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Table 5

Upper limits of CN and H2O production rates and dust production rates of MBCs (Snodgrass et al. 2017a) compared to 66P.

Objects Q(H2 O) Q(CN) rh Q(H2O) Q(CN) References
(1026 molec s−1) (1024 molec s−1) (kg s−1) (au) (1026molec s−1) (1024molec s−1) (kg s−1)
133P 0.1 0.1 7.2 2.64 0.02 0.01 1.4 Licandro et al. (2011)
176P 2.6 0.5 2.58 0.40 0.1 de Val-Borro et al. (2012)
259P 1.3 0.4 1.86 0.50 0.14 Jewitt et al. (2009)
288P 6.1 2.6 2.3 2.52 1.00 0.42 0.5 Hsieh et al. (2012a)
313P 3.2 1.6 1.7 2.41 0.60 0.18 0.4 Jewitt et al. (2015)
324P 7.1 1.9 1.1 2.66 1.00 0.30 0.2 Hsieh et al. (2012b)
358P 2.7 0.8 4.3 2.42 0.50 0.15 1.0 Hsieh et al. (2013)
P/2013 R3 1.9 1.2 <3.5 2.23 0.43 0.12 <1.0(c) Jewitt et al. (2014a)

66P 27.1 7.5 55.0 1.29 27.1 7.5 55.0 This work

Notes. (a) Scaled water and CN production rates to rh = 1.29 au, using Q(gas) given by A’Hearn et al. (1995). (b) Scaled dust production rates to rh = 1.29 au, using the proxy relationship: , given by A’Hearn et al. (1995). (c)The empirical limit to the mass loss, from Jewitt et al. (2017).

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