Insights into palaeorecharge conditions for European deep aquifers

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F11%3A10107743" target="_blank" >RIV/00216208:11310/11:10107743 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00020711:_____/11:00003326

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s10040-011-0765-7" target="_blank" >http://dx.doi.org/10.1007/s10040-011-0765-7</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10040-011-0765-7" target="_blank" >10.1007/s10040-011-0765-7</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Insights into palaeorecharge conditions for European deep aquifers

Popis výsledku v původním jazyce

Climatic instability during the late Pleistocene has been reflected in the pattern of groundwater recharge. This report summarizes palaeoclimate knowledge during the late Weichselian in Europe. During this period the majority of northern Europe was covered by thick ice sheets and permafrost, preventing aquifers from recharging. In contrast, southern Europe was generally free of these palaeoclimatic features. Palaeoclimatic information has been combined with isotope data to better understand the palaeorecharge conditions and recharge timing across the European continent. The (18)O and (2)H relationship shows latitudinal plus climatic influences. Radiocarbon data show that while southern European aquifers have generally been recharged continuously duringthe last 40,000 years, northern European aquifers typically show a recharge gap during the Last Glacial Maximum. Areas that underwent continuous recharge during the entire late Pleistocene period can also be distinguished from areas wher

Název v anglickém jazyce

Insights into palaeorecharge conditions for European deep aquifers

Popis výsledku anglicky

Climatic instability during the late Pleistocene has been reflected in the pattern of groundwater recharge. This report summarizes palaeoclimate knowledge during the late Weichselian in Europe. During this period the majority of northern Europe was covered by thick ice sheets and permafrost, preventing aquifers from recharging. In contrast, southern Europe was generally free of these palaeoclimatic features. Palaeoclimatic information has been combined with isotope data to better understand the palaeorecharge conditions and recharge timing across the European continent. The (18)O and (2)H relationship shows latitudinal plus climatic influences. Radiocarbon data show that while southern European aquifers have generally been recharged continuously duringthe last 40,000 years, northern European aquifers typically show a recharge gap during the Last Glacial Maximum. Areas that underwent continuous recharge during the entire late Pleistocene period can also be distinguished from areas wher

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F07%2F0691" target="_blank" >GA205/07/0691: Geotermální zdroje, jejich limity a trvale udržitelné využití: benešovsko-ústecký zvodněný systém</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

Hydrogeology Journal

ISSN

1431-2174

e-ISSN

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Svazek periodika

19

Číslo periodika v rámci svazku

8

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

18

Strana od-do

1545-1562

Kód UT WoS článku

000297197600007

EID výsledku v databázi Scopus

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