14 Royalty-Free Audio Tracks for "Expel"

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00:02
Birds being expelled.
Author: Christianand
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00:07
A snore with a flapping of lips whilst expelling air. Not natural created for comedy effect.
Author: Alankidd
00:00
00:16
I recorded this on a h4n zoom recorder as part of a college project.
Author: Robrt
00:00
00:07
A snore with a whistle whilst expelling air. Not natural created for comedy effect.
Author: Alankidd
00:00
00:03
A balloon deflating, recorded with a rode microphone.
Author: Hareball
00:00
00:25
A cloud of glass dust is expelled into the air. Created for the iron realm podcast.
Author: Zatar
00:00
00:09
Recording of me breathing out. Recorded using a sennheiser mkh416 and a sound devices 552.
Author: Squareal
00:00
00:03
Its a bright sneezy day 🤣.
Author: Jpbillingsleyjr
00:00
00:05
It is a constant sound of air expelled of the machine in the form of cold air streama and it has low pitch.
Author: Victoriarey
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00:01
What your mouth expels when somebody kicks your belly or legs (e. G. Sports). Sound recorded in pompeu fabra university (bcn, 2014).
Author: Joseppujol
00:00
00:06
The sound of Musket Fire at a civil war reenactment. Great for civil war, or wars in that time period.
Author: nps
00:00
00:24
Sound of person flushing the toilet. Toilet flush sound effect is public domain so use it however you want. Great bathroom, restroom, or cleaning sounds.
Author: Grzegorz Adam Hankie
00:00
10:29
Individual gryphons, davis-schrimpf seep field, salton sea, california. Lat: 33. 20070326716746lon: 244. 42179501054162. The davis-schrimpf onshore seep field site in the salton sea geothermal system is the result of shallow magmatic intrusions in a sedimentary basin. The ssgs is situated in the salton trough in southern california, an area with abundant surface manifestations of hydrothermal activity. The hydrothermal system in the salton trough occurs in a pull-apart setting where rifting and associated magmatic intrusions are responsible for the strong heat flow. One of the most concentrated and well-expressed onshore seep fields is the davis-schrimpf field, where more than 50 individual seeps are located in this area. Gas venting from gryphons and pools is vigorous with a continuous bubbling activity. Water and mud mixtures are continuously expelled down the flanks of the gryphons. Carbon dioxide produced from de-volatilization reactions involving sedimentary carbonate is the main driver for the seep activity. The morphological features of the davis- schrimpf seep field are strikingly similar to seep fields on dormant mud volcanoes however, the davis-schrimpf seeps are not related to mud volcanism, as mud volcanism normally implies large-scale mud breccia eruptions and a low temperature seep stage. From the; journal of geophysical research, vol. 114, b09201, doi:10. 1029/2008jb006247, 2009.
Author: Rtb
00:00
04:09
Mud volcano field, davis-schrimpf seep field, salton sea, california. Lat: 33. 20070326716746lon: 244. 42179501054162. The davis-schrimpf onshore seep field site in the salton sea geothermal system is the result of shallow magmatic intrusions in a sedimentary basin. The ssgs is situated in the salton trough in southern california, an area with abundant surface manifestations of hydrothermal activity. The hydrothermal system in the salton trough occurs in a pull-apart setting where rifting and associated magmatic intrusions are responsible for the strong heat flow. One of the most concentrated and well-expressed onshore seep fields is the davis-schrimpf field, where more than 50 individual seeps are located in this area. Gas venting from gryphons and pools is vigorous with a continuous bubbling activity. Water and mud mixtures are continuously expelled down the flanks of the gryphons. Carbon dioxide produced from de-volatilization reactions involving sedimentary carbonate is the main driver for the seep activity. The morphological features of the davis- schrimpf seep field are strikingly similar to seep fields on dormant mud volcanoes however, the davis-schrimpf seeps are not related to mud volcanism, as mud volcanism normally implies large-scale mud breccia eruptions and a low temperature seep stage. From the; journal of geophysical research, vol. 114, b09201, doi:10. 1029/2008jb006247, 2009.
Author: Rtb
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