Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Everett N. Jones"'
Autor:
David G. Browning, Everett N. Jones
Publikováno v:
Limnology and Oceanography. 16:503-509
Publikováno v:
Journal of the American Chemical Society. 90:1110-1115
Publikováno v:
Journal of the American Chemical Society. 92:2946-2949
Publikováno v:
Science (New York, N.Y.). 162(3858)
Lake Superior was chosen as an experimental site to compare sound absorption of freshwater with the results of absorption measurements in seawater. The relaxation-like absorption at 1 kilohertz occurring in seawater is also present in freshwater. A r
Publikováno v:
Chemischer Informationsdienst. Organische Chemie. 1
Die Kinetik der Auflosung von Cu in mit Sauerstoff gesattigten n-Butylamin- Tetrachlorkohlenstoff-Losungen bei einem Druck von 1 at wird untersucht.
Autor:
David G. Browning, William H. Thorp, Everett N. Jones, J. M. Gorman, F. G. Weigle, Robert H. Mellen
Publikováno v:
The Journal of the Acoustical Society of America. 51:108-108
In order to determine the cause of the low‐frequency sound attenuation anomaly in seawater, comparative measurements are being made in freshwater. The Lake Tanganyika experiment (23°C) was conducted to determine the temperature dependency of the a
Publikováno v:
The Journal of the Acoustical Society of America. 50:122-122
The trend to lower sonar frequencies following WWII has revealed the existence of two and possibly more regimes of excess attenuation of sound in the oceans. The first of these, identified as a relaxation absorption caused by the MgSO4 content in sea
Publikováno v:
The Journal of the Acoustical Society of America. 49:107-107
Extensive measurements in the Atlantic Ocean (4°C) have shown the attenuation of sound below 10 kHz to be anomalously high. In order to determine the temperature dependency of this anomaly, a similar experiment has been conducted in the warmer water
Publikováno v:
The Journal of the Acoustical Society of America. 53:299-299
With the support of the French Navy, a low‐frequency sound propagation experiment was conducted to obtain attenuation coefficients in the Indian Ocean for the frequency range 200&–10 000 Hz. The experiment was conducted along a 500‐km track, wh