Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
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
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
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment