fined la . al < 8G, |B Oceanorraphical Properties of Seawater a : * Masaru SHIOZAKI ~ L, Observations @®+- Seawater samples for chemical analysis and water temperature measurements were collected by Nansen _ “bottles equipped with reversable thermometers from tthe :150 and 300 m levels. Surface water was sampled shy; polyethylene bucket and the surface temperature was measured with a standard type thermometer. Chemical lysis was performed for dissolved oxygen, chlorine ‘content and hydrogen ion concentration. Yet 2. Measurements a. Dissolved oxygen - The amount found in the sea water was determined by the Winkler method. oan b. Chlorinity - Determined by the Fajans tritation ~~method using Uranin as the indicator and silver nitrate Splutions as the titrant. Lor oe, mad ; c. Hydrogen ion concentration - Determined by the visual colorimetric method. me FR eResults ~seecx Temperature measurements and chemical analysis of _the seawater samples are shown in Table 1. Horizontal “distribution of seawater temperature at the surface, 750%m level, 100 m level and 200 m level are shown in » Figs 1 to 4. Horizontal distribution of chlorinity and ‘dissolved oxygen at the surface and 150 m levels «re shown ‘in Figs 5 to 8. ™ mM Oo sO a QA, CN SO S&S @ 9 @ ww e Ww " un 0 © NN ~t t+ + 3 & Sectional distribution of seawater “temperature, chlorinity and dissolved oxygen are . Shown in Figs 9 to 11. ona 3 tC Se | a | ae , Hydrographic Division, Meritime Safety Board Agency a tleter 2 a ep ee ee ee —37— eeoeen ee ee =

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