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 1.5 KB | |
| Created: | Feb 08, 2023 at 9:33 p.m. | |
| Last updated: | Feb 08, 2023 at 9:33 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
|---|---|
| Views: | 256 |
| Downloads: | 189 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
Abstract
To investigate the relative importance of projected sea-level rise, climate change effects on recharge, and groundwater extraction on seawater intrusion in important coastal aquifers in Atlantic Canada, a three-dimensional numerical model of density-dependent groundwater flow coupled with solute transport was developed for the Richibucto region of New Brunswick. The model was used, with an efficient 2(k) factorial design approach, to perform simulations for the period 2011-2100. The results of the factorial analyses indicate that the relative importance of the three factors investigated varies depending on the model location considered. The effect of declining recharge is most significant at shallow to intermediate depths along the freshwater-seawater transition zone, while the effect of increasing pumping rates dominates at a location relatively close to the well field. The effect of sea-level rise is shown to be significant only at the much deeper inland toe of the transition zone. The spatial variation in importance is related to how different model boundary conditions influence freshwater flow at the different locations within the model domain. This investigation indicates that sea-level rise has the least significant effect (of the three factors considered) on future seawater intrusion in sandstone aquifers in the Richibucto region.
Subject Keywords
Coverage
Spatial
Content
Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.1007/s10040-013-1092-y |
| Depth | 160 |
| Scale | 101 - 1 000 km² |
| Layers | 21 |
| Purpose | Climate change;Salt water intrusion |
| GroMoPo_ID | 451 |
| IsVerified | True |
| Model Code | SEAWAT |
| Model Link | https://doi.org/10.1007/s10040-013-1092-y |
| Model Time | 2011-2100 |
| Model Year | 2014 |
| Model Authors | Green, NR; MacQuarrie, KTB |
| Model Country | Canada |
| Data Available | Report/paper only |
| Developer Email | ktm@unb.ca |
| Dominant Geology | Siliciclastic sedimentary (sandstones, shales) |
| Developer Country | Canada |
| Publication Title | An evaluation of the relative importance of the effects of climate change and groundwater extraction on seawater intrusion in coastal aquifers in Atlantic Canada |
| Original Developer | No |
| Additional Information | |
| Integration or Coupling | Solute transport |
| Evaluation or Calibration | Unsure |
| Geologic Data Availability | No |
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