Biogeochemical cycles of chlorine in the coniferous forest ecosystem: practical implications

0350302 - ÚEB 2011 RIV CZ eng J - Článek v odborném periodiku
Matucha, Miroslav - Clarke, N. - Lachmanová, Z. - Forczek, Sándor - Fuksová, Květa - Gryndler, Milan
Biogeochemical cycles of chlorine in the coniferous forest ecosystem: practical implications.
Plant, Soil and Environment. Roč. 56, č. 8 (2010), s. 357-367. ISSN 1214-1178. E-ISSN 1805-9368
Grant CEP: GA MŠMT 7F09026
Výzkumný záměr: CEZ:AV0Z50380511; CEZ:AV0Z50200510
Klíčová slova: chlorine cycle * chlorination * enzymatic
Kód oboru RIV: GK - Lesnictví
Impakt faktor: 1.076, rok: 2010
www.agriculturejournals.cz/publishedArticle?journal=PSE&volume=56&firstPage=357

Chlorine - one of the most widespread elements on the Earth - is present in the environment as chloride ion or bound to organic substances. The main source of chloride ions is the oceans while organically bound chlorine (OCl) comes from various sources, including anthropogenic ones. Chlorinated organic compounds were long considered to be only industrial products; nevertheless, organochlorines occur plentifully in natural ecosystems. However, recent investigations in temperate and boreal forest ecosystems have shown them to be products of biodegradation of soil organic matter under participation of chlorine. It is important to understand both the inorganic and organic biogeochemical cycling of chlorine in order to understand processes in the forest ecosystem and dangers as a result of human activities, i.e. emission and deposition of anthropogenic chlorinated compounds as well as those from natural processes.
Trvalý link: http://hdl.handle.net/11104/0190337