Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...

GroMoPo Metadata for Kyushu Island model


Authors:
Owners: This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource.
Type: Resource
Storage: The size of this resource is 1.8 KB
Created: Feb 08, 2023 at 4:51 a.m.
Last updated: Feb 08, 2023 at 4:51 a.m.
Citation: See how to cite this resource
Sharing Status: Public
Views: 577
Downloads: 225
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

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.

Subject Keywords

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°

Content

Additional Metadata

Name Value
DOI 10.1016/j.agwat.2006.03.006
Depth 250
Scale 101 - 1 000 km²
Layers 5
Purpose Groundwater resources;Subsidence;Climate change;Salt water intrusion
GroMoPo_ID 217
IsVerified True
Model Code MODFLOW;SEAWAT
Model Link https://doi.org/10.1016/j.agwat.2006.03.006
Model Time SS
Model Year 2006
Model Authors Don, NC; Hang, NTM; Araki, H; Yamanishi, H; Koga, K
Model Country Japan
Data Available Report/paper only
Developer Email don@ilt.saga-u.ac.jp
Dominant Geology Model focuses on multiple geologic materials
Developer Country Japan
Publication Title Groundwater resources and management for paddy field irrigation and associated environmental problems in an alluvial coastal lowland plain
Original Developer No
Additional Information 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.
Integration or Coupling Water use;Water management
Evaluation or Calibration Static water levels
Geologic Data Availability Yes

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

Comments

There are currently no comments

New Comment

required