Geologic Controls on Hydrology and Groundwater Flow

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Hydrogeology".

Deadline for manuscript submissions: closed (1 June 2022) | Viewed by 2715

Special Issue Editors


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Guest Editor
U.S. Geological Survey DFC, MS 980, Denver, CO 80225, USA
Interests: hydrogeology; 3D framework; stratigraphy; structural geology; subsurface; aquifers
Special Issues, Collections and Topics in MDPI journals

E-Mail Website
Guest Editor
U.S. Geological Survey DFC, MS 980, Denver, CO 80225, USA
Interests: hydrogeology; 3D framework; aquifer properties; numerical modeling

Special Issue Information

Dear Colleagues,

Management of surface-water and groundwater resources requires knowledge of the groundwater system, which in turn requires an understanding of the configuration and properties of aquifers. Surface and subsurface geology can influence the hydrologic system and groundwater flow in numerous ways, including influencing the relative amounts of net infiltration, forming the subsurface architecture of aquifer and confining units, and faults that may either impede or focus flow. Geologic information can be considered during basin conceptualization, be used to construct digital 3D framework models, or be added during calibration of the numerical model.  This issue seeks to bring together hydrologists, geologists, and 3D framework and numerical modelers who create or use geologic data or 3D geologic framework models to inform regional groundwater models or resource assessments. Topics of interest include development and integration of geologic and hydrologic data, integration of geologic data and 3D geologic frameworks into groundwater models, hydrology and modeling studies that provide evidence for geologic controls on hydrology, and future avenues for advancing the use of geologic data in hydrologic studies. We aim for submissions that demonstrate novel approaches and case studies that integrate geologic and hydrologic data.

Dr. Donald Sweetkind
Prof. Dr. Geoffrey Cromwell
Guest Editors

Manuscript Submission Information

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Keywords

  • hydrogeology
  • aquifer properties
  • 3D framework
  • conceptual models
  • aquitards
  • numerical model

Published Papers (1 paper)

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Research

21 pages, 9198 KiB  
Article
Hydrogeological Survey, Radiometric Analysis and Field Parametric Measurements: A Combined Tool for the Study of Porous Aquifers
by Enzo Cuiuli and Salvatore Procopio
Water 2022, 14(14), 2173; https://doi.org/10.3390/w14142173 - 09 Jul 2022
Viewed by 2071
Abstract
The use of isotopic geochemistry for hydrogeological studies is growing internationally. The use of isotopic geochemistry methodologies on hydrogeological survey data, integrated with the use natural tracers, is helpful when defining the hydrogeological model of the aquifer. In particular, the use of radioisotope [...] Read more.
The use of isotopic geochemistry for hydrogeological studies is growing internationally. The use of isotopic geochemistry methodologies on hydrogeological survey data, integrated with the use natural tracers, is helpful when defining the hydrogeological model of the aquifer. In particular, the use of radioisotope concentration measurements as natural tracers and the detection of the temperature, redox potential and dissolved oxygen in groundwater in the field provide information on underground water circulation, which is useful for identifying recharge areas and groundwater drainage. Variations in these parameters in the aquifer allow for information about its hydrodynamics to be obtained. The application of this method in a sample area showed how the uranium and radon concentrations, temperature, redox potential and dissolved oxygen vary in the different sectors of the aquifer, depending on water mobility. This information, integrated with the results of a hydrogeological survey of the static levels, distinguished the recharge and drainage areas of the aquifer and the preferential directions in terms of water flow and allowed for information on the mobility of the aquifer in the various sectors to be obtained. The method presented in this paper was tested in a larger hydrogeological study in the southern sector of the shallow aquifer of the S. Eufemia Lamezia plain (Calabria, Italy). Full article
(This article belongs to the Special Issue Geologic Controls on Hydrology and Groundwater Flow)
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