Download presentation
1
LESSON TOPIC: The Inorganic Chemistry of Water
2
What is salinity? What are the major sea salts?
Salinity- the total quantity or concentration of all dissolved inorganic solids, or more precisely, ions. This is the sodium chloride and everything else, commonly called the dissolved salts.
3
Salinity is expressed in parts per thousand .
The abbreviation ‰ stands for “parts per thousand” The ocean’s average salinity is 35‰. The most common salts: sodium chloride (NaCl) potassium chloride (KCl).
5
What are the colligative properties of seawater
What are the colligative properties of seawater? Does fresh water have these properties? The properties of a liquid that may be altered by the presence of a solute are called colligative properties.
6
Raised boiling point. Decreased freezing temperature. Ability to create osmotic pressure. Electrically conductive. Decreased heat capacity. Slowed evaporation.
7
What are the most abundant chemicals in seawater?
Let’s suppose you have one kilogram of seawater with average salinity (35‰). This means that 3.5%, or 35 grams, would be dissolved solids. Based on constant proportions, this would break down to these approximate numbers: Cl-) Chloride g (Na+) Sodium g (SO42-) Sulfate 2.65 g (Mg2+) Magnesium 1.28 g (HCO3) Bicarbonate 0.14 g (Ca2+) Calcium 0.40 g (K+) Potassium 0.38 g Other 0.61 g
8
How do marine scientists determine salinity?
Salinity is determined with a salinometer, which determines the electrical conductivity of the water. (CTD) sensors Thermistor - temperature. Conductivity - current flowing between two platinum electrodes sealed in a tube of non-conducting glass. Pressure measurements are made by measuring the natural frequency of a quartz crystal.
13
How do temperature and salinity affect seawater density?
Salinity and temperature also vary with depth. Density differences cause water to separate into layers. High-density water lies beneath low-density water. Low temperature and high salinity are features of high-density water.
14
What factors affect seawater’s pH? Why does pH change with depth?
Pure water has a pH of 7, which is neutral. Seawater pH typically ranges from 7.8 to 8.3, which is very mildly alkaline. However, the ocean’s pH remains relatively stable due to buffering. A buffer is a substance that reduces the tendency of a solution to become too acidic or too alkaline.
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.