{'fraction_non_alphanumeric': 0.029565217391304348, 'fraction_numerical': 0.019130434782608695, 'mean_word_length': 4.811447811447811, 'pattern_counts': {'":': 0, '<': 2, '<?xml version=': 0, '>': 0, 'https://': 0, 'lorem ipsum': 0, 'www.': 0, 'xml': 0}, 'pii_count': 0, 'substrings_counts': 0, 'word_list_counts': {'cursed_substrings.json': 0, 'profanity_word_list.json': 0, 'sexual_word_list.json': 0, 'zh_pornsignals.json': 0}}
Role of Organics in Regulating ClNO₂ Production at the Air-Sea Interface.

We report measurements of the product yield for nitryl chloride (ClNO2) production following the reactive uptake of dinitrogen pentoxide (N2O5) to a wide variety of ambient seawater samples as well as seawater mimics. The ClNO2 yield, as measured for ambient seawater collected from both coastal and open ocean waters, was found to be both insensitive to chlorophyll-a, a marker for biological activity, and significantly lower (0.16-0.30) than that expected for equivalent salt-containing solutions (0.82 ± 0.05). Suppression in the ClNO2 yield can be induced by the addition of aromatic organic compounds (e.g., phenol and humic acid) to synthetic seawater matrices. In the case of phenol, surface tension measurements reveal that the surface phenol:chloride ratio can be enhanced by more than a factor of 100 as compared to bulk ratios for subtle changes in surface tension (<1.5 mN m(-1)), providing a mechanism to suppress ClNO2 production at low bulk phenol concentrations. We interpret measurements of the dependence of the ClNO2 yield on phenol using a kinetic model, where we confine the surface enhancement in phenol to the top 1 nm of the interface. Our results are most consistent with a model where N2O5 is ionized within the first three water monolayers (<1 nm), where the product nitronium ions react rapidly with interfacial phenol molecules. These results suggest that ClNO2 may not be formed at the air-sea interface at the yield expected for NaCl, and that the reactive uptake of N2O5 and the subsequent product yield of ClNO2 may serve as a unique probe for the composition of the interfacial region of the sea surface microlayer.