The Hydrodynamics of Canadian Atlantic Waters
The Hydrodynamics of Canadian Atlantic Waters
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In our eReader you can find the full English version of the book. Read The Hydrodynamics of Canadian Atlantic Waters Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Hydrodynamics of Canadian Atlantic Waters
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There are thus many ways of drawing up graphic presentments of solenoids. We need not, however, here devote more time to these, but may pass directly to the problem of calculating, in the simplest and surest manner, their number, A. The number of solenoids between two stations in a horizontal water layer of one metre is obviously equal to the difference in specific volume between the two stations at the level in question. Our first task, then, will be to calculate this difference. Let us, for i...nstance, calculate the solenoids between the stations 34 and 35 in section IX. First of all, we note down the depth at which the water samples from each station were taken. This is shown in the first column of table 3. The second column shows the specific volumes for station 34, and the third those for station 35. The fourth column contains the differences between the specific volumes; i. E. , the number of solenoids in a water layer one metre thick situated between the two. The signsi before the figures shows the rotary tendency of the solenoids.
What to read after The Hydrodynamics of Canadian Atlantic Waters?
You can find similar books in the "Read Also" column, or choose other free books by J W Johan Wilhelm Sandstrm to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
There are thus many ways of drawing up graphic presentments of solenoids. We need not, however, here devote more time to these, but may pass directly to the problem of calculating, in the simplest and surest manner, their number, A. The number of solenoids between two stations in a horizontal water layer of one metre is obviously equal to the difference in specific volume between the two stations at the level in question. Our first task, then, will be to calculate this difference. Let us, for i...nstance, calculate the solenoids between the stations 34 and 35 in section IX. First of all, we note down the depth at which the water samples from each station were taken. This is shown in the first column of table 3. The second column shows the specific volumes for station 34, and the third those for station 35. The fourth column contains the differences between the specific volumes; i. E. , the number of solenoids in a water layer one metre thick situated between the two. The signsi before the figures shows the rotary tendency of the solenoids.
What to read after The Hydrodynamics of Canadian Atlantic Waters?
You can find similar books in the "Read Also" column, or choose other free books by J W Johan Wilhelm Sandstrm to read onlineMoreLess
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