2020
DOI: 10.1016/j.firesaf.2020.102977
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Evaluation of gas and particle sensors for detecting spacecraft-relevant fire emissions

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Cited by 26 publications
(15 citation statements)
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“…Coincidence errors lead to inaccurate size and concentration measurements [118,119]. This problem can be partially overcome by combining single particle counting with photometry as implemented in the DustTrak DRX (TSI Inc., Shoreview, MN, USA), which measures size-segregated concentrations up to 400 mg/m 3 [53,120]. The light scattering signal depends not only on particle size, but also on particle refractive index and shape.…”
Section: Optical Particle Sizingmentioning
confidence: 99%
“…Coincidence errors lead to inaccurate size and concentration measurements [118,119]. This problem can be partially overcome by combining single particle counting with photometry as implemented in the DustTrak DRX (TSI Inc., Shoreview, MN, USA), which measures size-segregated concentrations up to 400 mg/m 3 [53,120]. The light scattering signal depends not only on particle size, but also on particle refractive index and shape.…”
Section: Optical Particle Sizingmentioning
confidence: 99%
“…5B), the comparison had a lower R 2 value (0.79) and higher RSME and MAE values (24.3 and 8.0 µg cm -3 , respectively). Although this comparison was low, previous studies have shown that the OPS and DustTrak measure similar PM10 values, under laboratory conditions (Wang et al, 2020) The PM concentration for sizes PM10, PM4, PM2.5, and PM1 were compared between the Grimm 11-D and DustTrak; there were 671 parallel hours. The R 2 values ranged from 0.63 (for PM10; values ranged from 5.3 µg cm -3 to 10.6 µg cm -3 , and the MAE values ranged from 3.3 µg cm -3 to 6.6 µg cm -3 .…”
Section: Intercomparison Of Aerosol Instruments Using Atmospheric Particlesmentioning
confidence: 95%
“…In the operation of the OPS, the particle density is assumed as 1 g cm -3 , and no information on the reflective index is added, as there is very limited knowledge of the atmospheric particle chemical and mineralogical composition in this region (Gill et al, 2000; and, therefore, no way to correctly capture the particles' density or refractive index, which are needed to convert the optical concentration to aerodynamic sizes. The OPS has been used previously in many laboratory settings (Ardon-Dryer et al, 2015;Yamada et al, 2015;Hsiao et al, 2016) and indoor experiments (Mølgaard et al, 2015;Maragkidou et al, 2018;Wang et al, 2020). Several studies that examined the performance of the OPS under diverse laboratory conditions have found it to be comparable with various reference units (Ardon-Dryer et al, 2015;Vasilatou et al, 2021).…”
Section: Instruments Used In the Aerosol Measurements Unitmentioning
confidence: 99%
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