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Teaching Lesson 6 Lesson 6
vii. Bicarbonate (HCO
-
): 0.14g (< 1% by weight
How do scientists figure out how much salt is in the water? (slides 7 and 8)
1. Salinity is a measure of the total concentration of dissolved (inorganic) solids (e.g.,
salts) in water.
2. The major constituents or salts of seawater display an interesting feature. These
salts are always present in any of the world’s ocean basins and in the same
proportions to each other even if totally salinity varies. This is the Principle of
Constant Proportions and helps scientists measure salinity. This principle states
that the ratio of any two major constituents dissolved in seawater is constant. If a
scientist can measure
one of the major constituents in seawater, he/she can
calculate the amounts of all other major constituents and the salinity of the sample.
3. There are several tools available to measure ion concentration and to approximate
salinity. One example is an instrument known as a CTD, short for conductivity,
temperature and depth. The CTD measures how easily electric currents pass
through a sample of seawater (conductivity). Because salt content directly affects a
water sample’s conductivity, the measurement of conductivity can be translated to a
measurement of salinity. In addition, the NASA Aquarius satellite is a relatively new
technology that will be used to measure salinity on a global scale from space.
Salinity is variable across the ocean (slides 10 and 11)
1. Salinity is not homogenous throughout the ocean.
2. Geographically, salinity varies as a function of evaporation, precipitation and
freshwater input (e.g., river outflow, ice melt).
3. In general salinity increases with decreasing latitude from the poles to the tropics
and then decreases from the tropics to the equator. At the mid-latitudes, high
salinity levels can result from warm, dry conditions and increased evaporation. Near
the equator, greater rainfall occurs resulting in lowered salinity. At high latitudes,
melting ice contributes to lower salinity levels.
Why is salinity important? (slide 12)
1. Salinity is one variable that affects the density of water. When water has different
densities, it forms layers as was demonstrated at the beginning of the lesson.
2. Layers in the ocean are part of the reason the ocean has currents, which we will
learn about in future lessons.
III. Additional Web Resources
1. Background information:
http://www.classzone.com/books/earth_science/terc/navigation/home.cfm