TY - JOUR
T1 - Estimating the thickness of unconsolidated coastal aquifers along the global coastline
AU - Zamrsky, D.
AU - Oude Essink, G.H.P.
AU - Bierkens, M.F.P.
PY - 2018/9/3
Y1 - 2018/9/3
N2 - Knowledge of aquifer thickness is crucial for setting up numerical groundwater flow models to sup-port groundwater resource management and control. Fresh groundwater reserves in coastal aquifers are particularly under threat of salinization and depletion as a result of climate change, sea-level rise, and excessive groundwater withdrawal under urbanization. To correctly assess the possible impacts of these pressures we need better information about subsurface conditions in coastal zones. Here, we propose a method that combines available global datasets to estimate, along the global coastline, the aquifer thickness in areas formed by unconsolidated sediments. To validate our final estimation results, we collected both borehole and literature data. Additionally, we performed a numerical modelling study to evaluate the effects of varying aquifer thickness and geological complexity on simulated saltwater intrusion. The results show that our aquifer thickness estimates can indeed be used for regional-scale groundwater flow modelling but that for local assessments additional geological information should be included. The final dataset has been made publicly available (https://doi.pangaea.de/10.1594/PANGAEA.880771)
AB - Knowledge of aquifer thickness is crucial for setting up numerical groundwater flow models to sup-port groundwater resource management and control. Fresh groundwater reserves in coastal aquifers are particularly under threat of salinization and depletion as a result of climate change, sea-level rise, and excessive groundwater withdrawal under urbanization. To correctly assess the possible impacts of these pressures we need better information about subsurface conditions in coastal zones. Here, we propose a method that combines available global datasets to estimate, along the global coastline, the aquifer thickness in areas formed by unconsolidated sediments. To validate our final estimation results, we collected both borehole and literature data. Additionally, we performed a numerical modelling study to evaluate the effects of varying aquifer thickness and geological complexity on simulated saltwater intrusion. The results show that our aquifer thickness estimates can indeed be used for regional-scale groundwater flow modelling but that for local assessments additional geological information should be included. The final dataset has been made publicly available (https://doi.pangaea.de/10.1594/PANGAEA.880771)
U2 - 10.5194/essd-10-1591-2018
DO - 10.5194/essd-10-1591-2018
M3 - Article
SN - 1866-3508
VL - 10
SP - 1591
EP - 1603
JO - Earth System Science Data
JF - Earth System Science Data
ER -