20 Royalty-Free Audio Tracks for "Carbon Electra"

Cutted parts of an audio experiment using carbon electra saws with some internal pitch envelope going on, going into trash 2, going into eq modulation, going into manipulator (formant & pitch shift, a bit fm modulation on a shifting frequency at times), going into ott.

It's a recording of a calcium-sandoz® forte/fuerte 500 mg effervescent tabled falling into a glass of water and dissolving. You can hear the tablet dropping into the water and water droplet hitting water surface back. After w while - co2 buubles start to appear creating noisy sound. The recording has a long natural fadeout and unfortunately some background noise. I leaved "silence" before the sound starts so you can de-noise the recording to your needs (i prefer audacity for denoisig). Recorded inside of my wardrobe for acoustic isolation using zoom h2 on a mic-stand. Recoded as 96khz/24-bit wav. Normalized, truncated and convertet do 16-bit flac using audacity. I've converted this to 16-bit as it still has plenty of noise and 24-bits would not be any better after normalization.

Lockheed l-188 electra 4 engine turboprop airliner flyover.

Dry ice dumped in a small fountain and recorded with an r-09hr. The bubbles sound very frantic and are continuous. I couldn't get too close, or else the splashing would have entered the mic capsules. It is a very clear sound nonetheless.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Own creation. Created with audacity and yamaha moxf6.

Unedited raw sound of electra c1845w dishwasher on 15 minute prewash. Lots of water sounds filling, swishing, drainging, gurgling.

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.

A funky bass line in gmin. Synth patch made in carbon electra.

A funky bass line in the key of a. Synth patch made in carbon electra.