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Predicting Groundwater Hydrochemical Facies in Three Dimensions with Random Forest Classification, USA
Paul E Stackelberg, Katherine J Knierim1, Kenneth Belitz2
1U.S. Geological Survey, Little Rock, AR.
Ground Water
|April 24, 2026
Summary
A random forest model predicts groundwater hydrochemical facies (HCFs) across the US. The model accurately maps HCFs in 3D, revealing transitions from bicarbonate to chloride facies with depth.
Area of Science:
- Hydrogeology
- Geochemistry
- Machine Learning
Background:
- Understanding groundwater hydrochemical facies (HCFs) is crucial for managing water resources.
- Existing methods for HCF mapping are often limited in spatial and vertical resolution.
Purpose of the Study:
- To develop and apply a three-dimensional random forest classification (RFC) model to predict groundwater HCFs across the conterminous United States (CONUS).
- To map HCFs at a 1-km² resolution to depths of 400 m below the base of drinking water.
Main Methods:
- Utilized major-ion data from 152,673 sites to define six HCFs (CaMg-HCO₃, NaK-HCO₃, CaMg-SO₄, NaK-SO₄, Cl, Mixed).
- Engineered model features including elevation relative to the base of drinking water (ERDW) and geologic unit flags.
- Employed RFC modeling, identifying ERDW as the most significant feature.
Main Results:
- Successfully mapped HCFs across CONUS at a 1-km² resolution and to significant depths.
- Predicted CaMg-HCO₃ facies near the water table in humid regions and carbonate/crystalline rock areas.
- Observed a rapid transition from HCO₃ to Cl facies at depths below drinking water supplies.
Conclusions:
- The RFC model provides accurate, high-resolution 3D predictions of groundwater HCFs.
- Model predictions align with geochemical expectations and are validated by point data and regional averages.
- The HCF maps can inform groundwater resource management, including salinity and characteristic mapping.
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