

FOLLOWUS
Institute of Oceanology
纸质出版:1990
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Quantitative determination of the salinity of seawater droplet in 10−6 to 10−10 gram[J]. 海洋湖沼学报(英文), 1990,8(3):213-219.
Zhengxu, Q., Fangying, P. Quantitative determination of the salinity of seawater droplet in 10−6 to 10−10 gram., Chin. J. Ocean. Limnol. 8, 213–219 (1990). https://doi.org/10.1007/BF02849660
Quantitative determination of the salinity of seawater droplet in 10−6 to 10−10 gram[J]. 海洋湖沼学报(英文), 1990,8(3):213-219. DOI: 10.1007/BF02849660.
Zhengxu, Q., Fangying, P. Quantitative determination of the salinity of seawater droplet in 10−6 to 10−10 gram., Chin. J. Ocean. Limnol. 8, 213–219 (1990). https://doi.org/10.1007/BF02849660 DOI:
The rate of evaporation of seawater droplets in the air-sea boundary layer can be estimated by its salinity change compared to the sea surface salinity. A micro-chemical method based on Farlow (1954) is developed for quantitative determination of the salinity of an individual droplet without the error due to further evaporation after sampling. A halide ion-sensitive sampling surface is prepared by colloidally dispersing brown silver dichromate into the gelatin layer of a commercially available film. The reaction of soluble chlorides with the silver salt leaves a clear white halo with diametera on the brown film to reveal the volume of the droplet. After the film is developed in a water vapor saturated atmosphere
the halo grows to diameterd with the original as the embryo to indicate the quantity of chloride ion involved in the action. The ratio ofd/(a1.5) is a function of the salinity of the droplet. The method can be used to determine the salinity of seawater droplet of 10−6 to 10−10 gram. Details of the principle and preparation
and calibration of the reagent film
are presented.
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