In February 1801, the German physicist Johann Wilhelm Ritter observed that invisible rays just beyond the violet end of the visible spectrum darkened silver chloride-soaked paper more quickly than violet light itself. He announced this discovery in a brief letter to the Annalen der Physik and later called them "(de-)oxidizing rays" to emphasize chemical reactivity. The simpler term "chemical rays" was adopted soon afterwards and remained popular throughout the 19th century. Some scientists like John William Draper named them "tithonic rays," claiming they were entirely different from light. By 1878, researchers discovered the sterilizing effect of short-wavelength light by killing bacteria. In 1893, Victor Schumann made the discovery of ultraviolet radiation with wavelengths below 200 nm, which he named "vacuum ultraviolet" because it is strongly absorbed by oxygen in air. A committee of the Second International Congress on Light decided unanimously on the 17th of August 1932, at the Castle of Christiansborg in Copenhagen to divide UV into UVA, UVB, and UVC.
Spectral Subdivisions
The electromagnetic spectrum of ultraviolet radiation spans 10 to 400 nanometers and can be subdivided into ranges recommended by ISO standard ISO 21348. Ultraviolet A covers 315 to 400 nanometers and is known as long-wave or soft UV that is not absorbed by the ozone layer. Ultraviolet B spans 280 to 315 nanometers and is called medium-wave or intermediate UV that is mostly absorbed by the ozone layer. Ultraviolet C extends from 100 to 280 nanometers and is termed short-wave or hard UV that is completely absorbed by the ozone layer and atmosphere. Near ultraviolet ranges from 300 to 400 nanometers and is visible to birds, insects, and fish. Middle ultraviolet covers 200 to 300 nanometers while far ultraviolet spans 122 to 200 nanometers. Extreme ultraviolet occupies 10 to 121 nanometers and is entirely ionizing radiation by some definitions. Vacuum ultraviolet includes wavelengths from 10 to 200 nanometers that are strongly absorbed by atmospheric oxygen.