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Created: | Feb 08, 2023 at 3:38 p.m. | |
Last updated: | Feb 08, 2023 at 3:38 p.m. | |
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Sharing Status: | Public |
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Abstract
This paper presents a study of solute transport through ground water in the saturated zone and the resulting breakthrough curves (BTCs), using a field-scale numerical model that incorporates the processes of advection, dispersion, matrix diffusion in fractured volcanic formations, sorption, and colloid-facilitated transport. Such BTCs at compliance boundaries are often used as performance measures for a site. The example considered here is that of the saturated zone study prepared for the Yucca Mountain license application. The saturated zone at this site occurs partly in volcanic, fractured rock formations and partly in alluvial formations. This paper presents a description of the site and the ground water flow model, the development of the conceptual model of transport, model uncertainties, model validation, and the influence of uncertainty in input parameters on the downstream BTCs at the Yucca Mountain site. (c) 2010 Elsevier By. All rights reserved.
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Additional Metadata
Name | Value |
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DOI | 10.1016/j.jconhyd.2010.05.003 |
Depth | 6000 |
Scale | 101 - 1 000 km² |
Layers | |
Purpose | Groundwater contamination |
GroMoPo_ID | 318 |
IsVerified | True |
Model Code | FEHM |
Model Link | https://doi.org/10.1016/j.jconhyd.2010.05.003 |
Model Time | 10^6 years |
Model Year | 2010 |
Model Authors | Kelkar, S; Ding, M; Chu, S; Robinson, BA; Arnold, B; Meijer, A; Eddebbarh, AA |
Model Country | United States |
Data Available | Report/paper only |
Developer Email | kelkar@lanl.gov |
Dominant Geology | Model focuses on multiple geologic materials |
Developer Country | USA |
Publication Title | Modeling solute transport through saturated zone ground water at 10 km scale: Example from the Yucca Mountain license application |
Original Developer | No |
Additional Information | |
Integration or Coupling | Solute transport |
Evaluation or Calibration | Static water levels |
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/
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