Frequently asked questions

Health and safety

Every member of our field team has the following certifications:

  • OSHA HAZWOPER 40 Hour
  • TWIC
  • SafeLand
  • Red Cross CPR and First Aid

Some members of the field team also have the OSHA HAZWOPER supervisor certification as well as the NOLS Wilderness First Aid certification.

Yes.
For each measurement, our surveys use less than one amp of current for less than one second, which is considered safe for humans. Pets and livestock are kept clear of the area to protect the equipment.

Yes.
Particularly relative to other high-resolution site characterization (HRSC) methods. Electrode stakes are driven into the earth typically 12 to 16 inches deep, which is above most utility burial depths in theory. Aestus uses both public and private utility locating services to promote the protection of utilities and our field staff.

Vegetation clearing in straight lines is required prior to GeoTrax Survey field work, if dense vegetation exists. While large trees can normally stay, mitigation of trip hazards due to low lying stumps, etc., is important.

No.
Please do not drive over our cables as this will damage them. We have traffic ramps to place over the cables and allow vehicles to cross.

How it works

GeoTrax Survey™ is a geophysical survey technique that provides high-resolution, two-dimensional (2D) images of the earth’s subsurface. It is analogous to a CAT Scan in the medical industry.

It is used to map geology, locate environmental contamination, target production water wells, identify potential geohazards, monitor changes over time (temporal imaging), and has other uses.

Electrical current (safe level) is injected into the ground, and the voltage is measured coming back out. Ohm's Law is used to calculate resistivity:

  • Four electrodes yields one measurement data point (a “pixel”)
  • Iterative measurements yield a matrix of data points, or “pixels”
  • Proprietary software generates a subsurface image from the datapoints, which is similar to a digital camera taking an electrical picture of subsurface

The theoretical resolution is 1/2 the spacing of the electrodes.
Example: 1- meter spacing results in a 0.5 -meter data resolution. A 10 -meter spacing results in a 5 -meter resolution.

The depth of the image is 1/5 (20%) of the length of the transect line (electrode array) on the ground surface. So a 500-foot-long transect line yields an imaging depth of 100 feet below ground surface (BGS). Based on the imaging objective depth, we evaluate how to best obtain the data for the project objective.

We have imaged up to 1,000 feet BGS, but our stakes only go into the ground about 12-16 inches. The technique is indirect. The flow of current generates the image, not the electrode.

We use 3/8-inch diameter stainless steel electrode stakes, which are driven into the soil typically 12-16 inches deep. Cables are connected to the electrodes and to field computers that collect the data.

We pre drill a 1/2-inch diameter hole through the pavement such that our electrode stakes can be driven into the soil a short distance below the bottom of the pavement. We patch the holes in the pavement upon completing our work on site.

Yes.
Even with direct push HRSC tools (MIP, HPT, UVOST, TarGOST, etc.), investigations are still essentially “blind” without GeoTrax Survey™
guidance. Key site features such as vertical preferential flow paths and LNAPL zones can be missed if HRSC is used alone.

Please do not drive over our cables as this will damage them. We have traffic ramps to place over the cables and allow vehicles to cross

We use a standard 12-volt-deep cycle marine battery as a power source. A current of ~350 milliamps is “injected” into the ground. Because this is relatively low current, it is safe for pets and people to travel past our survey lines. People should avoid contact with electrode stakes and be careful not to trip over our geophysical cables.

Vegetation clearing in straight lines is required prior to GeoTrax Survey field work, if dense vegetation exists. While large trees can normally stay, mitigation of trip hazards due to low lying stumps, etc., is important.

No.
We can design our survey layouts around known utilities. You should avoid surveying immediately parallel to metallic pipelines, and if possible, turn cathodic protection off as a safeguard.

The physics of the technology dictates that the shape of the resulting survey images is trapezoidal. Therefore, if the surveys were performed with the ends touching and no overlap, there is effectively a hole in what would otherwise be a continuous image along the transect line.

Yes.
Provided the area is safe to walk on. Steep slopes, high to low elevation changes, piles of soil, concrete walls, etc. are all manageable obstacles.

Yes.
Please notify us in advance of field work if particular site material or specification is mandated. Otherwise, we will clean stake holes so they are free of any loose debris. We will fill holes with caulk patch material (asphalt or concrete colored). Finally, we will smooth patches so they are level with the surface of the concrete or asphalt.

Aestus likes to incorporate as many data sets into each 3-D model as possible. The more data that can be viewed together in one place, the better chance there is of seeing trends in the data and developing a better understanding of the site.

Yes.
Particularly relative to other high-resolution site characterization (HRSC) methods. Electrode stakes are driven into the earth typically 12 to 16 inches deep, which is above most utility burial depths in theory. Aestus uses both public and private utility locating services to promote the protection of utilities and our field staff.

Direct push HRSC generally provides higher vertical resolution, while GeoTrax Survey™ offers continuous lateral coverage. The results typically
correlate well and together provide a more complete understanding of subsurface conditions. For example, HRSC can confirm high-permeability
zones which GeoTrax Survey™ can then connect across the site.

Yes.
  • Electrodes along the cables are supported or floated at the water surface
  • The cable can remain submerged
  • Strong wave action or currents increases logistics

GeoTrax Survey™ transects consist of an electrical cable with 56 electrode stakes. These stakes are deployed in a straight line and driven 8-14 inches deep into the subsurface.

Aestus likes to incorporate as many data sets into each 3-D model as possible. The more data that can be viewed together in one place, the better chance there is of seeing trends in the data and developing a better understanding of the site.

3-D Models typically include the following data sets, at a minimum (assuming data is available from client):

  • GeoTrax Survey™ locations
  • Monitoring well locations
  • Interpolated groundwater level surface
  • Aerial photo or base map of the site
  • Interpolated bedrock surface
  • Groundwater and/or soil analytical data
  • Bioparameter indicators
  • Utility locations

Historically, both methods generally agree in terms of identifying impacted zones, but GeoTrax Survey™ often provides more context. For example, one energy firm compared GeoTrax Survey™, Laser-Induced Fluorescence (LIF), and soil samples and found that LIF sometimes produced false positives where GeoTrax Survey™ and soil borings showed no contamination. These false positives were viewed as a potential liability.

As another example, the image below provides a comparison of GeoTrax Survey™, TarGOST® (Tar-Specific Green Optical Screening Tool), and a traditional soil boring at a former tie treatment facility.

  • The GeoTrax Survey™ images were able to map the vertical/horizontal extents of DNAPL related impacts across the imaging domain – impacted zones correlated with the more moderately electrically resistive anomalies (i.e., orange zones)
  • Soil Boring 5 confirmed that there was a higher saturation of oil in the center of the orange zones (i.e., in the strongest part of the anomaly)
  • TarGOST (TG) log detects shown below in orange graphical plots generally occurred within the same electrical anomalies, but the higher TarGOST® reflectance was generally limited to the top of Aestus’ orange anomalies (NOT supported by the soil boring).

Your family pet is ailing so you consult a veterinarian who runs a few simple tests which indicate a more serious issue requiring surgery. The vet performs an MRI high resolution scan to identify exactly where/what is the root cause of the problem so the surgery can be targeted. The medical industry knows empirically that the investment in the scanning data (only ~10% of the surgery cost) is essential to facilitate successful surgery and minimize liability.

Similarly, if a site owner believes its site might be “sick” (environmentally impacted) it is typically prudent and necessary to spend up to ~10% of the projected remediation costs to perform Ultra-High Resolution Site Characterization (UHRSC) to target remediation work. The resulting data dense conceptual site model (CSM) identifies root cause(s) of site issues and facilitates faster and cheaper remediation, while reducing potential trailing liabilities.

Aestus’ proprietary method of data collection and processing (GeoTrax Survey™) is up to several orders of magnitude more sensitive than traditional methods (Miller et al., 2014), ensuring the resulting images are more representative of the subsurface. ERI data are collected as raw resistivity data that have to be inverted (i.e., processed) to produce a model of the resistivity structure of the subsurface. The sensitivity refers to how well the inversion can detect spatial variability of resistivity. Greater sensitivity yields higher image accuracy relative to representing subsurface conditions, which leads to a more “drillable” image.

Site considerations

Yes.

Aestus can:

  • Scan a proposed slurry wall alignment to find zones of competent geology, which might cause problems during installation
  • Locate slurry walls (post construction)
  • Image zones of slurry loss (during construction)
  • Scan a known slurry wall alignment to check for integrity of the slurry wall

It should be noted that slurry walls can be observed on a one-time basis to evaluate if flow is moving beneath or laterally around the wall. Additionally, temporal (GeoTrax Monitoring™) data can be used to test the effectiveness of the wall at installation and over time. This is especially helpful if the wall is a permeable reactive barrier and the flow dynamics need to be assessed.

Yes.
GeoTrax Survey™ lines can run across and parallel to railroad tracks. The survey lines can go over the tracks, and in many cases, electrode cables can be threaded through the track ballast beneath the track. This allows train traffic to continue during data collection.

Depending on the railroad’s governing body’s regulations, GeoTrax Survey™ work within ~25 feet of an active line or any electrode cables crossing over top of the rails will require no train traffic for a duration of approximately 3 hours per survey line. Sometimes, GeoTrax Survey™ work can be completed during non-operational hours for trains. We rely on our clients to attain the right entry permits and permissions necessary to work on railroad property.

Aestus field crew members currently have or have recently held the following railroad safety certifications:

Depending on the railroad, additional training or safety classes may be required.

Typically, no special equipment is required. Aestus will follow safety regulations from the governing railroad, which usually includes wearing reflective safety vests, hard hats, safety-toed boots, and safety glasses.

Yes.
  • A person can fit and function between buildings
  • Utilities can be located and avoided
  • 1/2 inch pilot holes are drilled into the buildings flooring to allow electrodes to make contact with the soil. Holes are filled and patched after use.

No.
Aestus relies on our consulting firm and/or railroad clients to provide one or more flagmen who will coordinate track time and communicate with any active trains in the vicinity of our work.

Yes.
GeoTrax Survey™ is independent of lithology, so refusal is not an issue. Aestus can image through bedrock without added cost, even when
use of direct push drilling methods is not possible due to hard lithology.

Yes.
Electrodes along the cables are supported or floated at the water surface. Strong wave action or currents increase logistics.

Yes.
  • Electrodes along the cables are supported or floated at the water surface
  • The cable can remain submerged
  • Strong wave action or currents increases logistics

Yes.
  • Aestus’ GeoTrax Survey™ specialty ERI methods CAN detect electrically resistive anomalies within a conductive environment such as brackish/saline groundwater and with good data quality
  • This is contrary to the use of standard electrical resistivity imaging (ERI) techniques which have difficulty imaging or “seeing” resistive targets of interest (e.g., contamination which sometimes has an electrically resistive signal) in a highly conductive environment
  • Aestus’ methods allow pockets of contamination to be detected, even in brackish/saline environments, to achieve more certainty of subsurface conditions
  • Other electrical resistive targets (e.g., gravel channels) can also be detected in an electrically conductive matrix.

Yes.
Continuous 2D GeoTrax Surverys™ can delineate horizontal and vertical extents.

Confirmation drilling

Similar to the medical industry where scanning data is calibrated via biopsies, or the oil industry where geophysics is calibrated with borehole data, we need to calibrate our imaging data (via targeted drilling) to contaminant concentrations, geology, and bioactivity levels.

No.
Our clients have local site drilling and laboratory experience and are typically closer to the site to perform confirmation drilling work more cost effectively.

All sites are different, and we can provide an estimate during the proposal process. The goal is to minimize drilling over time by focusing these efforts via targets from our electrical imaging.

No.
Both methods are qualitative in the sense that they do not provide precise contaminant concentrations in soil and groundwater. Therefore,
conventional sampling and analytical laboratory analyses may still be required, depending on site conditions and regulatory requirement.

Typically, we recommend installing monitoring wells to better assess groundwater chemistry and the presence or absence of non-aqueous phase liquids (NAPL), especially in fine-grained media. For example, it can take months for NAPL to show up in wells screened in clays. Most sites are regulatory driven by groundwater concentrations, so avoiding potential false negatives is important. An iterative discussion of confirmation drilling is recommended.

You should schedule confirmation drilling approximately 12 weeks after the last day of field work, which is just after we deliver your interim report with specific suggestions regarding drilling locations and sample intervals. This allows for data integration and discussions of confirmation drilling plans.

Aestus provides recommendations on sampling protocols that allow confirmation of GeoTrax Survey image results based on attaining regulatory endpoints. We provide a table of confirmation drilling locations and analytes for each project.
Technology Selection Matrix

The Subsurface Technology Selection Matrix

Choose the right subsurface tool for your jobsite.

Not sure which technology to use for site characterization? We’ve got you covered.

Our free Subsurface Technology Selection Matrix helps you match your project size and goals with the right scanning tools. Whether you’re chasing contamination, mapping groundwater, or planning remediation, this guide gives you the clarity you need to move forward with confidence.
This guide will help you…
  • Avoid wasted time and budget on tools that don’t fit your site needs
  • Learn the strengths and limitations of each major subsurface technology
  • Get expert guidance on when to scan, drill, or combine both for best results

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Madison Culver
Madison Culver, M.Sc.
Staff Geologist / Field Technician
Since joining Aestus in 2024, Madison has performed various project tasks including field data acquisition, data integration and analysis, 2D and 3D visualization, and project report development.

As an undergraduate at Oklahoma Sate University, Madison utilized electrical resistivity imaging to locate a drilling target for a municipal water well in rural Oklahoma. Her Master’s degree, also from Oklahoma State University, focused on the production and laboratory testing of a novel groundwater tracing particle for use in a sole source aquifer.

Madison previously worked at an environmental consulting firm in Dallas, Texas, where she performed soil/groundwater investigations/reporting, PFAS sampling programs, and Environmental Site Assessments.

Madison is based out of Irving, Texas.
Michelle Lahti
Michelle Lahti, PACE
Administrative Director
Since joining Aestus in 2021, Michelle has supported the CEO and other managers in their day-to-day needs. She also manages human resources and all elements of the many conferences Aestus attends. Michelle works hard to ensure that the needs of stakeholders are addressed in all steps of the business process when working with our clients.
Michelle has a bachelor’s degree in Avionics Engineering Technology from Embry-Riddle Aeronautical University. She also has experience as a small business owner, and over 15 years’ experience as an executive assistant in many different industries. She has her Professional Administrative Certification of Excellence (PACE) through the American Society of Administrative Professionals (ASAP).
Michelle is based out of Wellington, Colorado.
Autumn Town
Autumn M. Town, M.Sc.
Staff Geologist / Field Technician
Autumn performs various project tasks for Aestus, including field data acquisition, data integration and analysis, 2D and 3D visualization, and project report development. Since joining Aestus in 2023, she has helped meet project objectives such as mapping stratigraphy, identifying areas of contamination, and characterizing preferential flow pathways at complex sites across the United States.
As an undergraduate at Oklahoma State University, Autumn utilized electrical resistivity imaging (ERI) to evaluate the hydrogeologic effects of PFAS-containing firefighting foams. While completing her Master’s degree, also at Oklahoma State University, she focused primarily on sedimentology and stratigraphy as she studied the effects of depositional and diagenetic processes on porosity development in a tight gas sandstone reservoir.

Autumn is based out of Tulsa, Oklahoma.
Morgan Love
Morgan Love, M.Sc.
Senior Project Geologist
Morgan has been a part of the Aestus team since 2012. She supports all aspects of data integration for Aestus in 2D and 3D space, including modeling of geophysical, geochemical, and geologic data. She also performs geophysical data processing and develops quality control and automation protocols to ensure data integrity.

Prior to Aestus, Morgan used her environmental geology undergraduate degree working for a water resource company, a geosciences software company, and a seismic data acquisition company. She holds a Master's Degree in Computer Information Systems.

Morgan is based out of Fort Collins, Colorado.
Grant Eastman
Grant Eastman
Equipment Manager / Field Technician
Grant maintains all our equipment and vehicles at a firehouse ready status in order for the field team to be ready to mobilize at moment’s notice. He also troubleshoots any technical issues that come up as well as being a member of the field team.

Grant graduated from Colorado State University with a degree in Watershed Science. After graduating he completed 8 years of military service with the Colorado Army National Guard, including two deployments to the middle east. Before joining Aestus, he was a senior technician building custom automation equipment and wire harness mockups for aerospace companies.

Grant is based out of Milliken, Colorado.
Samantha Frandsen
Samantha Frandsen, M.Sc, P.Gp.
Hydrogeophysicist / Project Manager
Since joining Aestus in 2018, Samantha has performed all aspects of the Aestus project lifecycle, including acquisition field work, processing of geophysical data, data integration, 3D visualization, and reporting. As project manager, she oversees a variety of projects completed at complex sites across the United States and strives to help our clients efficiently leverage Aestus’ high-resolution GeoTrax Survey™ data to improve understanding of subsurface conditions.

Prior to her time with Aestus, she earned her Bachelor’s degree (magna cum laude) in Physics from the University of Richmond and taught high school physics as a Teach for America corps member. She then completed her Master’s degree (Distinction) in Exploration Geophysics at the University of Leeds in the UK. For her thesis, she utilized several different geophysical techniques to characterize the subsurface remains of a former gasworks facility for which she was awarded the GETECH award for best overall performance in the Independent Project and the Association for Industrial Archaeology’s Dissertation Award.

When she’s not investigating what’s below the ground, Samantha enjoys exploring all the above-ground fun her Stateline (South Lake Tahoe), NV home has to offer via trail running, mountain biking, and snowboarding.

Samantha is based out of Stateline, Nevada.
Michael McNair
Michael McNair
Project Geologist / Field Team Leader
Michael has worked on a variety of project types using Aestus’ electrical hydrogeology techniques to help Aestus’ clients succeed relative to characterization of contaminated sites, evaluating geohazards, municipal water well exploration, and monitoring subsurface changes over time. Michael currently manages Aestus’ field operations to collect high quality subsurface electrical imagery (GeoTrax Survey™) at rural, urban, and industrial sites with complex logistics. When not in the field, Michael is a key member of Aestus’ reporting team and leads or assists with 2D/3D data integration, QC, data interpretation, and reporting.

Michael previously worked at an environmental consulting firm in Dallas, Texas, where he performed soil/groundwater investigations in the field and subsequently developed reports. Michael earned a Bachelor of Science in Geology from Baylor University.

Michael is based out of Orlando, Florida.
Todd Halihan
Todd Halihan, Ph.D., P.Gp.
CTO/Data Interpretation Lead
Todd’s focus at Aestus centers on subsurface characterization using electrical hydrogeology and sustainable water supply. He is also a professor and the Sun Company Clyde Wheeler Chair in Hydrogeology at Oklahoma State University. He was the National Ground Water Association’s 2018 McEllhiney Lecturer and he is a founding member of the NGWAU program for groundwater outreach and education.

Dr. Halihan is the recipient of the American Institute of Hydrology’s C.V. Theis Award winner. He is also a professional geophysicist (CA), professional driller (OK) and a PADI divemaster.

Todd is based out of Stillwater, Oklahoma.
Stuart McDonald
Stuart W. McDonald, P.E.
CEO/Project Executive/Contracting
Stuart has dedicated over 20 years of his career overseeing the development of Aestus with the goal of empowering clients worldwide to gain more certainty in subsurface issues to make better technical decisions and save time and money on their projects. He has been involved in managing hundreds of projects for Aestus in the USA, Europe, Asia, and South America.

Stuart spent the first decade of his career as an environmental consultant primarily with Canonie Environmental and Harding Lawson Associates and gained experience performing cradle to grave site characterization and remediation work on high profile Superfund and other projects. This experience was the genesis of founding Aestus in 2001 as it became clear that the environmental industry needed more data density and more certainty for optimal decision-making on projects.

Stuart is based out of Loveland, Colorado.