How We Test Our Shilajit
Shilajit is one of the most adulterated supplements on the market. It is also one of the most tested by serious buyers. We think that is the right instinct, and we have designed our testing programme to hold up to scrutiny, not just to pass it.
Every origin we stock is independently tested by EkotechLAB Marek Klein S.K.A., a specialist analytical chemistry laboratory based in Gdansk, Poland. Their heavy metals testing carries PCA accreditation (AB 1755) under the ILAC-MRA framework, an international mutual recognition arrangement covering laboratories in over 100 countries. In practical terms, this means our heavy metals results are recognised as equivalent to those produced by accredited labs anywhere in the world.
What follows is a full account of what we test, why each test matters, and what the results tell you about the product in your hands.
Why we chose EkotechLAB
There are larger, more recognisable names in the testing industry. Eurofins is the most commonly used by supplement brands, and it is cheap, fast, and widely accepted. It is also a generalised, high-volume operation that outsources a significant proportion of its testing to third-party subcontractors. Many of the tests it produces are not themselves accredited, and the chain of custody between sample submission and result can be difficult to trace. For brands that need a certificate to put on a shelf, it serves its purpose.
We wanted something different. EkotechLAB are specialist analytical chemists, not a conveyor belt. The tests they run for us are conducted by their own scientists in their own facility, using methods that are fully accredited where accreditation exists for those methods. When we ask them a question about methodology or interpretation, we get a direct, technically informed answer.
That matters when you are trying to understand what a result actually means, not just whether it passes.
Why testing methodology matters more than any single number
Before you look at any results, it is worth understanding that not all shilajit testing is equal, and that the method chosen to measure humic substances can change a reported figure dramatically.
Many people assume fulvic acid percentage is the headline measure of shilajit quality. We think that framing is too narrow. The most meaningful picture of a shilajit comes from reading the full spectrum of what has been measured: humic acids, fulvic acids, the mineral and trace element profile, and what the testing does not find as much as what it does. A single high fulvic acid figure tells you one thing. A complete analytical profile tells you considerably more.
That said, how fulvic acid is measured matters enormously. We use an analytical method aligned with the standards of the International Humic Substances Society (IHSS), implemented under ISO 19822:2018. This is the reference method used by the scientific community for humic substance analysis. It is precise, reproducible, and internationally recognised.
Many suppliers use titration-based methods instead. Titration measures anything that behaves chemically like a fulvic acid, including compounds that are not fulvic acids at all. The result is a systematically inflated figure. A product tested by titration might report 80% fulvic acid. The same product tested under ISO 19822:2018 might return 40%. These numbers are not comparable, and customers who try to compare fulvic acid percentages across brands without knowing the testing method used are not comparing like with like.
Our results are lower than some you will see advertised. That is not a weakness. It reflects honest measurement.
What each test reveals
The full-spectrum picture: humic acids, fulvic acids, and mineral profile together
The ratio of humic to fulvic acids is not just a quality measure. It is a characteristic of the resin itself, reflecting both the geology of the source region and the degree of processing applied to the raw material.
A higher fulvic acid percentage can indicate a more purified product. But aggressive purification and filtration to concentrate fulvic acids will typically reduce humic acid content and strip out a proportion of the naturally occurring mineral profile. Our Hunza results illustrate this clearly: 64.13% fulvic acid, but only 1.16% humic acid and a comparatively modest mineral profile. Compare that to our Kashmiri at 18.59% humic and 44.87% fulvic, or the Siberian Altai at 5.8% humic and 41.19% fulvic, both of which retain richer humic and mineral profiles alongside their fulvic acid content.
Whether that trade-off is desirable is an open scientific question. Our view is that the full-spectrum composition of the resin, humic acids, fulvic acids, and the mineral matrix together, is likely more meaningful than any single figure in isolation. We present the complete picture and let you decide.
Mineral profile as geographic fingerprint
The mineral composition of a shilajit sample is one of the strongest indicators of its geographic origin. Different mountain ranges have fundamentally different geology, and the organic matter formed within them carries a distinct mineral signature as a result.
Strontium levels are characteristically elevated in shilajit from sedimentary limestone regions because strontium substitutes for calcium in carbonate minerals. Our Kashmiri sample returned 364 mg/kg strontium, the highest of any origin we stock, and consistent with the limestone-dominant sedimentary basin of the Kashmir Valley. Sodium and phosphorus distributions differ markedly between Siberian and Mongolian Altai sources despite both originating from the same mountain range. Iron concentrations in Siberian Altai, at 923 mg/kg, are among the highest of any shilajit origin, reflecting the ancient iron-rich Precambrian rock formations of the region.
A mineral profile that is inconsistent with the claimed origin is a meaningful red flag. One that is consistent with it is not proof of authenticity on its own, but it is a supporting data point that an adulterated or mislabelled product would struggle to replicate convincingly.
Heavy metals
Lead, cadmium, mercury, arsenic, silver, chromium, copper, nickel, and vanadium are all tested across our range. Our results are well within safe limits across all origins.
It is worth noting that trace arsenic levels, 0.7 mg/kg in our Siberian Altai, are geologically expected and not a cause for concern. The absence of any detectable arsenic in a product claiming Siberian origin would actually be the more suspicious result.
Mycotoxins
Mycotoxins are toxic compounds produced by certain moulds. They can be present in natural organic materials where moisture or inadequate handling during harvest or storage creates conditions for fungal growth. We test for aflatoxins B1, B2, G1 and G2, ochratoxin A, deoxynivalenol, and zearalenone on origins where the risk profile warrants it. All results have returned below detection limits. We are working towards extending mycotoxin screening across all origins as part of our ongoing quality programme.
Solvent residues (Siberian Altai)
One of the most common adulteration methods in the shilajit market involves using organic solvents to extract or artificially concentrate fulvic acid content. We test for seven solvent compounds in our Siberian Altai. All returned below 10 mg/kg, the limit of detection for the method used. Clean solvent results are evidence of a genuine resin extraction process, not a solvent-assisted one.
Polycyclic aromatic hydrocarbons (PAHs) (Siberian Altai)
PAHs including benzo[a]pyrene, benzo[a]anthracene, benzo[b]fluoranthene and chrysene can enter shilajit through improper drying or heating during processing. All four returned below 0.2 mg/kg. These results are a processing integrity marker as much as a safety one.
Microbiology (Siberian Altai)
Coliforms, Salmonella, coagulase-positive staphylococci, and yeast and mould counts were all tested. Salmonella was not detected. All other counts returned below 10 cfu/g.
Water content
Water content affects concentration. A lower water content indicates a denser, more concentrated resin. Our results range from 2.57% in Hunza to 7.42% in Mongolian Altai. A drier, firmer resin is sometimes mistaken by customers for a lower quality product. In fact, the opposite is generally true.
Our results by origin
Siberian Altai
The Siberian Altai sits on some of the oldest exposed geology on earth, ancient Precambrian and Palaeozoic rock formations that have produced a shilajit with the broadest mineral spectrum of any origin we stock. The testing programme for this origin is our most comprehensive, covering humic substances, a full mineral and trace element profile, heavy metals, solvent residues, PAHs, and microbiology.
Humic substances (ISO 19822:2018)
| Compound | Result |
|---|---|
| Fulvic acids | 41.19% m/m |
| Humic acids | 5.8% m/m |
Mineral and trace element profile
| Compound | Result |
|---|---|
| Iron (Fe) | 923 mg/kg |
| Potassium (K) | 6.81% m/m |
| Calcium (Ca) | 3.39% m/m |
| Sodium (Na) | 570 mg/kg |
| Manganese (Mn) | 64 mg/kg |
| Boron (B) | 60 mg/kg |
| Magnesium (Mg) | 0.45% m/m |
| Phosphorus (P) | 0.17% m/m |
| Aluminium (Al) | 0.12% m/m |
| Zinc (Zn) | 21 mg/kg |
| Copper (Cu) | 9 mg/kg |
| Lithium (Li) | 6 mg/kg |
| Nickel (Ni) | 5 mg/kg |
| Chromium (Cr) | 4 mg/kg |
| Vanadium (V) | 2 mg/kg |
| Zirconium (Zr) | 1 mg/kg |
| Selenium (Se) | <1 mg/kg |
The iron content of 923 mg/kg is notably high and consistent with the ancient iron-rich rock of the Siberian Altai region. The breadth of the trace element profile, 20 compounds across minerals, trace elements and light metals, reflects the geological complexity of the source formation.
Heavy metals
| Compound | Result |
|---|---|
| Lead (Pb) | <0.2 mg/kg |
| Cadmium (Cd) | <0.2 mg/kg |
| Mercury (Hg) | <0.2 mg/kg |
| Arsenic (As) | 0.7 mg/kg |
Solvent residues
| Compound | Result |
|---|---|
| Methanol | <10 mg/kg |
| Pentane | <10 mg/kg |
| Ethanol | <10 mg/kg |
| Acetone | <10 mg/kg |
| Isopropanol | <10 mg/kg |
| Hexane | <10 mg/kg |
| Heptane | <10 mg/kg |
PAHs
| Compound | Result |
|---|---|
| Benzo[a]pyrene | <0.2 mg/kg |
| Benzo[a]anthracene | <0.2 mg/kg |
| Benzo[b]fluoranthene | <0.2 mg/kg |
| Chrysene | <0.2 mg/kg |
Microbiology
| Compound | Result |
|---|---|
| Coliforms | <10 cfu/g |
| Salmonella | Not detected |
| Staphylococcus (coagulase-positive) | <10 cfu/g |
| Yeast and mould | <10 cfu/g |
Certificate images
Minerals and trace elements
Solvents, microbiology and PAHs
Hunza (Gilgit-Baltistan, Karakoram Range)
Hunza Shilajit originates from the Karakoram range in Gilgit-Baltistan, one of the most geologically distinct mountain systems on earth, dominated by metamorphic and igneous rock including granite, gneiss and schist. The mineral signature of this origin reflects that geology: relatively lower calcium and sodium than the sedimentary Kashmir origin, and a mineral profile that is characteristically consistent with Karakoram geology.
The fulvic acid concentration of 64.13% under ISO 19822:2018 is the highest of any origin we stock. A high fulvic acid figure with a very low humic acid figure (1.16%) and a comparatively modest mineral profile suggests a more purified resin, one in which the purification process has concentrated fulvic acids at the partial expense of humic acids and some mineral content. If fulvic acid concentration is your primary consideration, this is our highest. If you value the full-spectrum composition of a less processed resin, the Kashmiri or Siberian Altai may suit you better. We think it is important to say that plainly.
Humic substances (ISO 19822:2018)
| Compound | Result |
|---|---|
| Fulvic acids | 64.13% w/w |
| Humic acids | 1.16% w/w |
Mineral profile
| Compound | Result |
|---|---|
| Phosphorus (P) | 134 mg/kg |
| Iron (Fe) | 115 mg/kg |
| Strontium (Sr) | 40 mg/kg |
| Boron (B) | 24 mg/kg |
| Aluminium (Al) | 20 mg/kg |
| Manganese (Mn) | 19 mg/kg |
| Barium (Ba) | 3 mg/kg |
| Zinc (Zn) | 2 mg/kg |
| Nickel (Ni) | 1 mg/kg |
| Copper (Cu) | <1 mg/kg |
| Calcium (Ca) | 0.40% w/w |
| Potassium (K) | 0.98% w/w |
| Magnesium (Mg) | 0.28% w/w |
| Sodium (Na) | 0.46% w/w |
Heavy metals (PCA accredited, ILAC-MRA)
| Compound | Result |
|---|---|
| Silver, cadmium, chrome, copper, nickel, lead, vanadium, mercury | Below working range |
| Iron (Fe) | 108 mg/kg |
| Manganese (Mn) | 27 mg/kg |
Mycotoxins (Nuscana Biotechnika Laboratoryjna, AB 1179)
| Compound | Result |
|---|---|
| Aflatoxin B1 | <0.05 µg/kg |
| Aflatoxin B2 | <0.050 µg/kg |
| Aflatoxin G1 | <0.05 µg/kg |
| Aflatoxin G2 | <0.050 µg/kg |
| Ochratoxin A | <0.5 µg/kg |
| Deoxynivalenol | <60 µg/kg |
| Zearalenone | <5 µg/kg |
Water content
| Compound | Result |
|---|---|
| Water content | 2.57% w/w |
The lowest of any origin we stock, indicating a dense, concentrated resin.
Overall condition: CorrectCertificate images
Humic substances and minerals
Heavy metals — PCA/ILAC-MRA
Water content
Mycotoxin screening — Nuscana
Kashmiri
The Kashmir Valley sits within a sedimentary basin formed from ancient limestone and sandstone deposited over millions of years. The organic matter that forms shilajit in this region carries the geochemical signature of those carbonate-rich formations, most visibly in the strontium content.
Strontium substitutes for calcium in carbonate minerals and is therefore characteristically elevated in shilajit from limestone-dominant geological environments. Our Kashmiri sample returned 364 mg/kg strontium, the highest of any origin we stock, and consistent with what you would expect from a genuine Kashmir Valley source. This is one of the clearest examples of how mineral data functions as a geographic fingerprint rather than simply a quality metric.
The humic to fulvic ratio of this origin, 18.59% humic against 44.87% fulvic, suggests a less aggressively processed resin that retains a fuller spectrum of humic substances alongside its fulvic acid content.
Humic substances (ISO 19822:2018)
| Compound | Result |
|---|---|
| Fulvic acids | 44.87% w/w |
| Humic acids | 18.59% w/w |
Mineral profile
| Compound | Result |
|---|---|
| Strontium (Sr) | 364 mg/kg |
| Boron (B) | 218 mg/kg |
| Phosphorus (P) | 117 mg/kg |
| Iron (Fe) | 141 mg/kg |
| Manganese (Mn) | 33 mg/kg |
| Zinc (Zn) | 7 mg/kg |
| Barium (Ba) | 7 mg/kg |
| Potassium (K) | 5.92% w/w |
| Calcium (Ca) | 2.85% w/w |
| Magnesium (Mg) | 1.63% w/w |
| Sodium (Na) | 0.73% w/w |
The boron content of 218 mg/kg is notably high, consistent with the sedimentary geology of the Kashmir region.
Heavy metals (PCA accredited, ILAC-MRA)
| Compound | Result |
|---|---|
| Silver, cadmium, chrome, copper, nickel, lead, vanadium, mercury | Below working range |
| Iron (Fe) | 101 mg/kg |
| Manganese (Mn) | 26 mg/kg |
| Zinc (Zn) | 5 mg/kg |
Mycotoxins (Nuscana Biotechnika Laboratoryjna, AB 1179)
| Compound | Result |
|---|---|
| Aflatoxin B1 | <0.05 µg/kg |
| Aflatoxin B2 | <0.050 µg/kg |
| Aflatoxin G1 | <0.05 µg/kg |
| Aflatoxin G2 | <0.050 µg/kg |
| Ochratoxin A | <0.5 µg/kg |
| Deoxynivalenol | <60 µg/kg |
| Zearalenone | <5 µg/kg |
Water content
| Compound | Result |
|---|---|
| Water content | 4.67% w/w |
Certificate images
Humic substances and minerals
Heavy metals — PCA/ILAC-MRA
Water content
Mycotoxin screening — Nuscana
Mongolian Altai (South)
The southern Mongolian Altai shares its name with the Siberian Altai but is geologically distinct. The differences in mineral composition between the two are a clear illustration of how even origins within the same mountain system can produce meaningfully different shilajit profiles.
The Mongolian Altai shows significantly higher sodium (867 mg/kg vs 570 mg/kg in Siberian), much higher phosphorus (644 mg/kg), and higher aluminium and manganese. The southern Mongolian section contains more sedimentary and volcanic rock influence than the ancient Precambrian formations of the Siberian north, and the shilajit composition reflects that distinction clearly.
The fulvic acid result of 54.91% sits between Hunza and the other two origins, with a humic acid content of 15.87% that indicates a reasonably full-spectrum resin.
Humic substances (ISO 19822:2018)
| Compound | Result |
|---|---|
| Fulvic acids | 54.91% w/w |
| Humic acids | 15.87% w/w |
Mineral profile
| Compound | Result |
|---|---|
| Sodium (Na) | 867 mg/kg |
| Phosphorus (P) | 644 mg/kg |
| Iron (Fe) | 292 mg/kg |
| Aluminium (Al) | 151 mg/kg |
| Boron (B) | 117 mg/kg |
| Manganese (Mn) | 54 mg/kg |
| Strontium (Sr) | 53 mg/kg |
| Zinc (Zn) | 20 mg/kg |
| Barium (Ba) | 13 mg/kg |
| Copper (Cu) | 9 mg/kg |
| Nickel (Ni) | 3 mg/kg |
| Potassium (K) | 5.36% w/w |
| Magnesium (Mg) | 1.17% w/w |
| Calcium (Ca) | 1.5% w/w |
Heavy metals (PCA accredited, ILAC-MRA)
| Compound | Result |
|---|---|
| Silver, cadmium, chrome, nickel, lead, vanadium, mercury | Below working range |
| Copper (Cu) | 6 mg/kg |
| Manganese (Mn) | 46 mg/kg |
| Zinc (Zn) | 15 mg/kg |
Water content
| Compound | Result |
|---|---|
| Water content | 7.42% w/w |
Certificate images
Humic substances and minerals
Heavy metals — PCA/ILAC-MRA
Water content
Ready to choose your origin? Browse our full range of Shilajit resin, each independently tested and sourced from its declared region.
Shop Shilajit ResinEkotechLAB Marek Klein S.K.A. is a specialist analytical chemistry laboratory based in Gdansk, Poland. They are not a generalised testing facility. The scientists who conduct our analyses are specialists in instrumental analysis, and the tests they produce are conducted in-house rather than outsourced to subcontractors.
Their heavy metals testing carries PCA accreditation (AB 1755), the Polish Centre for Accreditation, under the ILAC-MRA international mutual recognition arrangement. ILAC-MRA membership means the laboratory's accredited results are recognised as technically equivalent to those of accredited laboratories in over 100 countries worldwide.
We do not conduct our own testing or commission testing from laboratories with a commercial interest in the outcome. EkotechLAB has no affiliation with One Life Foods beyond providing analytical services.
If you have questions about our testing programme, the methods used, or the results presented here, you are welcome to contact us directly.


