Identifying the flow pattern and natural recharge at a strategic groundwater resource in the Dornogobi Province, Mongolia
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F18%3A00103428" target="_blank" >RIV/00216224:14310/18:00103428 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.tandfonline.com/doi/pdf/10.1080/02626667.2018.1511053?needAccess=true" target="_blank" >https://www.tandfonline.com/doi/pdf/10.1080/02626667.2018.1511053?needAccess=true</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1080/02626667.2018.1511053" target="_blank" >10.1080/02626667.2018.1511053</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Identifying the flow pattern and natural recharge at a strategic groundwater resource in the Dornogobi Province, Mongolia
Popis výsledku v původním jazyce
The strategic project of economic development in the Dornogobi Province in Mongolia is dependent on water supply. Thus a comprehensive hydrogeological characterization was focused on the Upper Cretaceous multi aquifer system north of Sainshand City. A conceptual model was developed to discover the groundwater flow pattern essential to correct the setting of the numerical model of groundwater flow created using MODFLOW to assess the natural recharge of the aquifer. The conceptualization was based on geological and hydrogeological characterization. However, especially the evaluation of hydrochemistry proved to be the key factor revealing the principal feature of the groundwater flow pattern, which is the presence of preferential flow zones. These zones allow for intensive transfer of relatively fresh Na(Mg,Ca)/HCO3 dominated groundwater into discharge areas where it leaks into the Quaternary aquifer. The numerical model suggested an enormous natural recharge of 22 100 m3/d, originating in 64% of the preferential flow zones.
Název v anglickém jazyce
Identifying the flow pattern and natural recharge at a strategic groundwater resource in the Dornogobi Province, Mongolia
Popis výsledku anglicky
The strategic project of economic development in the Dornogobi Province in Mongolia is dependent on water supply. Thus a comprehensive hydrogeological characterization was focused on the Upper Cretaceous multi aquifer system north of Sainshand City. A conceptual model was developed to discover the groundwater flow pattern essential to correct the setting of the numerical model of groundwater flow created using MODFLOW to assess the natural recharge of the aquifer. The conceptualization was based on geological and hydrogeological characterization. However, especially the evaluation of hydrochemistry proved to be the key factor revealing the principal feature of the groundwater flow pattern, which is the presence of preferential flow zones. These zones allow for intensive transfer of relatively fresh Na(Mg,Ca)/HCO3 dominated groundwater into discharge areas where it leaks into the Quaternary aquifer. The numerical model suggested an enormous natural recharge of 22 100 m3/d, originating in 64% of the preferential flow zones.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Hydrological Sciences Journal
ISSN
0262-6667
e-ISSN
—
Svazek periodika
63
Číslo periodika v rámci svazku
9
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
16
Strana od-do
1408-1423
Kód UT WoS článku
000451778900008
EID výsledku v databázi Scopus
2-s2.0-85053320022