GroMoPo Metadata for Pingtung Coastal Aquifer model


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Created: Feb 06, 2023 at 9:02 p.m.
Last updated: Feb 06, 2023 at 9:02 p.m.
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Abstract

A three-dimensional variable-density finite element model was developed to study the combined effects of overabstraction and seawater intrusion in the Pingtung Plain coastal aquifer system in Taiwan. The model was generated in different layers to represent the three aquifers and two aquitards. Twenty-five multilayer pumping wells were assigned to abstract the groundwater, in addition to 95 observation wells to monitor the groundwater level. The analysis was carried out for a period of 8 years (2008-2015 inclusive). Hydraulic head, soil permeability, and precipitation were assigned as input data together with the pumping records in different layers of the aquifer. The developed numerical model was calibrated against the observed head archives and the calibrated model was used to predict the inland encroachment of seawater in different layers of the aquifer. The effects of pumping rate, sea-level rise, and relocation of wells on seawater intrusion were examined. The results show that all layers of the aquifer system are affected by seawater intrusion; however, the lengths of inland encroachment in the top and bottom aquifers are greater compared with the middle layer. This is the first large-scale finite-element model of the Pingtung Plain, which can be used by decision-makers for sustainable management of groundwater resources and cognizance of seawater intrusion in coastal aquifers.

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Taiwan
North Latitude
22.9000°
East Longitude
120.6000°
South Latitude
22.3000°
West Longitude
120.3000°
Leaflet Map data © OpenStreetMap contributors

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How to Cite

GroMoPo, D. Zamrsky (2023). GroMoPo Metadata for Pingtung Coastal Aquifer model, HydroShare, http://www.hydroshare.org/resource/10e2d8cc55b44a98a082241c71a113ac

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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