Item talk:Q274163
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Predicting regional fluoride concentrations at public and domestic supply depths in basin-fill aquifers of the western United States using a random forest model", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70225701", "url": "https://pubs.usgs.gov/publication/70225701" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70225701 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1016/j.scitotenv.2021.150960", "url": "https://doi.org/10.1016/j.scitotenv.2021.150960" } ], "journal": { "@type": "Periodical", "name": "Science of the Total Environment", "volumeNumber": "806", "issueNumber": "4" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Science of the Total Environment" } ], "datePublished": "2022", "dateModified": "2021-12-10", "abstract": "A random forest regression (RFR) model was applied to over 12,000 wells with measured fluoride (F) concentrations in untreated groundwater to predict F concentrations at depths used for domestic and public supply in basin-fill aquifers of the western United States. The model relied on twenty-two regional-scale environmental and surficial predictor variables selected to represent factors known to control F concentrations in groundwater. The testing model fit R2\u00a0and RMSE were 0.52 and 0.78\u00a0mg/L. Comparisons of measured to predicted proportions of four F-concentrations categories (<0.7\u00a0mg/L, 0.7\u20132\u00a0mg/L, >2\u00a0mg/L \u2013 4\u00a0mg/L, and\u00a0>\u00a04\u00a0mg/L) indicate that the model performed well at making regional-scale predictions. Differences between measured and predicted proportions indicate underprediction of measured F at values by between 4 and 20\u00a0mg/L, representing less than 1% of the regional scale predicted values. These residuals most often map to geographic regions where local-scale processes including evaporative discharge in\u00a0closed basins\u00a0or intermittent streams concentrate fluoride in shallow groundwater. Despite this, the RFR model provides spatially continuous F predictions across the basin-fill aquifers where discrete samples are missing. Further, the predictions capture documented areas that exceed the F maximum contaminant level for drinking water of 4\u00a0mg/L and areas that are below the oral-health benchmark of 0.7\u00a0mg/L. 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