At the intersection of isotope geochemistry and hydrogeology, we use environmental tracers to test what groundwater models assume — how aquifers connect, how long water is stored, and where it goes underground.
Recent peer-reviewed work from the lab
The systems we model as sealed are quietly talking to each other.
Every drop leaving a catchment carries a memory of when it arrived.
The subsurface refuses to mix.
The same fingerprints that date a raindrop can reconstruct an ancient climate.
Evaristo Critical Zone Hydrology Lab

Jaivime is an Assistant Professor at the University of Georgia. A full-blooded Filipino geoscientist and US permanent resident (green card holder) with a non-traditional career path, he earned an undergraduate degree in Cell Biology from the University of the Philippines before spending a decade in industry and management consulting. He later pursued an MS in Geosciences (hydrogeology concentration) at the University of Pennsylvania, followed by a PhD at the Global Institute for Water Security, University of Saskatchewan. From 2019 to 2024, he was a tenured Assistant Professor at Utrecht University.
His research focuses on the critical zone and uses tools in hydrology, water resources, and isotope geochemistry to characterize the influence of natural and anthropogenic processes on matter and energy exchange across the hydrosphere, geosphere, and atmosphere.
Outside of work, he loves spending time with his wife and two kids!
Jessica is a PhD student at the University of Georgia and an assistant professor at the University of the Philippines Los Baños. She finished an Erasmus Mundus Joint Masters Program in Sustainable Tropical Forestry (SUTROFOR) at Bangor University, UK and the University of Copenhagen, Denmark. She is particularly interested in how land use affects water quantity and quality.
Funding: U.S. Forest Service

Audra is a recent graduate of the College of Coastal Georgia with a BS in Environmental Science. She has experience as an environmental consultant and is passionate about wetland conservation and management. She is interested in surface and groundwater interaction using environmental tracers and numerical modeling.
Funding: The Chemours Company; U.S. Geological Survey

Maxton joins the lab as Summer 2026 Hydrology and Water Resources Intern. He is interested in understanding how natural disasters impact the stability of forest and coastal ecosystems. Maxton is a prospective 2028 graduate of the University of Georgia with a degree in Natural Resource Management and Sustainability with a concentration in Water and Soil Resources.
Testing what groundwater models assume, at the intersection of isotope geochemistry and hydrogeology
Hydrogeologists draw confining units as solid lines on a cross-section — an assumption inherited, not a quantity measured. Tracers say otherwise. At the Okefenokee Swamp, isotopes and hydraulic head show the Hawthorn Formation leaks, upending the regional conceptual model and the water budget built on it. Across Okefenokee, Coweeta, and Sapelo Island, the question is how many other "confined" systems are confined only on paper.
Storage is not a bucket waiting to be emptied. It is age-structured, and that structure — not the volume — governs how a catchment buffers, delays, and releases water and everything it carries. StorAge Selection functions and transit-time distributions make that hidden structure legible, turning "how much water" into "how old." Our TTD Toolkit puts those methods in anyone's hands.
We model the subsurface as a reservoir that blends whatever enters it. It does not. Water sits in compartments — pore-scale, depth-structured — that exchange so reluctantly a catchment can hold water for years to decades. The critical zone reaches well below its weathered skin, into fractured saprolite and bedrock no shovel can reach, so geophysics and depth-resolved tracers stand in for excavation. How much of a catchment's memory hides in rock nobody has sampled?
A tracer is not a topic; it is a method that ignores scale. The same isotopic and geochemical fingerprints that pin down a nitrate source, map submarine groundwater discharge, or follow a contaminant through an urban stream also read lithium from oil-field brines and temperature from ancient clays. One measurement principle stretches from a contaminant plume to a Paleogene summer.
Peer-reviewed (* = equal contributions / co-lead / co-corresponding)
University of Georgia
Advanced analysis of hydrologic processes — precipitation, evapotranspiration, streamflow, groundwater occurrence and movement, and soil zone flow and transport. Emphasis on quantitative methods with field and laboratory data.
Explore how scientists use environmental tracers — like isotopes and chemistry — to unravel the movement of water above and belowground, track pollution, and date water and contaminant sources using cutting-edge tools and data science.
Intensive, literature-driven and field-based exploration of hillslope hydrology. Students complete a journal-style critical review and collaborative field project synthesizing course concepts.
Soil formation and morphology, physical and chemical properties, soil-water interactions, hydrologic processes, and water quality. Co-taught with Matt Levi (Soils).
Hands-on introduction to stable and radioactive isotopes as natural "fingerprints" that trace the origins of water and other materials. First-Year Odyssey Seminar.
Professional and institutional service
Stable isotope analysis services for water and other liquid samples
Our Picarro L2140-i consistently outperforms factory specifications, achieving δ18O and δD precision approximately three times better than the manufacturer's guaranteed values. The instrument supports high-throughput, high-precision analysis of water isotopes for hydrology, ecology, and water resources applications.
Per-sample rates by isotope analysis, sample type, volume tier, and UGA affiliation.
| Isotope analysis | Sample type | UGA rate / sample | Outside UGA rate / sample | ||
|---|---|---|---|---|---|
| 1–200 samples | 200+ samples | 1–200 samples | 200+ samples | ||
| 2H, 18O | Water | $8.82 | $8.82 | $9.41 | $8.82 |
| 2H, 18O, 17O | Water | $10.29 | $10.29 | $10.98 | $10.29 |
| 2H, 18O | Other liquids* | $26.45 | $26.45 | $28.23 | $26.45 |
| 2H, 18O, 17O | Other liquids* | $30.86 | $30.86 | $32.94 | $30.86 |
*Other liquids = liquids with high total dissolved solids (e.g., plant leaves, stems, juices). Note: Analysis of brackish or brine samples may incur higher rates due to greater consumption of consumables (syringes, septa, salt liners). Please contact us for a custom quote on non-standard sample types.
Please contact Dr. Evaristo for detailed information prior to sample collection and before sending your samples to our lab. This ensures we can advise on appropriate sampling protocols, container types, shipment logistics, and turnaround times for your specific project.
Email: evaristo@uga.edu
Address: University of Georgia, Athens, GA 30602, USA
Upload a results spreadsheet to visualize your samples on a map and in δ²H–δ¹⁸O space against the Global Meteoric Water Line — with descriptive statistics, d-excess, and an optional Local Meteoric Water Line. Everything runs in your browser; no data is uploaded anywhere.
Interactive daily discharge records for every USGS gaging station in Georgia
Explore daily streamflow from more than 600 U.S. Geological Survey gaging stations across Georgia and the Georgia–Florida border strip — including the shared border rivers (St Marys, Suwannee, Apalachicola) whose gages USGS files under Florida — more than 5.4 million daily discharge values spanning 1883 to the present. Search or map-select a station, zoom through its full period of record, and examine seasonal flow regimes, flow duration curves, and annual water-year trends. The dataset refreshes automatically every morning from the USGS National Water Information System, so the record shown is always current. Any station’s records can be downloaded as CSV directly from the explorer — or grab the complete nightly-refreshed archive.
Interactive daily water-level records for every USGS recorder well in Georgia
Explore groundwater levels from nearly 3,000 U.S. Geological Survey wells across Georgia: 409 continuous recorder wells (2.6 million daily readings back to 1942) plus 2,536 periodic wells measured by field visits (315,000 measurements back to 1900), from the surficial aquifers of the coast to the Upper Floridan and the Piedmont crystalline rocks. Every well is labeled by type — recorder or periodic — with a type filter, and wells with fewer than three usable measurements are left out of the viewer. Search or map-select a well, zoom through its full record, and examine seasonal patterns, level duration curves, annual means, and water-table trends. The dataset refreshes automatically every morning from the USGS National Water Information System. Any station’s records can be downloaded as CSV directly from the explorer — or grab the complete nightly-refreshed archive.
Interactive daily water-level records for every USGS recorder well in California
Explore groundwater levels from nearly 13,000 U.S. Geological Survey wells across California: 486 continuous recorder wells (10 million daily readings across depth and elevation series) plus 12,369 periodic wells measured by field visits (2.3 million measurements back to 1900), from the Coastal Basin aquifers to the Central Valley and the Basin and Range. Every well is labeled by type — recorder or periodic — with a type filter, and wells with fewer than three usable measurements are left out of the viewer. Many recorder wells report both depth to water and water-surface elevation; switch between series, overlay field measurements, and examine seasonal patterns, level duration curves, annual means, and water-table trends. The dataset refreshes automatically every morning from the USGS National Water Information System. Any station’s records can be downloaded as CSV directly from the explorer — or grab the complete nightly-refreshed archive.
2019 – 2024 · Tenured Assistant Professor
From 2019 to 2024, I was a tenured Assistant Professor at Utrecht University in the Netherlands. This page archives my teaching and graduate supervision from that period.
Fundamental understanding of catchment functions (partition, storage, release) and hydrological processes in natural and built environments. Students explore sustainable strategies for water resources management using critical thinking, quantitative skills, and management methodologies.
Considerations, methods, and research best practices in water science and management. Prepares future water sector professionals to formulate and implement reasonable courses of action for complex water issues. Partly prepares students for their master thesis.
Scientific analysis of the processes governing the interaction between biota and the hydrological cycle. Practical application through computer modeling of ecohydrological systems at different scales.
Earth's energy balance, the hydrological cycle, and the elemental cycles of carbon, nitrogen and phosphorus. Major stocks of energy, water, and elements across the atmosphere, hydrosphere, lithosphere, and biosphere.
Total theses supervised at Utrecht: 11 Masters and 9 Bachelors.