Geochemical Records of Paleocontamination in Late Pleistocene Lake Sediments in West Flanders (Belgium)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F18%3A00000154" target="_blank" >RIV/00025798:_____/18:00000154 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.tandfonline.com/doi/full/10.1080/04353676.2017.1408955" target="_blank" >https://www.tandfonline.com/doi/full/10.1080/04353676.2017.1408955</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1080/04353676.2017.1408955" target="_blank" >10.1080/04353676.2017.1408955</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Geochemical Records of Paleocontamination in Late Pleistocene Lake Sediments in West Flanders (Belgium)

Popis výsledku v původním jazyce

Concentrations of trace elements in Late Pleistocene lake sediments from two localities in West Flanders (Belgium) were studied using inductively coupled plasma-mass spectrometry. The studied sediments were deposited during the transition of the Allerød to the Younger Dryas. Trace elements enter lake environments from a variety of sources, but mostly from bedrock weathering in catchments and as wind-blown dust particles. These sources create a natural trace element background in lake sediment records. The concentration and distribution of trace elements across the studied lake sediment sequences display features consistent with inputs of materials other than those from soil or bedrock. Input from volcanic eruptions, biomass burning and meteorite impacts should be considered among the main sources of non-anthropogenic contamination of lake environments

Název v anglickém jazyce

Geochemical Records of Paleocontamination in Late Pleistocene Lake Sediments in West Flanders (Belgium)

Popis výsledku anglicky

Concentrations of trace elements in Late Pleistocene lake sediments from two localities in West Flanders (Belgium) were studied using inductively coupled plasma-mass spectrometry. The studied sediments were deposited during the transition of the Allerød to the Younger Dryas. Trace elements enter lake environments from a variety of sources, but mostly from bedrock weathering in catchments and as wind-blown dust particles. These sources create a natural trace element background in lake sediment records. The concentration and distribution of trace elements across the studied lake sediment sequences display features consistent with inputs of materials other than those from soil or bedrock. Input from volcanic eruptions, biomass burning and meteorite impacts should be considered among the main sources of non-anthropogenic contamination of lake environments

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

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OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2018

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geografiska Annaler: Series A-Physical geography

ISSN

0435-3676

e-ISSN

—

Svazek periodika

100

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

SE - Švédské království

Počet stran výsledku

17

Strana od-do

204-220

Kód UT WoS článku

000437337300007

EID výsledku v databázi Scopus

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