Per- and polyfluoroalkyl substances (PFAS) have drawn increasing scrutiny due to their persistent nature and potential health risks. As regulations tighten and public awareness grows, accurate PFAS soil testing becomes crucial for environmental safety, regulatory compliance, and public health. As a senior environmental engineer, I have witnessed firsthand the complexities associated with PFAS contamination, especially in soil—a crucial medium that can impact water supply, agriculture, and human health. This article aims to provide a comprehensive overview of PFAS soil testing, covering its importance, methodologies, regulatory landscape, and emerging technologies to equip stakeholders with the knowledge they need to navigate this pressing issue.
Soil investigation is the field-facing half of PFAS Testing & Analysis. Where laboratory work determines what a sample contains, field work determines whether the sample means anything — whether it was taken in the right place, at the right depth, without contaminating it in the process, and against a background that makes the number interpretable. Soil testing is also where PFAS work departs most sharply from conventional contaminated-land practice, because the sampling prohibitions, the units, and the partitioning behaviour are all different.
PFAS, often referred to as "forever chemicals," are a group of synthetic compounds widely used for their water- and grease-resistant properties. They have been utilized in a variety of applications, from firefighting foam to non-stick cookware. According to the EPA’s PFAS Action Plan of 2023, nearly 200 PFAS compounds are currently detected in the environment. Their persistence raises concerns about bioaccumulation and potential adverse health effects, including immune dysfunction, hormonal imbalance, and increased cancer risks.
Research from the Centers for Disease Control and Prevention (CDC) indicates that PFAS can lead to significant health risks, including liver damage and thyroid dysfunction. As local agencies strive to assess and mitigate these risks, measuring PFAS levels in soil is essential for identifying contamination hotspots.
Soil acts as a reservoir for PFAS, influencing groundwater quality and agricultural productivity. As revealed by a 2024 study published in Environmental Science & Technology, 60% of urban soil samples near known PFAS sources contained detectable levels, highlighting the need for systematic testing.
Composite sampling, where small portions from various locations are combined, is cost-effective, but discrete sampling offers precise results in hotspots. A study from the American Society of Civil Engineers emphasizes the importance of choosing an appropriate sampling strategy to accurately represent contamination levels.
Sampling depth is pivotal; PFAS can migrate through soil layers. The EPA recommends sampling to a depth of at least 1 meter, particularly in areas with history of PFAS use.
This mainstream analytical method provides accurate detection of PFAS compounds. Recent advancements have increased sensitivity, allowing detection limits as low as 0.1 ppt (parts per trillion).
Emerging techniques, such as high-resolution mass spectrometry (HRMS), may soon revolutionize detection capabilities. Investments in research indicate a promising future for non-targeted analysis, potentially identifying unknown PFAS compounds present in contaminated sites.
Field screening kits are becoming increasingly sophisticated, enabling on-site analysis for immediate decision-making. However, these tools should complement laboratory tests due to variable accuracy.
Implementing rigorous QA/QC protocols is critical for ensuring data integrity. A detailed QA/QC plan aligns with EPA standard practices, covering everything from sample collection to laboratory analysis and reporting.
In 2023, the EPA issued new guidelines that set maximum contaminant levels (MCLs) for select PFAS in drinking water. These standards prompt a rigorous "test and regulate" approach, necessitating PFAS soil testing as an integral part of compliance assessment.
Many states have enacted their own PFAS regulations, often more stringent than federal guidelines. For instance, California’s regulations mandate annual soil testing near known contamination sites, reflecting a proactive stance towards public health.
As public awareness rises, additional regulations are anticipated. The National Defense Authorization Act (NDAA) could result in expanded monitoring requirements, signaling a comprehensive shift towards tackling PFAS pollution.
Understanding site history, potential PFAS sources, and environmental conditions is crucial. Developing a comprehensive site characterization plan will guide targeted soil testing strategies.
Engaging local communities and stakeholders enhances transparency and cultivates trust. Sharing findings and updates reinforces the commitment to environmental stewardship.
Clear communication regarding soil testing results is essential for public health and safety. Establishing a straightforward reporting framework can help local agencies convey complex information effectively.
Bioremediation technologies, leveraging microorganisms to degrade PFAS, are gaining traction. Research published by Remediation Journal in 2024 suggests that tailored bioremediation strategies can effectively reduce soil PFAS concentrations.
Innovations in sensor technologies allow continuous monitoring of PFAS levels, facilitating rapid response in mitigating exposure risks.
Remote sensing technologies offer a new frontier in identifying PFAS hotspots, employing satellite data to guide sampling and monitoring efforts.
A 2024 project in a Midwestern U.S. city demonstrated the effectiveness of integrating soil testing with water treatment processes. As a result, PFAS levels were dramatically reduced, ensuring safe drinking water.
A former manufacturing site used innovative soil testing methodologies that identified extensive contamination. Remediation efforts led to successful site redevelopment, serving as a model for similar initiatives.
Farmers are increasingly concerned about the implications of PFAS in soils used for crops. One case study showed how targeted soil testing not only identified PFAS levels but also educated local farmers about best practices for mitigating risks.
Soil investigation divides into a protocol question and a decision question: how the sample is taken, and what the result is used to decide. Both are developed in depth on their own pages.
PFAS field sampling has an unusually long list of prohibitions, and violating any of them can produce a result higher than the contamination being investigated. Our dedicated guide to the PFAS sampling protocol covers the materials that must be excluded from the sampling chain — PTFE-containing equipment, waterproof field notebooks, water-resistant treated clothing, adhesive tapes, certain personal care products worn by field staff — along with the container and preservation requirements, the decontamination procedure between locations, and the blank regime that makes a dataset defensible. It also covers chain of custody and the documentation that distinguishes an investigative result from an enforceable one. For soil work specifically, cross-contamination between depths during coring is the failure mode that most frequently invalidates a vertical profile.
Soil and pilot data exist to support a decision, and in a remediation context that decision is usually which technology to apply. Our coverage of best available technology for PFAS addresses how a technology comes to be regarded as best available, what evidence a regulator expects to see behind that determination, and how site characterisation data feeds the comparison. The link between the two is direct: a defensible technology selection rests on defensible site data, and an investigation designed without reference to the eventual decision routinely produces data that cannot support one.
PFAS do not behave in soil like conventional organic contaminants. Sorption is driven by a combination of hydrophobic interaction and electrostatic attraction to organic matter and mineral surfaces, and it is strongly chain-length dependent — long-chain compounds bind relatively strongly and stay near the release point, while short-chain compounds are far more mobile and migrate ahead of them. The practical consequence is that a soil profile separates chromatographically over time: the shallow zone retains the long-chain signature while the leading edge, often much deeper, is short-chain dominated. An investigation that samples only the shallow zone will characterise the wrong part of the problem and will systematically understate the groundwater threat.
Soil results are reported on a dry-weight basis, conventionally in micrograms per kilogram or nanograms per gram — not in the parts-per-trillion units used for water. Confusing the two produces errors of several orders of magnitude and is common enough in reporting to be worth checking on every deliverable. Results should also be moisture-corrected, and the correction basis stated, because a wet sample and a dry one from the same location will otherwise appear to differ.
PFAS are present at low concentrations in soils with no identifiable point source, which means a detection is not by itself evidence of a release. Background reference sampling — upgradient, off-site, and in comparable soil types — is what converts a detection into an attributable finding. Skipping it is the most common reason a soil dataset cannot support a liability or enforcement position later, and it costs a small fraction of the main investigation.
Because chain length drives mobility, depth resolution frequently matters more than areal density. A programme that takes many shallow samples across a wide area may map the surface footprint accurately while missing the leading edge entirely. Design discrete-depth intervals through the unsaturated zone to the water table where the objective is to assess groundwater threat, and reserve compositing for surface characterisation of a broad area where the objective is exposure assessment rather than migration.
Different objectives demand different designs, and conflating them wastes money. Delineating a source area calls for discrete high-density sampling near the release. Assessing agricultural exposure calls for surface compositing across the field. Evaluating groundwater threat calls for vertical profiling with leachability assessment. Supporting a liability position calls for background comparison and full chain-of-custody rigour. State the objective before designing the programme, because a single dataset rarely serves all four.
The table below compares the principal approaches on what each is actually good for. Most programmes combine two or more, sequenced from cheap and broad to expensive and definitive.
| Approach | What It Answers | Relative Cost | Defensibility | Principal Limitation |
|---|---|---|---|---|
| Discrete depth-interval sampling | Vertical distribution; leading edge location | High per location | High — the reference approach | Cost; cross-contamination risk between intervals |
| Surface composite sampling | Average surface concentration over an area | Low per unit area | Moderate — masks hotspots by design | Cannot resolve migration or hotspots |
| Background reference sampling | Whether a detection is attributable to a source | Low | Essential for any attribution claim | Requires genuinely comparable soil and land use |
| Leaching and partitioning tests | Groundwater threat from soil concentrations | Moderate | High for migration assessment | Laboratory conditions differ from field |
| Total oxidisable precursor assay | Hidden precursor mass not seen by targeted methods | Moderate–high | Investigative — not a compliance datum | Reports a difference, not identified compounds |
| Field screening kits | Where to place confirmatory samples | Lowest | Low — screening only | Not accepted for enforcement or liability |
| Non-targeted HRMS analysis | Presence of compounds outside the analyte list | Highest | Research-grade; not quantitative for compliance | Cost; interpretation requires specialist input |
Soil investigations follow a stable sequence. The steps most often skipped are the second and the fourth, and both are cheap relative to what skipping them costs.
Establish the release history, the likely source types, the soil and geology, the depth to groundwater, and the receptors before placing a single sampling point. Aqueous film-forming foam use at a fire training area, a landfill footprint, a biosolids application field, and a manufacturing discharge each produce a different spatial signature, and the model determines where sampling will actually be informative. Investigations designed on a grid without a conceptual model reliably spend most of their budget confirming that clean areas are clean.
Collect reference samples in comparable soils outside the suspected influence area, in the same round and by the same protocol. Doing this first rather than last means the comparison is available when results arrive, and it avoids the situation where an attribution question emerges after the field crew has demobilised.
Soil work follows EPA Method 1633, and laboratory accreditation is granted per method and per matrix — accreditation for aqueous samples does not extend to solids. Request the current scope document, confirm the required reporting limits per compound against the screening levels you will be comparing to, and hold laboratory, method, and analyte list constant across the programme. The laboratory selection process, accreditation questions, and quality control package are covered in our guide to PFAS lab testing, which applies directly here with the matrix requirement being the critical difference.
Field, trip, and equipment blanks are not optional in PFAS work, and a positive blank invalidates the associated batch rather than being a note in the report. Agree in advance what blank frequency will be run, what constitutes a failure, and who bears the cost of the resulting resample. Agreeing this before mobilisation converts a dispute into a procedure.
The failure mode specific to PFAS field work is that ambient contamination from ordinary field materials routinely exceeds the concentrations being measured. Exclude PTFE-containing equipment, waterproof or water-resistant notebooks, adhesive tape, and treated weather gear from the sampling chain, and brief field staff on personal care products applied that morning. Decontaminate between locations and between depth intervals, and document the procedure. On soil work specifically, carrying material down a borehole on sampling equipment is the most common source of a misleading vertical profile, and the remedy is procedural rather than analytical.
Log soil organic carbon content alongside every PFAS result. Sorption is driven substantially by organic matter, so two samples with identical PFAS concentrations but different organic carbon represent very different leaching risks — the low-carbon sample will release far more to groundwater. Organic carbon is inexpensive to measure and turns a concentration into an interpretable number. Programmes that omit it frequently have to re-sample when the migration question arrives.
Five recur. Sampling only the shallow zone, which characterises the long-chain signature while missing the short-chain leading edge that actually threatens groundwater. Omitting background reference samples, which leaves detections unattributable. Reporting soil results in water units. Compositing across a suspected hotspot, which averages the signal away by design. And running a field programme without a blank regime, producing a dataset that looks complete and fails when examined.
Treating a soil concentration as directly comparable to a water standard. Drinking water limits are expressed in nanograms per litre for a mobile liquid; soil results are micrograms per kilogram of a solid in which most of the mass is bound. Whether a given soil concentration threatens groundwater depends on organic carbon, chain-length distribution, infiltration, and depth to water — not on the number alone. Comparison requires a leaching assessment or a state screening level derived for that purpose, not arithmetic between incompatible units.
Read the compound distribution, not only the total. A short-chain-dominated profile at depth indicates active migration and a groundwater threat; a long-chain-dominated shallow profile indicates a source area with lower immediate mobility. A large unattributed organic fluorine fraction indicates precursors that will oxidise into regulated compounds over time, which means today’s comfortable result is a deferred one. And always read the case narrative and quality control summary rather than the results table alone — blank detections and recovery failures live there.
There is currently no federal soil cleanup standard for PFAS in the United States. Screening and cleanup levels are set at state level and vary widely in both value and derivation basis, and several states have adopted values considerably more stringent than any federal guidance. The CERCLA hazardous substance designation for PFOA and PFOS in 2024 creates reporting obligations and cost recovery exposure that apply to soil contamination independently of any cleanup standard, and it is the instrument most likely to drive site investigation. EPA regional screening levels provide risk-based reference values for certain compounds but are not enforceable standards. Land application of biosolids is governed by 40 CFR Part 503 together with state restrictions, several of which now specifically address PFAS and in some cases prohibit application. Drinking water obligations arise separately under the Safe Drinking Water Act through the National Primary Drinking Water Regulation for PFAS finalised in April 2024, which established enforceable maximum contaminant levels for water — those values apply to water and cannot be compared directly against soil concentrations. Investigations supporting enforcement or cost recovery should follow the applicable state guidance for data quality objectives and be conducted to a documented quality assurance project plan.
Depth should follow the conceptual site model rather than a fixed figure. Where the objective is to assess groundwater threat, sampling should extend through the unsaturated zone toward the water table, because short-chain compounds migrate ahead of long-chain ones and the leading edge is frequently well below the surface. Where the objective is surface exposure assessment — agricultural land, residential yards — shallow sampling is appropriate. A single prescribed depth applied to every site will be wrong for most of them.
Micrograms per kilogram or nanograms per gram on a dry-weight basis, not the parts per trillion used for water. This distinction matters because comparing a soil result against a drinking water limit is an error of both units and physical meaning: water standards apply to a mobile liquid, while most PFAS mass in soil is bound. Whether soil concentrations threaten groundwater requires a leaching assessment or an applicable state screening level.
No. Screening and cleanup levels are set at state level and vary substantially in both value and derivation. EPA regional screening levels provide risk-based reference values for some compounds but are not enforceable standards. The instrument most likely to drive investigation is the 2024 CERCLA hazardous substance designation for PFOA and PFOS, which creates reporting and cost recovery exposure regardless of whether a cleanup standard exists.
Because PFAS are detectable in soils with no identifiable point source, so a detection alone does not demonstrate a release. Background comparison in genuinely comparable soils is what makes a finding attributable, and attribution is what supports a liability position, an enforcement action, or a cost recovery claim. Programmes that omit background sampling frequently have to repeat the entire investigation when the attribution question arises.
No. They are useful for deciding where to place confirmatory samples across a large or poorly characterised site, which can substantially reduce total analytical cost. They are not accepted for enforcement, permitting, or cost recovery, and results from them should not be reported as though they were quantitative. Use them to allocate the confirmatory budget intelligently, not to replace it.
Not necessarily, and the answer depends on more than concentration. Sorption to organic matter retains a substantial share of the mass, particularly for long-chain compounds, so a high soil concentration in organic-rich material may represent a lower leaching risk than a lower concentration in sandy, low-carbon soil. Depth to groundwater, infiltration rate, and the chain-length distribution all matter. A short-chain-dominated profile at depth is the signature that most reliably indicates active migration.
PFAS soil testing represents a crucial effort to mitigate environmental risks associated with these persistent contaminants. As regulatory pressures intensify and technology continues to evolve, understanding the methodologies, frameworks, and best practices surrounding PFAS soil testing will empower stakeholders to make informed decisions. In navigating the complexities of PFAS contamination, proactive engagement and comprehensive testing strategies are essential for safeguarding public health and preserving the environment for future generations. With continued research and collaboration, we can pave the way towards effective solutions for managing PFAS risks in our soils.