Disintegrations per second to Rutherford

Because dps is literally what the instrument measures — a detector counts individual nuclear decay events over time. Calling it "dps" keeps the language grounded in what physically happened. Calling it "Bq" applies an SI label to the same number. Old lab protocols, standard operating procedures written before 1975, and some US-centric equipment manuals still use dps because nobody rewrote the paperwork. Numerically, 1 dps = 1 Bq, so the conversion is trivially multiplying by one.

Counts per second (cps) is what the detector actually registers; disintegrations per second (dps) is how many decays actually occurred. No detector catches every decay — some radiation misses the detector, some is absorbed before reaching it, and some types of radiation are invisible to certain detectors. The ratio of cps to dps is the detection efficiency, which can range from under 1% (for low-energy beta emitters in a Geiger tube) to over 90% (for gamma emitters in a well counter). Getting from cps to dps requires careful calibration.

The sample is dissolved in a scintillation cocktail — a solvent containing fluorescent molecules. Each beta particle or electron excites the cocktail, producing a flash of light detected by photomultiplier tubes. But chemical impurities in the sample absorb some of that light (a phenomenon called quenching), so the counter sees fewer flashes than decays. The instrument runs an internal or external standard to measure the quench level, then applies a correction curve to convert raw cpm to true dpm, which you divide by 60 to get dps.

Not numerically — they are identical. But contextually, "dps" emphasizes the physical measurement process and appears in lab protocols where you are calculating detector efficiency: "the source emits 10,000 dps and the detector reads 3,200 cps, so efficiency is 32%." Writing that sentence with Bq would be technically correct but odd, like referring to your morning coffee temperature in kelvin. The unit name signals what kind of work you are doing.

Before the becquerel was adopted in 1975, there was no named SI unit for radioactivity — scientists just said "disintegrations per second" or used the curie. The CGPM gave the name "becquerel" to one disintegration per second to honor Henri Becquerel and to bring radioactivity into the SI naming system alongside the gray and sievert. The dps description never went away; it just lost its status as the primary label. Think of it like saying "cycles per second" instead of "hertz" — correct, but dated.

The rutherford was proposed in the 1940s when the curie was the only game in town and was inconveniently large for many lab measurements. At 10⁶ dps (1 MBq), the rutherford sat in a useful range. But the 1975 SI reform chose the becquerel (1 dps) as the base unit with standard SI prefixes — kBq, MBq, GBq — which covered every scale. Having both the rutherford and the megabecquerel for the same quantity was redundant. The scientific community picked one, and the rutherford quietly disappeared from everything except unit conversion tables and physics trivia.

Rutherford discovered the atomic nucleus by firing alpha particles at gold foil (1911), identified alpha and beta radiation as distinct particle types, and performed the first artificial nuclear transmutation — turning nitrogen into oxygen — in 1917. He won the Nobel Prize in Chemistry in 1908, which famously annoyed him because he considered himself a physicist. His students went on to split the atom (Cockcroft and Walton) and discover the neutron (Chadwick). Nearly every branch of nuclear science traces back to his Manchester and Cambridge laboratories.

Several. The stat (1 disintegration per second, identical to the becquerel but proposed earlier), the eman (used for radon concentration in water, equal to 10⁻¹⁰ Ci/L), and the mache unit (another radon measure used in Austrian and German spa water literature) are all effectively extinct. The curie itself is technically obsolete under SI but persists through sheer institutional momentum in the US. The pattern is typical of measurement science: every era invents its own units, and standardisation eventually consolidates them.

Unlikely in practice because the rutherford disappeared from active use by the 1970s, before the megabecquerel entered common parlance in the 1980s. You would only encounter the rutherford in papers from roughly 1946–1970, primarily in European nuclear physics journals. If you see "Rd" in a modern unit conversion tool, it is there for completeness and historical interest, not because anyone is publishing in rutherfords. The real risk of confusion in old literature is between the curie and the becquerel, where a missing prefix can mean a billionfold error.

The "sunshine unit" — officially the strontium unit — was coined by the US Atomic Energy Commission in the 1950s to describe strontium-90 concentration in bones and milk during nuclear weapons testing. One sunshine unit equalled 1 picocurie of Sr-90 per gram of calcium. The name was a deliberate PR choice to make fallout contamination sound cheerful and harmless. It backfired spectacularly when journalists mocked it as Orwellian doublespeak, and the term was quietly dropped in favor of pCi/g Ca. It remains a cautionary tale about naming units for political rather than scientific reasons.