Initial interstellar detection HCNH+ was first detected in
interstellar space in 1986 toward the dense cloud
Sgr B2 using the
NRAO 12 m dish and the
Texas Millimeter Wave Observatory. These observations utilized the
J = 1–0, 2–1, and 3–2 pure rotational transitions at 74, 148, and 222 GHz, respectively.
Subsequent interstellar detections Since the initial detection, HCNH+ has also been observed in TMC-1 as well as DR 21(OH) The initial detection toward
Sgr B2 has also been confirmed. All 3 of these sources are dense molecular clouds, and to date HCNH+ has not been detected in diffuse interstellar material.
Solar System bodies While not directly detected via spectroscopy, the existence of HCNH+ has been inferred to exist in the atmosphere of
Saturn's largest moon,
Titan, based on data from the Ion and Neutral Mass Spectrometer (INMS) instrument aboard the
Cassini space probe. Models of Titan's atmosphere had predicted that HCNH+ would be the dominant ion present, and a strong peak in the mass spectrum at = 28 seems to support this theory. In 1997, observations were made of the long-period comet
Hale–Bopp in an attempt to find HCNH+, but it was not detected. However, the upper limit derived from these observations, along with the detections of
HCN,
HNC, and
CN, is important in understanding the chemistry associated with
comets. ==References==