scholarly journals Hydrogeologic settings and groundwater-flow simulations for regional investigations of the transport of anthropogenic and natural contaminants to public-supply wells—Investigations begun in 2004

2011 ◽  
pp. i-A-8 ◽  
Author(s):  
Sandra M. Eberts
Keyword(s):  
Groundwater Flow ◽  
Flow Simulations ◽  
Public Supply

scholarly journals Generation of 3D Spatially Variable Anisotropy for Groundwater Flow Simulations

Ground Water ◽  
2015 ◽  
Vol 53 (6) ◽  
pp. 955-958 ◽  
Author(s):  
Andrea Borghi ◽  
Philippe Renard ◽  
Gabriel Courrioux
Keyword(s):  
Groundwater Flow ◽  
Flow Simulations ◽  
Variable Anisotropy

scholarly journals Simulations of groundwater flow and particle-tracking analysis in the zone of contribution to a public-supply well in San Antonio, Texas

2011 ◽  
Author(s):  
Richard L. Lindgren ◽  
Natalie A. Houston ◽  
MaryLynn Musgrove ◽  
Lynne S. Fahlquist ◽  
Leon J. Kauffman
Keyword(s):  
Groundwater Flow ◽  
Particle Tracking ◽  
San Antonio ◽  
Public Supply

scholarly journals Groundwater flow modelling of main groundwater reservoirs in the Gdańsk region, Poland

Geologos ◽  
2018 ◽  
Vol 24 (3) ◽  
pp. 217-224
Author(s):  
Zbigniew Kordalski ◽  
Andrzej Sadurski
Keyword(s):  
Groundwater Flow ◽  
Groundwater Resources ◽  
Border Region ◽  
Flow Simulations ◽  
Delta Plain ◽  
Flow Modelling ◽  
Vistula River ◽  
Groundwater Flow Modelling ◽  
Groundwater Reservoir ◽  
The City

Abstract During the last nine years, the 133 main groundwater reservoirs in Poland (MGR) have been documented; these were published last year. Some of these are situated in the coastal zone of the southern Baltic Sea. MGR numbers 111 and 112 are in the Gdańsk area and are discussed in the present paper. The study area is situated on the border region of the moraine plateau of the Cashubian Lakeland, the western part of the Vistula River delta plain and the Bay of Gdańsk. The area of the main groundwater reservoir in no. 112 is developed in Quaternary strata and referred to as Żuławy Gdańskie; it comprises predominantly the city of Gdańsk and slightly exceeds 100 km2. There is also a Cretaceous aquifer, rich in groundwater resources, which is named MGR no. 111, beneath the Quaternary reservoir mentioned above. The area studied and modelled totalled 364 km2, on account of the hydraulic connection between these aquifers. Methods of hydrogeological research, groundwater flow simulations, resources calculation are outlined in the present paper.

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