masses during transport, i.e. a Lagrangian type of experiment, with one station being upwind and the other downwind of the city. N(V) and S(VI), was formed from emissions in the city within a few hours.
Česky
The near-ground aerosol chemical composition was studied at two stationary sites in the vicinity of Berlin during a field campaign in the summer of 1998. By means of analysis of the wind field, two episodes were identified which allow one to study changes within individual air masses during transport, i.e. a Lagrangian type of experiment, with one station being upwind and the other downwind of the city. N(V) and S(VI), was formed from emissions in the city within a few hours.
Návaznosti
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