Accurate measurements of the size and quantity of aerosols generated by various human activities in different environments are required for efficacious mitigation strategies and accurate modeling of respiratory disease transmission. Previous studies of speech droplets, using standard aerosol instrumentation, reported very few particles larger than 5 μm. This starkly contrasts with the abundance of such particles seen in both historical slide deposition measurements and more recent light scattering observations. We have reconciled this discrepancy by developing an alternative experimental approach that addresses complications arising from nucleated condensation. Measurements reveal that a large volume fraction of speech-generated aerosol has diameters in the 5- to 20-μm range, making them sufficiently small to remain airborne for minutes, not hours. This coarse aerosol is too large to penetrate the lower respiratory tract directly, and its relevance to disease transmission is consistent with the vast majority of severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2) infections initiating in the upper respiratory tract. Our measurements suggest that in the absence of symptoms such as coughing or sneezing, the importance of speech-generated aerosol in the transmission of respiratory diseases is far greater than generally recognized.Respiratory tract infections are caused by a wide range of pathogenic organisms (
1), including a large array of respiratory viruses, such as influenza virus, rhinovirus, measles virus, respiratory syncytial virus, adenovirus, and most recently, severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2). In all these diseases, person-to-person spread involves respiratory droplets, which originate from the mucus layer that covers the epithelium of the respiratory tract or from oral fluid present in the mouth, mostly as saliva. Thus, characterizing respiratory droplets is essential to understanding respiratory pathogen transmission and will inform effective public health policies to curb infections. Four mechanisms for droplet generation are generally considered: breathing, speaking (singing, laughing, etc.), coughing, and sneezing (
2). Considering the well-recognized importance of asymptomatic transmission of SARS-CoV-2 (
3), our study focuses on the first two of these mechanisms.As highlighted by Wells (
4) and Duguid (
2) nearly a century ago, the vast majority of respiratory droplets are smaller than ca. 100-μm diameter and fully dehydrate once entering the atmosphere. These desiccated droplets can remain airborne for minutes to hours before landing on solid surfaces. If generated by a person infected by a respiratory virus, they will contain virions that can remain viable and infectious for many hours (
5,
6). Upon inhalation, airborne particles can reach different parts of the respiratory tract depending on their size: coarse aerosols with diameter
D 5 μm (
7) deposit in the upper respiratory tract (URT), and fine aerosols with
D < 5 μm can penetrate deep into the lower respiratory tract (LRT). Many viral pathogens, including SARS-CoV-2, influenza, rhinovirus, and measles virus, can infect both URT and LRT epithelia (
1,
8,
9), with URT infections typically associated with mild initial symptoms and LRT infections possibly resulting in life-threatening pneumonia (
1,
10–
13). Direct infection of the LRT, before the adaptive immune system has been triggered by vaccination or a preceding URT infection, presents a greater risk.An URT infection also can expand into the LRT through microaspiration of oropharyngeal fluids (
14,
15). The extent to which inhalation of self-generated URT cough, speech, or sneeze aerosols may contribute to this migration remains unknown. However, it has been argued that this pathway could be significant because an infected carrier is invariably at the center of their own speech aerosol cloud, which results in strongly elevated exposure (
16). The risk of migration from the URT to the LRT rises with the viral load and the viability of the virus, which peak around and just prior to the onset of symptoms, respectively (
17,
18). For the original Wuhan strain of the SARS-CoV-2 virus, the onset of symptoms occurs about 5 days after the initial infection (
17,
19), but it occurs somewhat earlier for the more infectious delta and omicron variants (
20).To evaluate the risk of LRT infection, it is important to know the size distribution of particles generated by various respiratory activities. For talking, coughing, and sneezing, studies historically relied on slide sampling techniques of increasing sophistication, followed by microscope observation (
2,
21,
22). Droplets generated by breathing or vowel sounds are numerous but very small (≲2 μm) and thus more difficult to evaluate with those classical methods. Instead, such small droplets are now commonly quantified by aerosol detection equipment, such as optical particle sizers (OPSs), based on light scattering (
22,
23); aerodynamic particle sizers (APSs), based on the time-of-flight measurement in an accelerating flow field (
24); and scanning mobility particle sizers that derive a particle’s size from its mobility in an electric field and are best suited for very small sizes (≲1 μm) (
25,
26). APS instruments are less efficient at detecting medium-sized liquid particles, and undercounts as high as 75% for 10-μm droplets have been reported (
27).There is some confusion in the literature about the hydration state of reported sizes of respiratory aerosol particles, which shrink by a factor of γ upon evaporation of their aqueous content, thus by a factor of γ
3 in volume. After full dehydration, a particle’s radius is determined by its amount of nonvolatile matter. Estimates for γ vary substantially: Nicas et al. (
28) proposed γ = 2 for breath particles, based on data extracted from breath condensate by Effros et al. (
29) that indicated a high fraction (ca. 8% wt/vol) of glycoproteins, presumably mucins. Holmgren et al. (
30) reported γ = 2.4 for breath particles when the relative humidity (RH) is reduced from 99.5% in the small airways to 75%. Bagheri et al. (
26) observed γ = 4.5 for singing particles in a diffusion dryer or γ = 4 for large saliva droplets observed directly by microscope imaging. Some of those measurements were conducted directly at the mouth opening, observing the hydrated state using light scattering or holographic imaging techniques (
26,
31). Clearly, the concentration of pathogens in dehydrated particles scales with γ
3 relative to the originating airway lining fluid (ALF) or saliva. However, the high uncertainty in the applicable γ value, which is frequently not even reported, prevents accurate estimates of airborne virus concentrations.Recently, we and others demonstrated that speech particles can be readily observed by simple video recordings of light scattering by these particles (
32–
35). Such recordings not only present a visually compelling warning to the public but also provide opportunities to monitor particles before, during, and after dehydration. Those light scattering measurements focused on particles larger than a few microns due to technical sensitivity issues. The intensity of scattered light scales with the square of a particle’s diameter, causing a dynamic range problem and rendering it more challenging to observe the smallest particles, especially in the presence of larger particles. Inexpensive, fast consumer cameras typically use 10- to 12-bit analog-to-digital converters (ADCs), thereby limiting dynamic range; while detectors with an increased ADC range are available, their speed is often insufficient for high-speed recording.Here, we aim to evaluate the entire range of speech droplet sizes produced during different breathing and speaking protocols. To do so, we combined video-recorded light scattering and an OPS to evaluate droplets from 0.3 to 100 μm. Our data show a continuous spectrum that lacks previously reported gaps in the size distribution (
36). Our measurements confirm that the gravitational settling rate for dehydrated particles larger than 5 μm steeply increases with size, but considering the high numbers, volumes, and airborne lifetimes of those particles, they are likely to be a dominant factor in transmission of disease.
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