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Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments
Natural aquatic environments such as oceans, lakes, and rivers are home to a tremendous diversity of microorganisms. Some may cross the air-water interface within droplets and become airborne, with the potential to impact the Earth’s radiation budget, precipitation processes, and spread of disease....
Autores principales: | , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
PeerJ Inc.
2018
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6163035/ https://www.ncbi.nlm.nih.gov/pubmed/30280035 http://dx.doi.org/10.7717/peerj.5663 |
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author | Pietsch, Renee B. Grothe, Hinrich Hanlon, Regina Powers, Craig W. Jung, Sunghwan Ross, Shane D. Schmale III, David G. |
author_facet | Pietsch, Renee B. Grothe, Hinrich Hanlon, Regina Powers, Craig W. Jung, Sunghwan Ross, Shane D. Schmale III, David G. |
author_sort | Pietsch, Renee B. |
collection | PubMed |
description | Natural aquatic environments such as oceans, lakes, and rivers are home to a tremendous diversity of microorganisms. Some may cross the air-water interface within droplets and become airborne, with the potential to impact the Earth’s radiation budget, precipitation processes, and spread of disease. Larger droplets are likely to return to the water or adjacent land, but smaller droplets may be suspended in the atmosphere for transport over long distances. Here, we report on a series of controlled laboratory experiments to quantify wind-driven droplet production from a freshwater source for low wind speeds. The rate of droplet production increased quadratically with wind speed above a critical value (10-m equivalent 5.7 m/s) where droplet production initiated. Droplet diameter and ejection speeds were fit by a gamma distribution. The droplet mass flux and momentum flux increased with wind speed. Two mechanisms of droplet production, bubble bursting and fragmentation, yielded different distributions for diameter, speed, and angle. At a wind speed of about 3.5 m/s, aqueous suspensions of the ice-nucleating bacterium Pseudomonas syringae were collected at rates of 283 cells m(−2) s(−1) at 5 cm above the water surface, and at 14 cells m(−2) s(−1) at 10 cm above the water surface. At a wind speed of about 4.0 m/s, aqueous suspensions of P. syringae were collected at rates of 509 cells m(−2) s(−1) at 5 cm above the water surface, and at 81 cells m(−2) s(−1) at 10 cm above the water surface. The potential for microbial flux into the atmosphere from aquatic environments was calculated using known concentrations of bacteria in natural freshwater systems. Up to 3.1 × 10(4) cells m(−2) s(−1) of water surface were estimated to leave the water in potentially suspended droplets (diameters <100 µm). Understanding the sources and mechanisms for bacteria to aerosolize from freshwater aquatic sources may aid in designing management strategies for pathogenic bacteria, and could shed light on how bacteria are involved in mesoscale atmospheric processes. |
format | Online Article Text |
id | pubmed-6163035 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2018 |
publisher | PeerJ Inc. |
record_format | MEDLINE/PubMed |
spelling | pubmed-61630352018-10-02 Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments Pietsch, Renee B. Grothe, Hinrich Hanlon, Regina Powers, Craig W. Jung, Sunghwan Ross, Shane D. Schmale III, David G. PeerJ Biophysics Natural aquatic environments such as oceans, lakes, and rivers are home to a tremendous diversity of microorganisms. Some may cross the air-water interface within droplets and become airborne, with the potential to impact the Earth’s radiation budget, precipitation processes, and spread of disease. Larger droplets are likely to return to the water or adjacent land, but smaller droplets may be suspended in the atmosphere for transport over long distances. Here, we report on a series of controlled laboratory experiments to quantify wind-driven droplet production from a freshwater source for low wind speeds. The rate of droplet production increased quadratically with wind speed above a critical value (10-m equivalent 5.7 m/s) where droplet production initiated. Droplet diameter and ejection speeds were fit by a gamma distribution. The droplet mass flux and momentum flux increased with wind speed. Two mechanisms of droplet production, bubble bursting and fragmentation, yielded different distributions for diameter, speed, and angle. At a wind speed of about 3.5 m/s, aqueous suspensions of the ice-nucleating bacterium Pseudomonas syringae were collected at rates of 283 cells m(−2) s(−1) at 5 cm above the water surface, and at 14 cells m(−2) s(−1) at 10 cm above the water surface. At a wind speed of about 4.0 m/s, aqueous suspensions of P. syringae were collected at rates of 509 cells m(−2) s(−1) at 5 cm above the water surface, and at 81 cells m(−2) s(−1) at 10 cm above the water surface. The potential for microbial flux into the atmosphere from aquatic environments was calculated using known concentrations of bacteria in natural freshwater systems. Up to 3.1 × 10(4) cells m(−2) s(−1) of water surface were estimated to leave the water in potentially suspended droplets (diameters <100 µm). Understanding the sources and mechanisms for bacteria to aerosolize from freshwater aquatic sources may aid in designing management strategies for pathogenic bacteria, and could shed light on how bacteria are involved in mesoscale atmospheric processes. PeerJ Inc. 2018-09-26 /pmc/articles/PMC6163035/ /pubmed/30280035 http://dx.doi.org/10.7717/peerj.5663 Text en ©2018 Pietsch et al. http://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, reproduction and adaptation in any medium and for any purpose provided that it is properly attributed. For attribution, the original author(s), title, publication source (PeerJ) and either DOI or URL of the article must be cited. |
spellingShingle | Biophysics Pietsch, Renee B. Grothe, Hinrich Hanlon, Regina Powers, Craig W. Jung, Sunghwan Ross, Shane D. Schmale III, David G. Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments |
title | Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments |
title_full | Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments |
title_fullStr | Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments |
title_full_unstemmed | Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments |
title_short | Wind-driven spume droplet production and the transport of Pseudomonas syringae from aquatic environments |
title_sort | wind-driven spume droplet production and the transport of pseudomonas syringae from aquatic environments |
topic | Biophysics |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6163035/ https://www.ncbi.nlm.nih.gov/pubmed/30280035 http://dx.doi.org/10.7717/peerj.5663 |
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