Due to the massive size of its nucleus, Comet Hale–Bopp was observed intensively by
astronomers during its perihelion passage, and several important advances in cometary science resulted from these observations. The dust production rate of the comet was very high (up to 2.0 kg/s), which may have made the inner coma
optically thick. Based on the properties of the dust grainshigh temperature, high
albedo and strong 10 μm silicate emission featurethe astronomers concluded the dust grains are smaller than observed in any other comet. Hale–Bopp showed the highest ever linear polarization detected for any comet. Such polarization is the result of solar radiation getting scattered by the dust particles in the coma of the comet and depends on the nature of the grains. It further confirms that the dust grains in the coma of comet Hale–Bopp were smaller than inferred in any other comet.
Sodium tail One of the most remarkable discoveries was that the comet had a third type of tail. In addition to the well-known gas and dust tails, Hale–Bopp also exhibited a faint
sodium tail, only visible with powerful instruments with dedicated filters. Sodium emission had been previously observed in other comets, but had not been shown to come from a tail. Hale–Bopp's sodium tail consisted of
neutral atoms (not
ions), and extended to some in length. The source of the sodium appeared to be the inner
coma, although not necessarily the
nucleus. There are several possible mechanisms for generating a source of sodium atoms, including collisions between dust grains surrounding the nucleus, and "sputtering" of sodium from dust grains by
ultraviolet light. It is not yet established which mechanism is primarily responsible for creating Hale–Bopp's sodium tail, and the narrow and diffuse components of the tail may have different origins. While the comet's dust tail roughly followed the path of the comet's orbit and the gas tail pointed almost directly away from the Sun, the sodium tail appeared to lie between the two. This implies that the sodium atoms are driven away from the comet's head by
radiation pressure.
Deuterium abundance The abundance of
deuterium in comet Hale–Bopp in the form of
heavy water was found to be about twice that of Earth's oceans. If Hale–Bopp's deuterium abundance is typical of all comets, this implies that although cometary impacts are thought to be the source of a significant amount of the
water on Earth, they cannot be the only source. Deuterium was also detected in many other
hydrogen compounds in the comet. The ratio of deuterium to normal hydrogen was found to vary from compound to compound, which astronomers believe suggests that cometary ices were formed in
interstellar clouds, rather than in the
solar nebula. Theoretical modelling of ice formation in interstellar clouds suggests that comet Hale–Bopp formed at temperatures of around 25–45
kelvin. ( –414 to –387 Fahrenheit / –248 to –233 Celsius).
Organics Spectroscopic observations of Hale–Bopp revealed the presence of many
organic chemicals, several of which had never been detected in comets before. These complex molecules may exist within the cometary nucleus, or might be synthesised by reactions in the comet.
Detection of argon Hale–Bopp was the first comet where the
noble gas argon was detected. Noble gases are chemically inert and vary from low to high
volatility. Since different noble elements have different
sublimation temperatures, and don't interact with other elements, they can be used for probing the temperature histories of the cometary ices.
Krypton has a sublimation temperature of 16–20 K (−430 to −423 Fahrenheit/ −257 to −253 Celsius) and was found to be depleted more than 25 times relative to the solar abundance, while argon with its higher sublimation temperature was enriched relative to the solar abundance. Together these observations indicate that the interior of Hale–Bopp has always been colder than 35–40 K (−396 to −387 Fahrenheit / −238 to −233 Celsius), but has at some point been warmer than 20 K (−423 Fahrenheit / −253 Celsius). Unless the solar nebula was much colder and richer in argon than generally believed, this suggests that the comet formed beyond Neptune in the
Kuiper belt region and then migrated outward to the
Oort cloud.
Rotation Comet Hale–Bopp's activity and outgassing were not spread uniformly over its nucleus, but instead came from several specific jets. Observations of the material streaming away from these jets allowed astronomers to measure the rotation period of the comet, which was found to be about 11 hours 46 minutes.
Binary nucleus question In 1997 a paper was published that hypothesised the existence of a binary
nucleus to fully explain the observed pattern of comet Hale–Bopp's dust emission observed in October 1995. The paper was based on theoretical analysis, and did not claim an observational detection of the proposed satellite nucleus, but estimated that it would have a diameter of about , with the main nucleus being about across, and would orbit in about three days at a distance of about . This analysis was confirmed by observations in 1996 using Wide-Field Planetary Camera 2 of the
Hubble Space Telescope which had taken images of the comet that revealed the satellite. Although observations using
adaptive optics in late 1997 and early 1998 showed a double peak in the brightness of the nucleus, controversy still exists over whether such observations can only be explained by a binary nucleus. The discovery of the satellite was not confirmed by other observations. Also, while comets have been observed to break up before, no case had been found of a stable binary nucleus until the subsequent discovery of the cometary nature of P/2006 VW139| in 2016. == UFO claims ==