Details
Original language | English |
---|---|
Pages (from-to) | 648-659 |
Number of pages | 12 |
Journal | Journal of hydrology |
Volume | 551 |
Publication status | Published - 3 Mar 2017 |
Abstract
Application of numerical models is a common method to assess groundwater resources. The versatility of these models allows consideration of different levels of complexity, but the accuracy of the outcomes hinges upon a proper description of the system behaviour. In seawater intrusion assessment, the implementation of the sea-side boundary condition is of particular importance. We evaluate the influence of the slope of the sea-side boundary on the simulation results of seawater intrusion in a freshwater aquifer by employing a series of slope variations together with a sensitivity analysis by varying additional sensitive parameters (freshwater inflow and longitudinal and transverse dispersivities). Model results reveal a multi-dimensional dependence of the investigated variables with an increasing relevance of the sea-side boundary slope for seawater intrusion (decrease of up to 32%), submarine groundwater discharge zone (reduction of up to 55%), and turnover times (increase of up to 730%) with increasing freshwater inflow or dispersivity values.
Keywords
- Coastal aquifers, Numerical investigation, OpenGeoSys, Residence times, Saltwater intrusion, Sea-side boundary condition, Submarine groundwater discharge
ASJC Scopus subject areas
- Environmental Science(all)
- Water Science and Technology
Sustainable Development Goals
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In: Journal of hydrology, Vol. 551, 03.03.2017, p. 648-659.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - How significant is the slope of the sea-side boundary for modelling seawater intrusion in coastal aquifers?
AU - Graf, Thomas
AU - Kolditz, Olaf
AU - Liedl, Rudolf
AU - Post, Vincent
AU - Walther, Manfred
N1 - Publisher Copyright: © 2017 Elsevier B.V. Copyright: Copyright 2017 Elsevier B.V., All rights reserved.
PY - 2017/3/3
Y1 - 2017/3/3
N2 - Application of numerical models is a common method to assess groundwater resources. The versatility of these models allows consideration of different levels of complexity, but the accuracy of the outcomes hinges upon a proper description of the system behaviour. In seawater intrusion assessment, the implementation of the sea-side boundary condition is of particular importance. We evaluate the influence of the slope of the sea-side boundary on the simulation results of seawater intrusion in a freshwater aquifer by employing a series of slope variations together with a sensitivity analysis by varying additional sensitive parameters (freshwater inflow and longitudinal and transverse dispersivities). Model results reveal a multi-dimensional dependence of the investigated variables with an increasing relevance of the sea-side boundary slope for seawater intrusion (decrease of up to 32%), submarine groundwater discharge zone (reduction of up to 55%), and turnover times (increase of up to 730%) with increasing freshwater inflow or dispersivity values.
AB - Application of numerical models is a common method to assess groundwater resources. The versatility of these models allows consideration of different levels of complexity, but the accuracy of the outcomes hinges upon a proper description of the system behaviour. In seawater intrusion assessment, the implementation of the sea-side boundary condition is of particular importance. We evaluate the influence of the slope of the sea-side boundary on the simulation results of seawater intrusion in a freshwater aquifer by employing a series of slope variations together with a sensitivity analysis by varying additional sensitive parameters (freshwater inflow and longitudinal and transverse dispersivities). Model results reveal a multi-dimensional dependence of the investigated variables with an increasing relevance of the sea-side boundary slope for seawater intrusion (decrease of up to 32%), submarine groundwater discharge zone (reduction of up to 55%), and turnover times (increase of up to 730%) with increasing freshwater inflow or dispersivity values.
KW - Coastal aquifers
KW - Numerical investigation
KW - OpenGeoSys
KW - Residence times
KW - Saltwater intrusion
KW - Sea-side boundary condition
KW - Submarine groundwater discharge
UR - http://www.scopus.com/inward/record.url?scp=85017554150&partnerID=8YFLogxK
U2 - 10.1016/j.jhydrol.2017.02.031
DO - 10.1016/j.jhydrol.2017.02.031
M3 - Article
AN - SCOPUS:85017554150
VL - 551
SP - 648
EP - 659
JO - Journal of hydrology
JF - Journal of hydrology
SN - 0022-1694
ER -