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CHAP. 2 CHEMICAL FACTORS PGS. 33-37 AND 40-55 ACTIVITIES- Ice Coring Sample, Thermal Stratification, Geological Time Scale.

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Presentation on theme: "CHAP. 2 CHEMICAL FACTORS PGS. 33-37 AND 40-55 ACTIVITIES- Ice Coring Sample, Thermal Stratification, Geological Time Scale."— Presentation transcript:

1 CHAP. 2 CHEMICAL FACTORS PGS. 33-37 AND 40-55 ACTIVITIES- Ice Coring Sample, Thermal Stratification, Geological Time Scale

2 I. PROPERTIES OF WATER A. hydrogen bonds- holds molecules together with weak chemical bridges polar molecule high heat capacity viscosity = “thickness” surface tension

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4 B. density- mass/vol. provides buoyancy expansion of water at 0ºC temperature influences density

5 Bond width expands

6 II. COMPOSITION OF SEA WATER dissolved inorganic particles (salts) dissolved organic (nutrients)

7 dissolved gases suspended particles

8 A. salts NaCl Principle of Constant Proportion –(see handout) ions per 1000 g of water Cl, Na, S, Ca, K =99 % 86% salinity = 1.8050 x chlorinity

9 B. Dissolved gases O 2, CO 2,N 2 fig. 2-7 in text

10 B. Dissolved gases O 2, CO 2,N 2 fig. 2-7 in text Gas is more soluble in cold water O 2 enters from the atmosphere and photosynthesis Anaerobic= without oxygen

11 III. THERMAL STRATIFICATION water layered by temperature- 25 0 C to 4 0 C Thermocline - narrow region of rapid temperature change

12 Spring Turn over SUMMER

13 Spring Turn over FALL

14 Spring Turn over WINTER

15 Spring Turn over SPRING

16 Nutrients are brought up from the bottom Oxygen is carried down to aid in aerobic respiration

17 IV. LIGHT ABSORPTION 65% of light is absorbed in the first meter "heats water" colors are selectively absorbed absorption depends on suspended particles in the water

18 Why is the ocean BLUE? colors are selectively absorbed by the water molecules Blue light penetrates the furthest RED LIGHT penetrates the least

19 absorption depends on suspended particles in the water –Reflection of light occurs too! Each area has its own absorption and reflection profile –estuaries, –open ocean –continental shelf

20 V. BUFFERING the ability of a liquid to resist pH change with the addition of acid pH scale 1-14 log scale sea water typically 7.5-8.4 CO 2 is the main influencing agent on pH Large amounts of CO 2 can be stored in sea water because it is converted into other compounds

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22 Test Topics for Friday Ocean chemistry properties of water (polarity, density, viscosity,etc. distribution of components -be able to draw graphs (light, temp, oxygen) Geological time scale (Era names and dates) important marine events Chap 2 text PGS. 33-37 AND 40-55

23 Geological Time Scale

24 Nonconformity in the Grand Canyon - Sediments deposited over Schist JUST ADMIRE THE PICTURE

25 Names are given to times in the past that have been marked by a significant change in the fossil and rock record

26 Correlation of rock layers Matching strata of similar ages in different regions is called correlation http://www.uwsp.edu/geo/faculty/ozsvath/images/stratigraphy.jpg

27 Geologic Timescale Divisions based on fossils Eon, Era, Period, Epoch Homework Learn Timescale.doc less Epochs

28 Origin of Period Names


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