Identifying recharge sources and their impacts on a North Central New Mexico shallow aquifer using unsupervised machine learning

Shallow aquifers are important but highly variable resources in arid to semi-arid regions. Limited shallow aquifer volume results in high sensitivity to recharge fluctuations, which can impact the local fauna and flora, and transport of contaminants in the aquifer or vadose zone. Aquifer response to external forcing (e.g., precipitation) is usually solved by estimating aquifer parameters and running physics-based models to match known fluctuations of hydraulic head. However, this technique is time and computationally expensive. Furthermore, high aquifer complexity decreases precision in physics-based models. Alternatively supervised machine learning is used to predict aquifer dynamics. However, these techniques rely on input data and struggle to interpret aquifer response for missing sources (i.e., snowpack data). To counter these problems, we propose an unsupervised machine learning technique (NMFk) to estimate the impact of different sources on aquifer recharge. NMFk is used to understand the influence of external forcing on shallow aquifer recharge in the Pajarito Plateau (Los Alamos, NM, USA). The results show how NMFk can be used to reduce the data dimension in a complex field dataset to three recharge signals that cause fluctuations within the field data. Here, the source signals are interpreted as rainfall, snowmelt, and a delayed aquifer response to the previous two signals. These results evidence how heterogeneous aquifers delimited by canyons incised into the Pajarito Plateau respond in similar ways to the source signals identified by NMFk. Furthermore, results show the importance of the local geology where faults act as sinks, and anthropogenic disturbances can facilitate infiltration amplifying the interpreted signal. • Aquifer is highly dependent on climate forcing e.g., snowfall and rainfall recharge. • Snowmelt acts as a baseline recharge source while rainfall is the main driver for hydraulic head fluctuation. • Shallow aquifer is not compartmentalized and is sensitive to anthropogenic activities. • Recharge identified with machine learning.

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Publication Details

Journal
Journal of Hydrology
Published
2024-12-12
DOI
https://doi.org/10.1016/j.jhydrol.2024.132503
Citations
1
Primary Topic
Groundwater flow and contamination studies
Type
article
Field-Weighted Citation Impact
0.21

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article

Identifying recharge sources and their impacts on a North Central New Mexico shallow aquifer using unsupervised machine learning

Katrina E. Bennett, Philip H. Stauffer, Noah Hobbs, Bulbul Ahmmed et al.
1 citations
Journal of Hydrology
Groundwater flow and contamination studies
0.21
article

Identifying recharge sources and their impacts on a North Central New Mexico shallow aquifer using unsupervised machine learning

Katrina E. Bennett, Philip H. Stauffer, Noah Hobbs, Bulbul Ahmmed, D.F. Sulca
article en
1 citations

Abstract

Shallow aquifers are important but highly variable resources in arid to semi-arid regions. Limited shallow aquifer volume results in high sensitivity to recharge fluctuations, which can impact the local fauna and flora, and transport of contaminants in the aquifer or vadose zone. Aquifer response to external forcing (e.g., precipitation) is usually solved by estimating aquifer parameters and running physics-based models to match known fluctuations of hydraulic head. However, this technique is time and computationally expensive. Furthermore, high aquifer complexity decreases precision in physics-based models. Alternatively supervised machine learning is used to predict aquifer dynamics. However, these techniques rely on input data and struggle to interpret aquifer response for missing sources (i.e., snowpack data). To counter these problems, we propose an unsupervised machine learning technique (NMFk) to estimate the impact of different sources on aquifer recharge. NMFk is used to understand the influence of external forcing on shallow aquifer recharge in the Pajarito Plateau (Los Alamos, NM, USA). The results show how NMFk can be used to reduce the data dimension in a complex field dataset to three recharge signals that cause fluctuations within the field data. Here, the source signals are interpreted as rainfall, snowmelt, and a delayed aquifer response to the previous two signals. These results evidence how heterogeneous aquifers delimited by canyons incised into the Pajarito Plateau respond in similar ways to the source signals identified by NMFk. Furthermore, results show the importance of the local geology where faults act as sinks, and anthropogenic disturbances can facilitate infiltration amplifying the interpreted signal. • Aquifer is highly dependent on climate forcing e.g., snowfall and rainfall recharge. • Snowmelt acts as a baseline recharge source while rainfall is the main driver for hydraulic head fluctuation. • Shallow aquifer is not compartmentalized and is sensitive to anthropogenic activities. • Recharge identified with machine learning.

Journal of HydrologyVol. 650
Los Alamos National Laboratory (US)
Office of Science, Office of Environmental Management
Openalex Percentile: Top 48%
Groundwater flow and contamination studies
0.21
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