Mechanisms, timing, and rates of arid region mountain front recharge

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F12%3A10127052" target="_blank" >RIV/00216208:11310/12:10127052 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.jhydrol.2011.12.043" target="_blank" >http://dx.doi.org/10.1016/j.jhydrol.2011.12.043</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.jhydrol.2011.12.043" target="_blank" >10.1016/j.jhydrol.2011.12.043</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mechanisms, timing, and rates of arid region mountain front recharge

Popis výsledku v původním jazyce

Arid region mountain front recharge (MFR) for two catchments (17.5 and 25.6 km(2)) in the Silver Island Mountains, Utah, USA was evaluated by an analysis of catchment precipitation, mountain front and playa infiltration rates, aquifer parameters, and groundwater level responses in 59 shallow monitoring wells located at the distal end of the catchments. The 3-7 km long mountain front surfaces transition from alluvial fan deposits to a thin alluvial covering on lacustrine pediment surfaces. Precipitationand groundwater level data were collected from October 2005 to October 2010, which represents five recharge cycles. Average annual precipitation for all rain gauges during the 2005-2010 water years was 14.9 cm. Monitoring well water levels increased 91-97% of the time in response to storm events during times of general monitoring well water level increases and 29-38% of the time during times of general monitoring well water level declines. A surprising 81.7% of total catchment precipitat

Název v anglickém jazyce

Mechanisms, timing, and rates of arid region mountain front recharge

Popis výsledku anglicky

Arid region mountain front recharge (MFR) for two catchments (17.5 and 25.6 km(2)) in the Silver Island Mountains, Utah, USA was evaluated by an analysis of catchment precipitation, mountain front and playa infiltration rates, aquifer parameters, and groundwater level responses in 59 shallow monitoring wells located at the distal end of the catchments. The 3-7 km long mountain front surfaces transition from alluvial fan deposits to a thin alluvial covering on lacustrine pediment surfaces. Precipitationand groundwater level data were collected from October 2005 to October 2010, which represents five recharge cycles. Average annual precipitation for all rain gauges during the 2005-2010 water years was 14.9 cm. Monitoring well water levels increased 91-97% of the time in response to storm events during times of general monitoring well water level increases and 29-38% of the time during times of general monitoring well water level declines. A surprising 81.7% of total catchment precipitat

Druh

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

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Journal of Hydrology

ISSN

0022-1694

e-ISSN

—

Svazek periodika

428

Číslo periodika v rámci svazku

March

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

17

Strana od-do

15-31

Kód UT WoS článku

000302503100002

EID výsledku v databázi Scopus

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