GroMoPo Metadata for Kyushu Island model


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Created: Feb 08, 2023 at 4:51 a.m.
Last updated: Feb 08, 2023 at 4:51 a.m.
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Abstract

Groundwater is an important resource for water use in the alluvial coastal lowland plain. In the Shiroishi lowland plain, southwestern Kyushu Island of Japan, land subsidence and salinity intrusion due to intense withdrawals of groundwater have become the main environmental issues for public concern. In this study, an integrated surface and groundwater model was established and applied to the Shiroishi site to simulate groundwater flow hydraulics, aquifer compaction and solute transport in the alluvial lowland plain. Moreover, a groundwater optimization model was also formulated to search for an optimal safe yield of groundwater extraction without violating salinity intrusion and other constraints. The simulated results show that groundwater levels in the aquifer greatly vary in response to varying climatic and pumping conditions. Consequently, land subsidence has rapidly occurred throughout the area with the central prone in Shiroishi basin. As a result of pumping and land subsidence, seawater has been intruded along the coast. in case of relative sea level rise, seawater intrusion appears to extend much farther in land from the coast. From the viewpoint of agricultural water management, pumping for irrigation with an optimal pumping amount that is a new finding from the optimization model will sustain groundwater quality in the study area. (c) 2006 Elsevier B.V. All rights reserved.

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Japan
North Latitude
33.3677°
East Longitude
130.3150°
South Latitude
33.1052°
West Longitude
129.9726°
Leaflet Map data © OpenStreetMap contributors

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Additional Metadata

How to Cite

GroMoPo, E. Leijnse (2023). GroMoPo Metadata for Kyushu Island model, HydroShare, http://www.hydroshare.org/resource/492063c0585b468faf6cafe711248f30

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

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

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