2014
DOI: 10.5194/jsss-3-355-2014
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Development of a portable active long-path differential optical absorption spectroscopy system for volcanic gas measurements

Abstract: Abstract. Active long-path differential optical absorption spectroscopy (LP-DOAS) has been an effective tool for measuring atmospheric trace gases for several decades. However, instruments were large, heavy and powerinefficient, making their application to remote environments extremely challenging. Recent developments in fibre-coupling telescope technology and the availability of ultraviolet light emitting diodes (UV-LEDS) have now allowed us to design and construct a lightweight, portable, low-power LP-DOAS i… Show more

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Cited by 14 publications
(7 citation statements)
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“…The magmatic intrusion located 1-2 km of depth, and the magmatic storage at about 5-3 km, have been strongly influencing the shallow hydrothermal system, feeding the fumarolic field of the Grancratere of La Fossa, during the historical observation period. The remote sensing technique of passive DOAS (differential optical absorption spectroscopy), [54,55] allows the quantifying of different volcanic gases within the columns emitted from active volcanoes by collecting the spectra in the ultraviolet region (UV) in order to supply indirect measurements of magmatic volatiles [7,[56][57][58]. The DOAS method is based on the principles of absorption spectroscopy (Bouger-Beer-Lambert law) and is used for the quantification of different trace gases' concentrations (e.g., SO 2 , NO 2 , BrO).…”
Section: Geological and Volcanological Backgroundmentioning
confidence: 99%
“…The magmatic intrusion located 1-2 km of depth, and the magmatic storage at about 5-3 km, have been strongly influencing the shallow hydrothermal system, feeding the fumarolic field of the Grancratere of La Fossa, during the historical observation period. The remote sensing technique of passive DOAS (differential optical absorption spectroscopy), [54,55] allows the quantifying of different volcanic gases within the columns emitted from active volcanoes by collecting the spectra in the ultraviolet region (UV) in order to supply indirect measurements of magmatic volatiles [7,[56][57][58]. The DOAS method is based on the principles of absorption spectroscopy (Bouger-Beer-Lambert law) and is used for the quantification of different trace gases' concentrations (e.g., SO 2 , NO 2 , BrO).…”
Section: Geological and Volcanological Backgroundmentioning
confidence: 99%
“…This arrangement has two advantages: First, the light beam crosses the plume twice, thus doubling the sensitivity and second (and usually more important), all parts of the instrument, which require power are at one end of the light path, while only a passive reflector is at far end. Prerequisite for this approach is the availability of suitable sites on either side of the plume (e.g., two points at the crater rim) for mounting light source and detector or reflector (see e.g., [30,31]). In addition, the technique largely avoids the problems of the large background column density of e.g., H 2 O.…”
Section: Absorption Spectroscopy In the Uv/visiblementioning
confidence: 99%
“…The researchers in these fields have attempted to achieve high-sensitivity and portable monitoring. [32][33][34] Vita et al 32 could design and construct a lightweight, portable, and low-power long-path DOAS instrument for use at remote locations, specifically to measure the degassing from active volcanic systems, due to the developments in fiber-coupling telescope technology and the availability of UV light-emitting diodes (LEDs). Their instrument could measure SO 2 and potentially other trace gases through long open paths around volcanic vents.…”
Section: Differential Optical Absorption Spectroscopymentioning
confidence: 99%
“…The open paths have been used to increase the optical length in the applications. [32][33][34] However, these applications are unsuitable for detecting the decomposition products of SF 6 . The SF 6 -insulated electrical equipment is enclosed.…”
Section: Differential Optical Absorption Spectroscopymentioning
confidence: 99%