ScienceJohn Michels (Journalist) 1959 |
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Стр. 330
... troposphere and Nsg is the number of bomb - pro- duced C14 atoms in the Southern Hemi- sphere stratosphere . In words , this equa- tion simply says that the rate at which the amount of tropospheric bomb C14 increases is directly ...
... troposphere and Nsg is the number of bomb - pro- duced C14 atoms in the Southern Hemi- sphere stratosphere . In words , this equa- tion simply says that the rate at which the amount of tropospheric bomb C14 increases is directly ...
Стр. 332
... troposphere can be estimated directly from Fig . 2 and a knowledge of the pre - bomb tropospheric C14 inventory ( 25 x 1027 atoms ) . Up to March 1958 the amounts are 1.5 x 1027 atoms of bomb C14 in the Southern Hemisphere troposphere ...
... troposphere can be estimated directly from Fig . 2 and a knowledge of the pre - bomb tropospheric C14 inventory ( 25 x 1027 atoms ) . Up to March 1958 the amounts are 1.5 x 1027 atoms of bomb C14 in the Southern Hemisphere troposphere ...
Стр. 552
... troposphere ( 6 ) . The stratospheric inventory is constant , al- most within experimental error , at 7.2 x 1027 carbon - 14 atoms during the period 1 July 1955 to 1 July 1958 ( see Table 5 ) . The average rate of increase of car- bon ...
... troposphere ( 6 ) . The stratospheric inventory is constant , al- most within experimental error , at 7.2 x 1027 carbon - 14 atoms during the period 1 July 1955 to 1 July 1958 ( see Table 5 ) . The average rate of increase of car- bon ...
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