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Chemical and Physical Features of Seawater and the World Ocean

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Chemical and Physical Features of Seawater and the World Ocean Ch. 3 How do we get this data? CTD: Conductivity-temp-depth meters Fig. 3.9 in text Red arrow for water ... – PowerPoint PPT presentation

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Title: Chemical and Physical Features of Seawater and the World Ocean


1
Chemical and Physical Features of Seawater and
the World Ocean
  • Ch. 3

2
(No Transcript)
3
Objectives
  1. Understand the basic chemical and physical
    properties of water seawater.
  2. The origin of the seas

4
(No Transcript)
5
Global Water Distribution Estimate (Scroll down
to global water distribution table)
6
What percentage of the human body consists of
water?
  • Babies 78
  • One Year old 65
  • Adult men 60
  • Women 55
  • Why do women have less water?
  • They have a higher percentage of fat --gt hold
    less water

7
What about marine organisms?
  • Most consist of about 80 of water
  • Jellyfish?
  • Over 95!!

Recently discovered species of sea anemone,
Aleutian Islands
Nomura Jellyfish, Japan
8
Water is unique. Why?
  • Naturally occurs in all three states
  • Solid, liquid, and gas
  • No other substance on earth does this

9
Element vs. Molecule
  • Whats the difference?
  • Element
  • Composed of a single type of atom (only about 118
    of these in the world)
  • Molecule
  • Combination of two or more atoms
  • What does water consist of?

10
Molecular Makeup H2O
  • Opposite charges
  • Oxygen is (-)
  • Hydrogen is ()
  • Draw a water molecule
  • Forms weak hydrogen bonds
  • Why is it important that water has weak bonds??

11
Hydrogen bonds
  • This is what allows water to go from state to
    state
  • Molecules in constant motion
  • What happens when they speed up?
  • They get warmer and then . . . ?

12
Fast and Slow molecules
  • The bonds break and water enters the vapor state
  • What about when it cools?
  • Movement slows down, becomes dense until is slows
    down so much that. . .

13
It freezes!
  • What temperature is water at its most dense
    form?
  • 4º C. Is it frozen at this temperature?
  • Why is this important?
  • What if ice were waters densest state?

14
The Changing Molecular Structure of H2O
What do you notice about the structure of each
state?
15
Bottom line
  • Seawater becomes denser as it cools, until it
    freezes.
  • Ice is less dense than liquid water

16
Heat and Water
  • Water has the highest latent heats of melting and
    evaporation
  • How does ice keep our drinks cold?
  • It takes a lot of heat to melt ice
  • Heat breaks hydrogen bonds in ice instead of
    heating up your drink --gt drink stays cold
  • Why do we sweat?
  • H2O has high heat capacity
  • Absorbs a lot of heat w/ a relatively small
    increase in temp
  • Why is this important for marine organisms?
  • Not subject to drastic temp change

17
The Universal Solvent
  • Why can water dissolve more things than any other
    substance?
  • Its both (-) and () charged!
  • Pulls apart salt
  • Sodium (Na) Chloride (Cl-)

18
What Makes up Seawater?
Ions (charged particles) enter the sea from
different places
19
Composition of Seawater
  • Theres a little bit of everything
  • 6 ions compose over 99 of dissolved solids in
    seawater
  • NaCl make up over 85
  • This composition stays relatively the same
  • Rule of constant proportions
  • Why is this important?
  • Sea organisms rarely have to deal with changes in
    the ratios of various ions --gt easier to control
    their internal water/salt balance

20
How Salty is the Ocean?
  • Seawater has a salinity of 35 parts per thousand
    (ppt)
  • For every 1000 g of seawater --gt 35 g of salt
  • Exactly how salty is 35 ppt?

21
Thats a lot of salt . . .
  • If salt were removed from ocean and spread evenly
    over earths land surface, it would form a layer
    about 500 feet thick (the height of a 40-story
    office building)
  • How do the seas get so salty?
  • How did the seas get here in the first place?

22
Origin of the Oceans vid clip
23
Origin of the Oceans
  • 4 bya earth was large, hot rock w/out a trace of
    water
  • Outgassing
  • Releasing of gasses from mantle through volcanic
    activity
  • Comets and meteorites brought gasses as well
  • Methane, ammonia, water vapor, carbon dioxide
  • 3.8 bya, earths surface cooled below 100C --gt
    water condensed into rain and poured onto land
    for centuries
  • Water filled basins and gravity kept it there

24
Check with your neighbor about salt
  • Where does the salt in the oceans come from?
  • Why cant we drink salt water?
  • How does a whale, which is a mammal, survive in
    the ocean? Do they drink salt water?
  • Show Salty Water video clip (5 min)
  • Where does the ocean salt come from?

25
The Water Cycle
  • Quick review of the water cycle.
  • What does this mean?

26
Water Cycle
  • Rap or Folk song?

27
Cleopatra
  • Your drinking the same water Cleopatra bathed in
    over 2000 years ago! Yum!
  • Par 5 Demo to intro salinity, temperature, and
    density

28
Salinity, Temperature, Density Demo
  • Density ball demo Is cold water or hot water
    more dense?
  • Lets do a demo comparing all three of these
    things . . .
  • demo

29
Salinity, Temperature, and Density
  • Halocline
  • A layer of cold, salty water that acts as a
    barrier
  • Sea ice forms --gt releases salt --gt denser water
    sinks
  • Keeps warmer water from melting ice
  • Halocline animation (slow)

30
Halocline in cenotes
  • Also occurs in cenotes (freshwater caves)
  • This is Chak Mool, on the Yukatan peninsula in
    Mexico
  • More pics of Chak Mool

31
Salinity, Temperature, and Density
  • Thermocline
  • Layer of water where the temp changes rapidly
  • What causes this?
  • Solar radiation absorbed and mixed (waves and
    turbulence) evenly in the first 30-40 m
  • 90 of total ocean volume is below thermocline
  • Avgerage SST?
  • 62F
  • Average temp of the rest of ocean (below
    thermocline)?
  • 32-37 F

32
Salinity, Temperature, and Density
  • Temp decreases --gt ?
  • density increases
  • Salinity increases --gt?
  • density increases
  • Pycnocline
  • Layer where there is a rapid change in density

33
Bottom Line
  • Temp and salinity of seawater determine its
    density It gets denser as it gets saltier,
    colder, or both
  • How do scientists get these measurements?

34
How do we get this data?
  • CTD
  • Conductivity-temp-depth meters
  • Fig. 3.9 in text
  • Red arrow for water samples
  • Yellow arrow electronic instruments (temp,
    salinity, light, clarity)
  • CTD description

35
Dissolved Gases
  • How do fish breathe?
  • What are they filtering out of the water?
  • Dissolved oxygen
  • Seawater has dissolved gasses O2, CO2 (80!), N2
  • How much O2 in seawater?
  • 4-6 ml/l (less than 1)
  • In the air we breathe?
  • 210 ml/l of air or 21

36
Transperency
  • Seawater is relatively transparent. Why is this
    so important?
  • So photosynthetic organisms can grow
  • What colors are in sunlight?
  • Do they all travel equal distances?

37
True colors
  • Fig 3.12 in text at 30m (90ft) only blue light
    remains
  • With an electronic flash you see sea stars true
    colors
  • Can a plant photosynthesize at this depth if only
    blue light is present?

38
Pressure
  • At surface, how much pressure?
  • Tin can demo
  • 1 ATM or 14.7 lbs/in2
  • Every 10m (33ft) of increased depth --gt 1 ATM
  • How much pressure on a organisms that dives to
    100m?
  • 14.7psi x 11 161 psi
  • What happens if that organisms surfaces too
    quickly?

39
Fig 3.15 in text swim bladder blows up like a
balloon because of decreased pressure.
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