108 безкоштовних аудіофайлів для "Грязюка"

One of a series of heavily processed sounds of a squelchy stress reliever toy. I ran the original recordings through s-layer, the sample-mangling plugin from twisted tools, combining and mulching everything into new, dynamic sounds with lots of interesting, muddy contours.

Boots walking through short grass. Heavy rain the previous day had created a large amount of mud which can also be heard in this recording. Should be enough space in between each step to be effectively cut up for foley work. Recorded with a ntg2 mono shotgun microphone into a r05 recorder.

Mud and rocks river. Created by strong rains on the top of a volcano. After the rains, mud comes down dragging rocks. Night. Iruya, very small town in salta, northwest argentina. Recorded using zoom h4n internal mics (stereo xy setup) and rodentg-2. 3 meters distance.

Sounds of walking in the forest in poland. Walking on the path, on the leaves (with some sticks breaking) and in some mud.

A small fountain pitched down and reverb added. Recorded with zoom h4n pro x/y mics.

An organic squish sound. Perfect for chewing gum or gore effects. Recorded on zoom h2.

A second attempt at recording the deep mud i keep finding myself walking through each morning on walthamstow marshes. This recording was made using a sound devices mixpre6ii and a stereo pair of fel em172 mics (connected to a bent wire clothes hanger and positioned about 30cm above my feet). Processing: normalize -1. 0db, low cut filter 100hz, minor noise reduction to reduce background traffic/train noise. I do not require any credit or attribution. If any of these sounds have been of help, and you are feeling charitable, please do consider donating to freesound to help keep the site running (a link is also on the home page). Any donations are greatly appreciated!.

A wet napkin being squished. Take 1.

Walking on a watery surface or mud.

Step on a slug (splat!) 1.

Step on a slug (splat!) 2.

Footsteps with rubber boots in a muddy path with wet grass. Close upsome wind and some residual far away voice, one is calling "a table!"france, nov2022. Recorded with schoeps cmc6-mk41recorded on sounddevice mixpre648khz, 24 bits, wave mono.

A cartoony splat! sound.

A muddy splat.

I walked along a quiet forest path in the evening and recorded my steps. In the background you can hear quietly call a tawny owl.

Close up of rubber boots trampling in mud. Some "splurp" sounds sometimes. France, january 2023. Recorded wuth shoeps cmc6 mk41recorded on sounddevice mixpre624bits, 48khz, wave mono.

A very slimy and gross sound.

Walking through something wet.

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.

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.

Sticky cartoonish sound of web, net, goo, dirt, mud, creak, squeeze, squeak, screech.

Foley recording for picture of a person walking through muddy terrain with raincoat put on.