Becquerel to Kilocurie

A single banana contains about 15 Bq of potassium-40, which led to the informal "banana equivalent dose" — a tongue-in-cheek way to put radiation exposure in perspective. It caught on because it makes an invisible phenomenon suddenly tangible. But the comparison has limits: your body tightly regulates potassium levels, so eating more bananas does not actually increase your internal K-40 inventory. You just excrete the excess.

The 1975 General Conference on Weights and Measures adopted the becquerel as part of the push to make all scientific measurement coherent under the SI system. The curie was awkwardly large (3.7 × 10¹⁰ disintegrations per second) and defined by a specific material — radium-226 — rather than a fundamental quantity. One becquerel equals exactly one decay per second, which is conceptually cleaner even if impractically small for everyday use.

A typical human body carries about 7,000–8,000 Bq from naturally occurring potassium-40 and carbon-14. This sounds alarming until you realize that activity (how many atoms decay per second) is not the same as dose (how much energy those decays deposit in tissue). The radiation from K-40 delivers roughly 0.17 millisieverts per year — a tiny fraction of the 2.4 mSv annual background. Your cells repair low-level DNA damage constantly; it is the rate and type of damage that matters, not the raw count of decays.

Becquerels count events — how many atoms disintegrate per second in a source. Sieverts measure the biological consequence of radiation absorbed by a person. A million-becquerel source locked in a lead safe delivers essentially zero sieverts to someone standing outside. The same source ingested could deliver a significant dose. You need to know the isotope, the radiation type, and the exposure pathway to go from Bq to Sv.

Bq/kg tells regulators exactly how many radioactive decays are occurring per second in each kilogram of food, which can then be converted to an ingestion dose using well-established dose coefficients for each isotope. The EU limit for caesium-137 in food after a nuclear accident is 1,250 Bq/kg; Japan set a much stricter 100 Bq/kg post-Fukushima. The unit is universal, isotope-neutral, and directly measurable with a gamma spectrometer — no assumptions about the consumer needed.

In 1987, scrap metal scavengers in Goiânia, Brazil broke open an abandoned caesium-137 teletherapy source containing about 1,375 Ci (50.9 TBq). The glowing blue Cs-137 powder fascinated locals — they rubbed it on skin, gave it to children, and spread it across multiple homes. Four people died, 249 were contaminated, and the cleanup produced 3,500 m³ of radioactive waste. The incident became the textbook case for why sealed sources must be tracked and securely stored throughout their entire lifecycle, and why the IAEA created its Code of Conduct on the Safety and Security of Radioactive Sources.

Yes, multiple times. In Ciudad Juárez, Mexico (1983), a stolen Co-60 teletherapy source was sold as scrap and melted into rebar, contaminating 4,000 tonnes of steel and exposing thousands. In Samut Prakan, Thailand (2000), a junked Co-60 source killed three scrap workers who pried it open. In Yanango, Peru (1999), a welder pocketed an Ir-192 industrial radiography source and carried it in his pocket for hours — his leg was amputated. The IAEA documents over 30 serious radiation accidents involving orphaned or stolen sources since the 1960s, collectively killing dozens and injuring hundreds.

Cobalt-60 has a 5.27-year half-life, so a 500 kCi source drops to 250 kCi after five years and becomes too weak for industrial throughput after about 15–20 years. The spent source pencils are returned to the manufacturer (typically in Canada or Russia) for reprocessing or secure storage. Transport uses heavily shielded Type B casks certified to survive a 9-meter drop and 30-minute fire. The manufacturer often offers a swap program: deliver fresh sources and take back decayed ones in the same shipment, minimising the number of high-activity transports.

The Fukushima Daiichi disaster released an estimated 10–30 PBq (10,000–30,000 TBq) of caesium-137 directly into the Pacific Ocean between March and July 2011 — the largest single marine radioactive release in history. For comparison, the Sellafield reprocessing plant in the UK discharged about 40 PBq of Cs-137 into the Irish Sea over decades of operation (1952–2000). Soviet dumping of entire reactor compartments from nuclear submarines in the Arctic added further inventory. Despite these numbers, ocean dilution is vast: Pacific Cs-137 levels from Fukushima peaked at about 50 Bq/m³ near the plant and dropped below 2 Bq/m³ within a few hundred kilometers.

This is exactly why the IAEA, NRC, and national agencies track high-activity sources so aggressively. A kilocurie Cs-137 or Co-60 source dispersed by conventional explosives would contaminate a few city blocks — not causing acute radiation casualties (the blast itself is deadlier) but creating a costly, panic-inducing cleanup lasting months. The actual health risk to the public would be low, but the economic and psychological damage would be enormous. Post-9/11 programs like the US GTRI (now NNSA OSRP) have recovered or secured thousands of orphaned high-activity sources worldwide.