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Phosphorus cosmogenic

Benitez-Nelson, C.R., and Karl, D.M. (2002) Phosphorus cycling in the North Pacific Subtropical Gyre using cosmogenic 32P and 33P. Limnol. Oceanogr. 47, 762-770. [Pg.544]

Of the isotopes listed in Table 2 the study of the cosmogenic isotopes of phosphorus (half-life = 14.3 d) and (half-life = 25.3 d) provides insights into the residence time of aerosols in upper troposphere air because of the relatively short half-lives of the nuclides. Waser and Bacon (1995) measured the concentrations of P and P in precipitation at Bermuda over three seasons. They concluded that, with the average activity ratio of P to P of 0.96 and a production activity ratio of 0.7, the average residence time of aerosols in the upper troposphere was 40 d. This increase in the... [Pg.2185]

Cosmogenic and as Tracers of Phosphorus Cycling in Surface Waters... [Pg.575]


See other pages where Phosphorus cosmogenic is mentioned: [Pg.375]    [Pg.615]    [Pg.4486]    [Pg.4486]    [Pg.4500]    [Pg.314]    [Pg.567]    [Pg.576]    [Pg.11]   


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Cosmogenic

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