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USGS · 70189203

Knowledge, transparency, and refutability in groundwater models, an example from the Death Valley regional groundwater flow system

Abstract

This work demonstrates how available knowledge can be used to build more transparent and refutable computer models of groundwater systems. The Death Valley regional groundwater flow system, which surrounds a proposed site for a high level nuclear waste repository of the United States of America, and the Nevada National Security Site (NNSS), where nuclear weapons were tested, is used to explore model adequacy, identify parameters important to (and informed by) observations, and identify existing old and potential new observations important to predictions. Model development is pursued using a set of fundamental questions addressed with carefully designed metrics. Critical methods include using a hydrogeologic model, managing model nonlinearity by designing models that are robust while maintaining realism, using error-based weighting to combine disparate types of data, and identifying important and unimportant parameters and observations and optimizing parameter values with computationally frugal schemes. The frugal schemes employed in this study require relatively few (10–1000 s), parallelizable model runs. This is beneficial because models able to approximate the complex site geology defensibly tend to have high computational cost. The issue of model defensibility is particularly important given the contentious political issues involved.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 35.5° to 38° latitude; -118° to -115° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Mary C. Hill, Claudia C. Faunt, Wayne Belcher, Donald S. Sweetkind, Claire R. Tiedeman, Dmitri Kavetski. 2013. Knowledge, transparency, and refutability in groundwater models, an example from the Death Valley regional groundwater flow system. https://doi.org/10.1016/j.pce.2013.03.006

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Separation, characterization and initial reaction studies of magnetite particles from Hanford sediments

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