1 2 New techniques have recently been developed to capture reactive nitrogen species for 3 accurate measurement of their isotopic composition. Reactive nitrogen species play 4 important roles in atmospheric oxidation capacity (hydroxyl radical and ozone formation) 5 and may have impacts on air quality and climate. Tracking reactive nitrogen species and 6 their chemistry in the atmosphere based upon concentration alone is challenging. Isotopic 7 analysis provides a potential tool for tracking the sources and chemistry of species such 8 as nitrogen oxides (NO x = NO + NO 2 ), nitrous acid (HONO), nitric acid (HNO 3 ) and 9 particulate nitrate (NO 3 -(p)). Here we study direct biomass burning (BB) emissions 10 during the Fire Influence on Regional to Global Environments Experiment (FIREX, later 11 evolved into FIREX-AQ) laboratory experiments at the Missoula Fire Laboratory in the 12 fall of 2016. 13 14 An annular denuder system (ADS) developed to efficiently collect HONO for isotopic 15 composition analysis was deployed to the Fire Lab study. Concentrations of HONO 16 recovered from the ADS collection agree well with mean concentrations averaged over 17 each fire measured by 4 other high time resolution techniques, including mist 18 chamber/ion chromatography (MC/IC), open-path Fourier transform infrared 19 spectroscopy (OP-FTIR), cavity enhanced spectroscopy (CES), proton-transfer-reaction 20 time-of-flight mass spectrometer (PTR-ToF). The concentration validation ensures 21 complete collection of BB emitted HONO, of which the isotopic composition is 22preserved during the collection process. In addition, the isotopic composition of NO x and 23 NO 3 -(p) from direct BB emissions were also characterized. 24In 20 "stack" fires (direct emission within ~5 seconds of production by the fire) that 25 burned various biomass materials, δ 15 N-NO x ranges from -4.3 ‰ to +7.0 ‰, falling near 26 the middle of the range reported in previous work. The first measurements of δ 15 N-27HONO and δ 18 O-HONO in biomass burning smoke reveal a range of -5.3 -+5.8 ‰ and 28 +5.2 -+15.2 ‰ respectively. Both HONO and NO x are sourced from N in the biomass 29 fuel and δ 15 N-HONO and δ 15 N-NO x are strongly correlated (R 2 = 0.89, p<0.001), 30suggesting NO x and HONO are connected via formation pathways. 31 32Our δ 15 N of NO x , HONO and NO 3 -(p) ranges can serve as important biomass burning 33 source signatures, useful for constraining direct emissions of these species in 34 environmental applications. The δ 18 O of HONO and NO 3 obtained here verify our 35 method is capable of determining oxygen isotopic composition in BB plumes. The δ 18 O 36for both species in this study reflect the laboratory conditions (i.e. a lack of 37 photochemistry), and would be expected to track with the influence of ozone (O 3 ), 38 photochemistry and nighttime chemistry in real environments. The methods used in this 39 study will be further applied in future field studies to quantitatively track reactive 40 nitrogen cycling in fresh and aged Western US wild...