Solubility of Oxygen in Sea Water.

Abstract

GEh'EIL4t, PHYSICAL AKD INORGANIC. slowly collecting. ii7hatever the cause, hair-ever, the method advocated eliminates it; while in a11 other case5 this method gives the same result as the regula1 OSIC. In the next paper of this serieq will be considered the standardization of a tip, and the calculation, from the drop weight, of surface tension and the molecular weight; while in the succeeding ones, which will appear in the immediate future, will be presented the results already obtained with the fifty or more liquids examined, using tips of various diameters.

Thermal and Chemical Evolution of Comet Nuclei and Kuiper Belt Objects

“…The pioneering work towards answering this question is that of Whipple and Stefanik (1996), who considered the decay of longlived radionuclides and found that it would lead to loss of the most volatile species. It was followed by the studies of Wallis (1980) and Irvine et al (1980), who showed by simple calculations that liquid water could be obtained in the cores of comet nuclei.…”

Evaluating an Innovative Oxygen Sensor for Remote Subsurface Oxygen Measurements

“…Their equation and constants are provided below and are also referenced in the Aanderaa manual (Aanderaa Instruments, 2004 The various equations were compared assuming O 2 air content of 20.9% and a total pressure of 760 mm Hg. Results are presented in Figure 5 and show good agreement among Fox (1909) and Whipple and Whipple (1911);Perry (1973);Colt (1984);and Garcia and Gordon (1992) particularly for temperatures between 0 and 30 o C.…”

“…Oxygen solubility data for fresh and sea water based on work from Whipple and Whipple (1911) and Fox (1909) 4. Bunsen coefficients and other formulas to account for barometric pressure, water vapor pressure and depth for calculating the solubility of gases in fresh water as documented by Colt (1984).…”

Limnology of selected lakes in Ohio, 1975

“…Calculated equilibrium values of dissolved oxygen, extrapolated from the sea level data of Whipple and Whipple (1911) Except for photosynthesis, almost all oxygen transter to the water occurs at the air-water interface. Because oxygen diffuses very slowly in water (Hutchinson, 1957, p. 587) , winds, water turbulence, and currents play a major role in the aeration of a water body.…”