Subscriber access provided by TUFTS UNIV
Environmental Processes
Time-Resolved Measurements of Nitric Oxide, Nitrogen Dioxide, and Nitrous Acid in an Occupied New York Home Shan Zhou, Cora J Young, Trevor Casey VandenBoer, Shawn Finley Kowal, and Tara F Kahan Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.8b01792 • Publication Date (Web): 05 Jul 2018 Downloaded from http://pubs.acs.org on July 7, 2018
Just Accepted “Just Accepted” manuscripts have been peer-reviewed and accepted for publication. They are posted online prior to technical editing, formatting for publication and author proofing. The American Chemical Society provides “Just Accepted” as a service to the research community to expedite the dissemination of scientific material as soon as possible after acceptance. “Just Accepted” manuscripts appear in full in PDF format accompanied by an HTML abstract. “Just Accepted” manuscripts have been fully peer reviewed, but should not be considered the official version of record. They are citable by the Digital Object Identifier (DOI®). “Just Accepted” is an optional service offered to authors. Therefore, the “Just Accepted” Web site may not include all articles that will be published in the journal. After a manuscript is technically edited and formatted, it will be removed from the “Just Accepted” Web site and published as an ASAP article. Note that technical editing may introduce minor changes to the manuscript text and/or graphics which could affect content, and all legal disclaimers and ethical guidelines that apply to the journal pertain. ACS cannot be held responsible for errors or consequences arising from the use of information contained in these “Just Accepted” manuscripts.
is published by the American Chemical Society. 1155 Sixteenth Street N.W., Washington, DC 20036 Published by American Chemical Society. Copyright © American Chemical Society. However, no copyright claim is made to original U.S. Government works, or works produced by employees of any Commonwealth realm Crown government in the course of their duties.
Page 1 of 35
Environmental Science & Technology
1
Time-Resolved Measurements of Nitric Oxide, Ni-
2
trogen Dioxide, and Nitrous Acid in an Occupied
3
New York Home
4 5
Shan Zhou1, Cora J. Young 2, Trevor C. VandenBoer 2, Shawn F. Kowal1, Tara F. Kahan1,*
6
1
Department of Chemistry, Syracuse University, Syracuse, NY, USA
7
2
Department of Chemistry, York University, Toronto, ON, Canada
8
*
Corresponding Author: Tara Kahan,
[email protected], (315) 443-3285, Department of Chemis-
9
try, Syracuse University, Syracuse, NY 13244
10 11
KEYWORDS
12
Photochemistry, air exchange rate (AER), indoor air quality, oxidants, combustion, photon flux
13 14
ABSTRACT
15
Indoor oxidizing capacity in occupied residences is poorly understood. We made simultaneous
16
continuous time-resolved measurements of ozone (O3), nitric oxide (NO), nitrogen dioxide
17
(NO2), and nitrous acid (HONO) for two months in an occupied detached home with gas appli-
18
ances in Syracuse, New York. Indoor NO and HONO mixing ratios were higher than those out-
19
doors, whereas O3 was much lower (sub-ppbv) indoors. Cooking led to peak NO, NO2, and
20
HONO levels 20 - 100 times greater than background levels; HONO mixing ratios of up to 50
21
ppbv were measured. Our results suggest that many reported NO2 levels may have a large posi1 ACS Paragon Plus Environment
Environmental Science & Technology
22
tive bias due to HONO interference. Nitrous acid, NO2, and NO were removed from indoor air
23
more rapidly than CO2, indicative of reactive removal processes or surface uptake. We measured
24
spectral irradiance from sunlight entering the residence through glass doors; hydroxyl radical
25
(OH) production rates of (0.8 – 10) × 107 molec cm-3 s-1 were calculated in sunlit areas due to
26
HONO photolysis, in some cases exceeding rates expected from ozone-alkene reactions. Steady
27
state nitrate radical (NO3) mixing ratios indoors were predicted to be lower than 1.65 × 104 molec
28
cm-3. This work will help constrain the temporal nature of oxidant concentrations in occupied
29
residences and will improve indoor chemistry models.
30 31
TOC Art
32 33
INTRODUCTION
34
Considering that people typically spend 90% of their time indoors (and 80% of that time in
35
residences), air quality in residences is of major concern for human health.1 In addition to direct
36
indoor sources and infiltration from the ambient atmosphere, harmful pollutants can be formed
37
indoors through in-situ secondary chemistry initiated by oxidants.2-5 Yet our understanding of
38
indoor oxidation processes, especially in occupied residences, lags substantially behind that for
39
outdoors.
2 ACS Paragon Plus Environment
Page 2 of 35
Page 3 of 35
Environmental Science & Technology
40
The hydroxyl radical (OH) is the most important oxidant in the atmosphere. In indoor envi-
41
ronments, OH levels are expected to be much lower than those outdoors because the primary pro-
42
duction mechanism (ozone photolysis) does not occur.6 The primary indoor OH source is thought
43
to be non-photochemical reactions between ozone and alkenes.7-8 Recent studies suggest that pho-
44
tolysis of nitrous acid (HONO), formaldehyde, and hypochlorous acid (HOCl, which is generated
45
during cleaning events using commercial bleach solution) can also be a source of indoor OH.9-15
46
Nitrate radicals (NO3) have also been suggested to be potentially important oxidants indoors.4, 16
47
There are few indoor measurements of reactive species such as OH and NO3, and none in resi-
48
dences.17-18 Even levels of more stable oxidants are not well constrained in residences because
49
most measurements have been performed in non-residential buildings; lower air exchange rates
50
(AER) in residences may result in very different oxidant mixing ratios, as indoor levels can de-
51
pend strongly on AER. For example, ozone is thought to be the most important oxidant in indoor
52
environments, but some studies suggest that ozone levels in residences may be very low, likely
53
due to low AER, adsorption to surfaces, and titration by nitric oxide (NO).19-20
54
Nitrous acid is an emerging household oxidant that may be an important indoor photochemi-
55
cal OH source.10, 12, 14-15, 21 It can be emitted directly in indoor settings by combustion processes
56
such as burning candles, open fireplaces, gas stoves, and cigarette smoking.14, 22-23 Heterogeneous
57
reactions of nitrogen dioxide (NO2) also lead to the secondary formation of HONO.24 However,
58
there have been limited HONO measurements in residences and its indoor mixing ratio is subject
59
to high levels of uncertainty. Peak HONO mixing ratios (15 min time resolution) of up to 100
60
ppbv and 24 h averages of 40 ppbv were measured in controlled house experiments.25 Measure-
61
ments made in real homes yielded much lower mean (1 – 7 days) HONO mixing ratios ranging
62
from 0.8 to 11.3 ppbv.23, 26-28 In addition, most existing measurements of the important HONO
63
precursor NO2 have been made with passive samplers that are exposed to the indoor environment 3 ACS Paragon Plus Environment
Environmental Science & Technology
64
for extended periods of time (1 to 14 days). Such extended sampling periods are unlikely to cap-
65
ture short-term peak levels and temporal changes in mixing ratios, which are important for under-
66
standing chemistry that occurs indoors. Furthermore, it has been shown that HONO interferes
67
with most NO2 measurement methods used indoors.29-30 This suggests that many reported indoor
68
NO2 values may be positively biased, further confounding the relative importance of NO2 and
69
HONO in residences.
70
In this study, we conduct time-resolved measurements of a suite of oxidants and oxidant pre-
71
cursors including O3, NO, NO2, and HONO in an occupied residence to better characterize their
72
mixing ratios, sources, and sinks. We also measure spectral irradiance from sunlight entering the
73
residence, and calculate OH production rates from HONO photolysis as well as steady-state NO3
74
concentrations under various conditions.
75 76
EXPERIMENTAL METHODS
77
Research House
78
From September 27 to November 20, 2017, continuous ambient sampling of indoor air was
79
made in a single-family dwelling in Syracuse, NY. Located in an urban residential area, it is a 4-
80
bedroom 1.5 story house (250 m3 volume) with an unfinished basement and a detached garage.
81
The house utilizes both natural ventilation (opening windows) and forced-air system (heating or
82
air-conditioning) using 100% recirculated air. Most floors are hardwood; the family room has a
83
mixture of carpet and bamboo flooring. Illumination is primarily provided by LED lights and
84
sunlight filtered through windows. Combustion appliances include a natural gas stove with four
85
burners and an oven. Water heater, heating, and air conditioning systems were also operated us-
86
ing commercial natural gas supplied to the house. During the sampling period, the house was oc-
4 ACS Paragon Plus Environment
Page 4 of 35
Page 5 of 35
Environmental Science & Technology
87
cupied by two non-smoking adults, one child, and a dog. Daily activity was carried out normally
88
and a human activity log book was kept at the residential site.
89
Real-Time Measurements
90
A custom-built mobile analytical laboratory (Mobile Indoor Laboratory for Oxidative Spe-
91
cies; MILOS) was deployed for time-resolved measurements of O3, NO, NO2, HONO, carbon
92
dioxide (CO2), relative humidity (RH), and temperature (T). Ozone mixing ratios were measured
93
by an Ecotech Serinus 10 UV photometric analyser (accuracy of 0.5 ppbv or 2% of reading). Ox-
94
ides of nitrogen (NOx: NO and NO2) were measured using an Ecotech Serinus 40 O3-based chem-
95
iluminescence analyser (accuracy of 0.4 ppbv or 0.5% of reading). The NOx analyser was modi-
96
fied to allow simultaneous quantitative measurements of HONO by a difference technique.30 A
97
HONO inlet consisting of a gas denuder (GD) channel and a bypass (BP) channel was inserted
98
upstream of the NOx analyser. The GD removes gaseous acids including HONO using a sodium
99
carbonate-coated annular denuder (URG Corp.), but does not remove NO2. The denuder was pre-
100
pared by coating the interior with a saturated aqueous Na2CO3 solution (Fisher Scientific), shak-
101
ing gently, pouring out the excess solution, and drying with zero air for ~5 min. Air sampled
102
through the BP contains NO2 and HONO; both molecules are converted to NO by the molyb-
103
denum-catalyst.25, 30-32 A Teflon solenoid three-way valve enabled the sampling of GD (NO2 on-
104
ly) and BP (sum of NO2 and HONO, Σ(NO2+HONO)) air alternating at 5 min intervals. Distinct
105
measurements of NO2 and HONO (rather than the sum of the two species) were made after
106
October 31. CO2, RH, and temperature indoors were monitored with a TSI IAQ7545. Data were
107
logged at 30 s intervals for all measurements. For NO2 and HONO, during each 5-min interval,
108
the first 1 minute of data was excluded to reject data influenced by the instrument response time.
109
Data acquired over the remaining 4 minutes was averaged. MILOS was stationed in the living
110
room while its Teflon sampling inlet was positioned in the kitchen or living room at head height 5 ACS Paragon Plus Environment
Environmental Science & Technology
111
(approximately 1.5 m above the floor). Outdoor mixing ratios were measured intermittently
112
throughout the sampling period by moving the inlet to the patio or front stoop, generally during
113
the day. Outdoor temperature (Tout) and relative humidity (RHout) at Syracuse Hancock Interna-
114
tional Airport, ~7.3 km north to the sampling site, were retrieved from the NOAA National Cen-
115
ters for Environmental Information’s Integrated Surface Hourly Database.33
116
Calibration and Quality Control
117
Given low nitric acid (HNO3) levels previously reported in residences,25, 34 its interference to
118
NO2 and HONO measurements is considered negligible in this study. The conversion efficiency
119
of HONO by the molybdenum catalyst was determined by introducing zero air containing
120
HONO, generated using a custom-built apparatus,35 into the NOx analyser and comparing the
121
level reported by the NOx analyser to the mixing ratio measured offline using ion chromatog-
122
raphy with conductivity detection. The conversion efficiency was determined to be to be (83.5 ±
123
3)%. Previous studies have shown that small amounts of NO2 can adsorb to annular denuders.36-37
124
We flowed NO2 ranging from 13 to 270 ppbv through the GD line and NO2 losses were found to
125
be (7.0 ± 0.45)%. Reported values were corrected to account for the conversion efficiency and
126
loss.
127
Calibrations and linearity checks were performed at the beginning, middle, and end of the
128
sampling period using a dilution calibrator and ozone generator (Ecotech GasCal 1100) and NO
129
cylinder (19.8 ppmv in N2, analytical uncertainty of 5%). The 30 s limit of detection (LOD) of the
130
analytes were determined as 3 times the standard deviations (3σ) of the corresponding signals in
131
zero air. Limits of detection were 0.63, 1.1, 1.3, and 1.3 ppbv for O3, NO, NO2, and
132
Σ(NO2+HONO), respectively. Higher LODs for NO, NO2, and HONO than for O3 are due to the
133
use of different digital filters. The 5 min LOD for HONO was calculated as 0.7 ppbv, 3 times the
134
standard deviation propagated from the subtraction of 5 min NO2 from Σ(NO2+HONO). The en6 ACS Paragon Plus Environment
Page 6 of 35
Page 7 of 35
Environmental Science & Technology
135
durance of the GD was tested and the annular denuder was recoated on average every day (6
136
hours – 4 days depending on accessibility) to minimize the influence of denuder deactivation on
137
NO2 and HONO mixing ratios. Time periods potentially influenced by denuder deactivation were
138
identified based on decreasing HONO/NO2 ratios.
139
Data Analysis
140
The decay (removal) rate constants (k) of NO, NO2, HONO, and CO2 were estimated from
141
indoor measurements during periods affected by a dominant indoor source (e.g. cooking). Only
142
time periods when all species peaked at concentrations significantly higher than the background
143
values, followed by a non-source period, were considered in the calculations. Assuming constant
144
removal rates and background mixing ratios during the decay period, and assuming an even dis-
145
tribution of indoor concentrations of these species,
146
Ct = e-kt Co + Cb
147
where Ct is the indoor mixing ratio after time t, Co is the initial (peak) mixing ratio, and Cb is the
148
background mixing ratio of the analyte gas during the decay event. The decay rate constant was
149
determined using an exponential regression of the observed mixing ratio versus time for each
150
decay period. Decay rate constant error was determined as the standard error of k obtained from
151
the regression. Time periods for CO2 decay calculations were identified based on stringent crite-
152
ria to exclude potential impacts from occupant emissions (see the Supplementary Information for
153
details).
154
Light Measurements and Photolysis Rate Calculations
[1]
155
Wavelength-resolved spectra of sunlight entering the residence through double-paned patio
156
doors (4.8 m2) leading to a deck off of the south-facing family room were acquired using a cali-
157
brated Ocean Optics USB4000 spectrometer coupled to a 1 m fiber optic cable and a cosine cor-
158
rector. Full details of the measurement procedure and data analysis are described in Kowal et al.12 7 ACS Paragon Plus Environment
Environmental Science & Technology
Page 8 of 35
159
In brief, 3 background-subtracted spectral irradiances of sunlight indoors were measured with 1.5
160
ms integration. Average spectral irradiances were calculated, and photon fluxes (F) were estimat-
161
ed. These measurements were acquired on September 21, 2017 at approximately noon; the sky
162
was cloudless and the solar zenith angle was 41.4°.38
163
HONO photolysis rate constants (JHONO) were calculated as described previously using meas-
164
ured photon fluxes and reported absorption cross sections (σ) and photolysis quantum yields
165
(ϕ).12
166 ఒ
ܬுைேை = න ߪுைேை ሺߣሻ߶ுைேை ሺߣሻܨఒ ݀ߣ
[2]
ఒ
167
Rate constants were then multiplied by measured indoor HONO concentrations to calculate OH
168
production rates.
ܴܽܬ = ݁ݐுைேை ሾܱܱܰܪሿ
[3]
169 170
RESULTS and DISCUSSION
171
Outdoor temperature (Tout) ranged from -8.3 to 32.2 ºC and RHout ranged from 29 to 100%,
172
with means (± 1σ) of 9.8 ± 7.6 ºC and 78.4 ± 17.2%, respectively. Precipitation occurred 22% of
173
the time throughout the study period as rain or snow. The indoor environment was generally
174
warmer (average temperature of 20.5 ± 1.2 ºC) and drier (average RH of 44.5 ± 5.7%), with little
175
temporal variation in T and RH. Figure 1 shows a sector of the real-time temperature, RH, and
176
gas species mixing ratios measured indoors during the sampling period. The time series over the
177
entire sampling period are shown in Fig. S1. Mixing ratios of all species varied dynamically with
178
high amplitudes (Fig. S1). Ozone levels indoors were often below the detection limit (58% of the
179
observation period), whereas outdoor levels of up to 34.2 ppbv were measured. 8 ACS Paragon Plus Environment
Page 9 of 35
180
Environmental Science & Technology
Mixing Ratios under Background Conditions
181
Indoor background oxidant mixing ratios during periods without emission sources (i.e., doors
182
closed, no cooking or heating events) were examined to obtain a baseline of mixing ratios indoors.
183
Nitric oxide mixing ratios were much higher indoors than outdoors, with an average (± 1σ) in-
184
door background mixing ratio of 4.0 ± 2.5 ppbv. Most (70%) outdoor NO levels were below the
185
LOD. Using the LOD as an upper limit for the NO mixing ratio under these conditions, we esti-
186
mated a lower limit for the background indoor/outdoor (I/O) ratio of 2.1. Comparable average
187
levels of the sum of NO2 and HONO (Σ(NO2+HONO)) were observed under indoor background
188
conditions and outdoors (5.4 vs 5.2 ppbv). The average (± 1σ) indoor background NO2 and
189
HONO mixing ratios (acquired after October 31, excluding periods with potential influence from
190
denuder passivation) were 2.0 ± 0.68 and 4.3 ± 2.2 ppbv, respectively. Note that we had very lim-
191
ited outdoor distinct measurements of NO2 and HONO; their outdoor levels are not reported. Alt-
192
hough outdoor HONO mixing ratios can be variable, they are typically on the order of 1 – 2 ppbv
193
at night and sub-ppbv at midday.39 This is suggestive of higher HONO levels indoors under
194
background conditions than outdoors, in agreement with previous studies.23,
195
above its detection limit, its average background mixing ratio was 1.0 ppbv, significantly lower
196
than the outdoor levels measured (mean of 12.6 ppbv, Fig. S2).
28
When O3 was
197
The observed complex relationship between the indoor background and outdoor oxidant lev-
198
els reflect different source and sink strengths. Direct emission from traffic is the dominant source
199
of NOx in ambient urban environments. As shown in Fig. S2, outdoor NO mixing ratios peaked at
200
6 – 8 EST (12 ppbv) and 16 – 20 EST (6 ppbv). However, during the daytime with high ambient
201
ozone levels (~20 ppbv, Fig. S2), which convert NO to NO2, ambient NO levels ranged from 2
202
ppbv to below the LOD. A similar, yet less pronounced, diurnal profile was also observed for
203
ambient Σ(NO2+HONO) (Fig. S2), likely corresponding to rush-hour traffic emissions of NOx. 9 ACS Paragon Plus Environment
Environmental Science & Technology
204
Nitrous acid on the other hand is photolyzed rapidly by sunlight, so its ambient outdoor concen-
205
tration is quite low during the day, and measured outdoor Σ(NO2+HONO) levels during the day
206
are likely almost entirely due to NO2.
207
Significantly higher NO and HONO mixing ratios indoors compared to outdoors suggest that
208
transport of outdoor NO and HONO by air infiltration were likely not the primary indoor sources
209
of these species. This is supported by the absence of rush-hour peaks for indoor levels. Combus-
210
tion processes indoors, e.g. biomass, incense, and candle burning, gas cooking, and smoking,
211
have been shown as major direct sources of NOx and HONO in indoor environments.14, 40-42 Gas
212
cooking is likely the main indoor HONO source in the current study. Elevated concentrations of
213
NO and HONO throughout the study period (including in the absence of combustion) are likely
214
due to weaker sinks for these species indoors; low O3 in the case of NO and reduced photolysis
215
indoors in the case of HONO. Since surface area to volume ratios are generally greater indoors
216
than outdoors, heterogeneous reactions of NO2 may be more important indoors, and may have
217
contributed to higher indoor background HONO levels.43
218
In addition to indoor sources (e.g. combustion), infiltration of NO2 from outdoor air also con-
219
tributes to indoor NO2 levels.40, 44 Transport of ambient O3 is the dominant source of indoor O3,
220
which often is present at mixing ratios 10 – 80% of ambient outdoor values, depending on the
221
AER.45 Our observations of lower background mixing ratios of NO2 and O3 indoors are consistent
222
with outdoor-to-indoor transport of these species. Weak indoor production of NO2 from the reac-
223
tion of NO and O3 due to low levels of indoor O3 may account for low background indoor NO2
224
mixing ratios. Strong sinks – e.g. NO2 deposition to indoor surfaces and O3 titration by NO – may
225
have also contributed to lower NO2 and O3 mixing ratios indoors compared to outdoors in the
226
absence of direct sources.
227
Mixing Ratios Influenced by Cooking 10 ACS Paragon Plus Environment
Page 10 of 35
Page 11 of 35
Environmental Science & Technology
228
Indoor mixing ratios of NO frequently exceeded 100 ppbv, and occasionally reached 340
229
ppbv, 2 orders of magnitude higher than background levels (Fig. S1c). Dramatically higher in-
230
door mixing ratios of NO2 and HONO than the background values were also observed, peaking at
231
59 and 50 ppbv (Fig. S1c), which correspond to mixing ratios approximately 30 and 12 times
232
higher than background levels, respectively. These peak episodes correspond to cooking events,
233
as suggested in Fig. 1c. The average diurnal variations of indoor NO, NO2, and HONO during
234
this study also showed three recurring spikes corresponding to meal times at ~ 8 – 9, 12 – 14, and
235
16 – 19 EST with the highest levels occurring around supper time (Fig. S3). These observations
236
together suggest that direct emission from gas cooking was the major source of NOx and HONO
237
in this residence. Reactions involving NO2 likely also contribute to HONO formation during
238
cooking events.22 Our measurements do not have the temporal resolution required to distinguish
239
between primary and secondary HONO formation.
240
Statistics of maximum 5 min peak concentrations during cooking events are presented in
241
Fig. 2 and Table 1; means (± 1σ) were 113.2 ± 72.7, 17.3 ± 12.8, and 19.5 ± 10.5 ppbv for NO,
242
NO2, and HONO, respectively. These values are significantly higher than the mixing ratios meas-
243
ured under background conditions as well as those measured outdoors. Peak NO mixing ratios are
244
in agreement with those observed in other residences (~40 – 300 ppbv) but significantly lower
245
than those measured during controlled cooking experiments (100 – 2000 ppbv).22, 46-48 The peak
246
NO2 levels in this study were generally at the low end of the concentration range previously re-
247
ported (~20 – 550 ppbv),22,
248
ppbv).22
46, 48
whereas peak HONO levels were on the high end (3 – 16
249
As shown in Fig. 1c, when cooking appliances were in use, mixing ratios of combustion by-
250
products (NO, NO2, and HONO) rapidly rose. The rise time of the signal corresponded to the
251
time the appliance was on (i.e. cooking duration) which varied between 4 and 86 minutes in this 11 ACS Paragon Plus Environment
Environmental Science & Technology
Page 12 of 35
252
field study. After the appliance was turned off, the levels rapidly reached peak levels and slowly
253
decayed away. To investigate possible factors that affect the peak mixing ratios, 74 cooking
254
events were analyzed. Positive correlations between the measured peak mixing ratios of these
255
species and cooking duration were observed (r2 = 0.42 - 0.72; Fig. 3), suggesting that operating
256
time of cooking appliances could explain 42% – 72% of the variability in the peak levels of NOx
257
and HONO. In addition, mixing ratios measured when cooking with individual burners at differ-
258
ent positions overlaps with oven operation, which suggests that appliance type overall exerted
259
little effect on the emissions. Furthermore, cooking events using multiple appliances fall tightly
260
along the same trend, indicative of negligible effect of additional appliances on the mixing ratios
261
observed. In previous controlled experiments, peak NOx levels depended on the number of gas
262
elements used.47 The reason for the lack of influence of combustion elements in this study is un-
263
certain. There may be other variables that are not accounted for such as the power of the appli-
264
ances and the setting during individual cooking events (e.g. oven temperature, gas mark on stove).
265
A ventilated range hood was used during some cooking events (N = 15) during the study pe-
266
riod. Recent assessments of range hood performance in the US indicate wide variations across
267
hoods and airflow and burner positions. Several studies reported that using overhead kitchen ex-
268
haust fans was associated with reduced NOx levels indoors.42,
269
Σ(NO2+HONO) production rates during cooking events were lower when the fan was in opera-
270
tion than when it wasn’t: 2.4 vs. 4.2 ppbv min-1 for NO, and 0.97 vs. 1.32 ppbv min-1 for
271
Σ(NO2+HONO) (Fig. 3a,3b). These observations suggest that the vented exhaust fan in the kitch-
272
en reduced NO and the sum of NO2 and HONO mixing ratios by approximately 43% and 27%,
273
respectively.
274
Indoor Decay/Removal Rate Constants
12 ACS Paragon Plus Environment
46, 49-50
In this study, NO and
Page 13 of 35
Environmental Science & Technology
275
For many of the cooking events, there was a clear exponential decay of the combustion by-
276
product mixing ratios after the appliance was shut off. The decay/removal rate constants of the
277
combustion by-products were estimated for 55 uninterrupted episodes after cooking. The decay
278
rate constant of CO2 can potentially be referred to as the indoor-outdoor air exchange rate (AER).
279
Estimated AER from 19 selected cooking events ranged from 0.1 – 1.6 hr-1 with a mean value of
280
0.62 (± 0.36) hr-1. This is consistent with reported AER for US residential homes (median/mean
281
of 0.3 – 1.12 hr-1).51-54 Decay rate constants of NO, Σ(NO2+HONO), NO2, and HONO were di-
282
rectly compared to AER; all were significantly higher (Fig. 4). This suggests that mixing ratios of
283
all these species decrease more rapidly than can be accounted for by air exchange alone and that
284
reactive processes (gas phase reactions and surface uptake) in the house make a significant con-
285
tribution to their removal.
286
The NO decay rate constant, kNO, was on average 0.92 ± 0.37 hr-1. A plot of kNO vs. kCO2
287
yielded an intercept of 0.35 h-1 (Fig. 4a), which can be considered the approximate reactive re-
288
moval rate constant of NO. The reactive NO removal rate constant can also be estimated as the
289
difference between kNO and the AER; rate constants determined by this method ranged from 0.12
290
to 0.79 hr-1 and averaged 0.33 hr-1. Although we are not certain of NO removal mechanisms other
291
than air exchange, its reaction with O3 infiltrated indoors is one possibility. As NO mixing ratios
292
indoors were high, it possibly quickly reacted with O3 and resulted in stable low levels of ozone
293
whereas high NO levels were sustained for hours. The lifetime of NO, i.e. the time it took for the
294
mixing ratio to decrease to e-1 of its initial value, varied between 30 – 228 min.
295
Reactive decay rate constants for NO2 and HONO were also determined via the difference
296
method. We note that limited distinct measurements of NO2 and HONO resulted in considerable
297
scatter in the data, especially for kNO2 (Fig. 4c, 4d). The performance of the denuder may also
298
have contributed to the scatter, as the denuder was sometimes deactivated quickly during cooking 13 ACS Paragon Plus Environment
Environmental Science & Technology
299
events when very high HONO concentrations were generated. This denuder passivation could
300
result in overestimations of kHONO and underestimations of kNO2 in this study. However, since the
301
decay rate constants calculated during periods with potential influence from denuder deactivation
302
match the trend of those without (Fig. 4c, 4d), the uncertainty introduced by this potential artefact
303
is minimal, and we are confident that the reactive HONO loss observed in this residence is real.
304
On average, kNO2 was 1.54 ± 0.52 hr-1. The reactive NO2 removal rate constant determined
305
from the difference method was 0.74 (± 0.35) hr-1, larger than the mean AER. This suggests that
306
reactive removal was more important to NO2 lifetimes indoors than air exchange. The mean reac-
307
tive NO2 removal rate constant determined in this house is similar to the mean reactive rate con-
308
stants reported in controlled experiments in residences.44, 55 Laboratory experiments have demon-
309
strated that heterogeneous reactions play an important role in removing NO2 from the air in in-
310
door environments due to the elevated surface area to volume ratios.24, 56-59 The reactive NO2 re-
311
moval rate constants determined in this study are comparable to those determined through cham-
312
ber experiments in the presence of carpets under various conditions,43 further suggesting that NO2
313
surface chemistry may be the dominant reactive NO2 removal mechanism indoors. Photolysis is a
314
significant sink for NO2 outdoors, but photolysis rates indoors are much lower due to the lack of
315
high energy photons. An NO2 photolysis rate constant of 8.49 × 10-4 s-1 was determined for sunlit
316
indoor regions based on our spectral irradiance measurements (see discussion below). This results
317
in a photochemical loss rate of 1.70 × 10-3 ppb s-1 (4.57 × 107 molec cm-3 s-1) at background NO2
318
levels (2.0 ppb) and 5.01 × 10-2 ppb s-1 (1.35 × 109 molec cm-3 s-1) at peak NO2 concentrations (59
319
ppb). However, photolysis likely did not significantly affect our measured kNO2 because only
320
small volumes of air in the residence were in direct sunlight at any given time, and the sampling
321
inlet was in shaded regions of the house throughout the campaign. Indeed, NO2 removal rate con-
14 ACS Paragon Plus Environment
Page 14 of 35
Page 15 of 35
Environmental Science & Technology
322
stants did not show dependence on time of day (or availability of indoor sunlight) in this study
323
(Fig. S4).
324
The average decay rate constant for HONO (kHONO) was 1.68 (± 0.55) hr-1, with a mean reac-
325
tive removal rate constant of 0.58 (0.16 – 1.03) hr-1. Previous experiments have reported negligi-
326
ble reactive HONO removal constants indoors.43-44 One possible HONO sink is uptake to surfac-
327
es.57 Although the specific mechanism is not clear, heterogeneous reaction of HONO with sur-
328
face-deposited nicotine from tobacco smoke highlights the possible reactive sinks on indoor inter-
329
faces involving HONO and organics.2 Thermodynamic partitioning of HONO into indoor materi-
330
als that act as HONO reservoirs could be another possible sink.43 As with NO2, photolysis is the
331
dominant sink for HONO outdoors, but this is likely not the case indoors, for the same reasons
332
outlined above with respect to NO2 (Fig. S4).
333
Photochemical OH Production
334
HONO photolysis has been predicted to be an important source of indoor OH; this has been
335
experimentally verified in sunlit classrooms.10 Indoor OH production rates from HONO in resi-
336
dences have not been reported. We measured spectral irradiance from sunlight entering the resi-
337
dence through glass patio doors and calculated OH production rates at measured HONO levels.
338
We do not present steady state OH mixing ratios because mixing ratios of OH sinks (especially
339
VOCs) are poorly constrained in residences, and were not measured in this study. Estimated
340
steady state OH mixing ratios would therefore be associated with very large uncertainty. Hydrox-
341
yl radical production rates, which are much better constrained in this study, can be incorporated
342
into indoor chemistry models to estimate steady state OH mixing ratios under a range of condi-
343
tions. Figure 5 shows the noon maximum wavelength-resolved photon fluxes inside this resi-
344
dence through the glass patio doors. A spectrum with the glass doors open is shown for compari-
15 ACS Paragon Plus Environment
Environmental Science & Technology
Page 16 of 35
345
son. Light is completely attenuated by the glass at wavelengths shorter than ~340 nm, but a sig-
346
nificant amount of light is transmitted in the actinic region (