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Стр. 985
The ratio , Rco of measured to calculated dissolved CO concentrations , in which the calculated values are obtained by multiplying the measured partial pressures of Co in the atmosphere by the solubility coefficients for CO in seawater ...
The ratio , Rco of measured to calculated dissolved CO concentrations , in which the calculated values are obtained by multiplying the measured partial pressures of Co in the atmosphere by the solubility coefficients for CO in seawater ...
Стр. 1345
The calculated lifetime is in good on the direction of initial recoil ) . ... and a computer calculation of the attenua- level , is extremely strong evidence for this distribution of gamma - ray energies tion factor F as a function of ...
The calculated lifetime is in good on the direction of initial recoil ) . ... and a computer calculation of the attenua- level , is extremely strong evidence for this distribution of gamma - ray energies tion factor F as a function of ...
Стр. 1701
Difference synthesis calculated with the difference between the amplitudes of a six - atom random structure ( crosses ) and the tyrosine structure ( dots ) , and the phases of the tyrosine structure . Contours are at intervals of 1 ...
Difference synthesis calculated with the difference between the amplitudes of a six - atom random structure ( crosses ) and the tyrosine structure ( dots ) , and the phases of the tyrosine structure . Contours are at intervals of 1 ...
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LETTERS | 932 |
Y Pomeranz K F Finney R C Hoseney | 950 |
BOOK REVIEWS | 968 |
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