1. CHAPTER 3 CONT’D- WATER 9/2/2014

2. WARM-UP 5 MINUTES TO COMPLETE EXPLAIN HOW WATER IS TRANSPORTED FROM THE ROOTS OF A TREE TO THE LEAVES. IN YOUR EXPLANATION, MAKE SURE TO INCLUDE AND DEFINE ‘HYDROGEN BONDS’ AND ‘COHESION’

3. HOMEWORK READ CHAPTER 22, PP 452-460 DRAW THE BEAKS OF THE FINCHES ON PAGE 457, FIGURE 22.6 AND EXPLAIN WHY THE BEAKS ARE DIFFERENT SHAPES PRINT OUT THE CLOVER STUDY DOCUMENT POSTED ON THE CLASS WIKI PAGE MAKE SURE YOUR MASTERING BIOLOGY ACCOUNT WORKS B/C OUR FIRST ONLINE ASSIGNMENT IS DUE THIS THURSDAY MAKE SURE YOU CAN ACCESS THE ETEXT MAKE SURE YOU HAVE ACCESS TO OUR COURSE PAGE, CALLED DRCAOBIOLOGY MAKE SURE YOUR STUDENT ID IS ENTERED!!! THIS IS IMPORTANT FOR GRADES

4. EVIDENCE FOR LIFE ON MARS?

5. THE REMARKABLE PROPERTIES OF WATER SUPPORT LIFE ON EARTH IN MANY WAYS ASTROBIOLOGISTS SEEKING LIFE ON OTHER PLANETS ARE CONCENTRATING THEIR SEARCH ON PLANETS WITH WATER TO DATE, MORE THAN 200 PLANETS HAVE BEEN FOUND OUTSIDE OUR SOLAR SYSTEM; ONE OR TWO OF THEM CONTAIN WATER IN OUR SOLAR SYSTEM, MARS HAS BEEN FOUND TO HAVE WATER POSSIBLE EVOLUTION OF LIFE ON OTHER PLANETS WITH WATER

6. HEAT AND TEMPERATURE KINETIC ENERGY IS THE ENERGY OF MOTION HEAT IS A MEASURE OF THE TOTAL AMOUNT OF KINETIC ENERGY DUE TO MOLECULAR MOTION TEMPERATURE MEASURES THE INTENSITY OF HEAT DUE TO THE AVERAGE KINETIC ENERGY OF MOLECULES

7. WATER’S HIGH SPECIFIC HEAT THE SPECIFIC HEAT OF A SUBSTANCE IS THE AMOUNT OF HEAT THAT MUST BE ABSORBED OR LOST FOR 1 G OF THAT SUBSTANCE TO CHANGE ITS TEMPERATURE BY 1ºC THE SPECIFIC HEAT OF WATER IS 1 CAL/G/ºC WATER RESISTS CHANGING ITS TEMPERATURE BECAUSE OF ITS HIGH SPECIFIC HEAT

8. WATER’S HIGH SPECIFIC HEAT CAN BE TRACED TO HYDROGEN BONDING HEAT IS ABSORBED WHEN HYDROGEN BONDS BREAK HEAT IS RELEASED WHEN HYDROGEN BONDS FORM THE HIGH SPECIFIC HEAT OF WATER MINIMIZES TEMPERATURE FLUCTUATIONS TO WITHIN LIMITS THAT PERMIT LIFE

9. FIGURE 3.5 Santa Barbara 73° Los Angeles (Airport) 75° Pacific Ocean 68° Santa Ana 84° Burbank 90° San Bernardino 100° Palm Springs 106° Riverside 96° San Diego 72° 40 miles 70s (°F) 80s 90s 100s Why is it useful for water to absorb heat?

10. https://www.polleverywhere.com/multiple_choice_polls/v5lyNhj 7nhLOSwj

11. 2. WATER HAS AN UNUSUALLY HIGH SPECIFIC HEAT. THIS IS DIRECTLY RELATED TO WHICH ONE OF THE FOLLOWING? A)AT ITS BOILING POINT, WATER CHANGES FROM LIQUID TO VAPOR. B) MORE HEAT IS REQUIRED TO RAISE THE TEMPERATURE OF WATER. C) ICE FLOATS IN LIQUID WATER. D) SALT WATER FREEZES AT A LOWER TEMPERATURE THAN PURE WATER. E) FLOATING ICE CAN INSULATE BODIES OF WATER.

12. 2. WATER HAS AN UNUSUALLY HIGH SPECIFIC HEAT. THIS IS DIRECTLY RELATED TO WHICH ONE OF THE FOLLOWING? A) AT ITS BOILING POINT, WATER CHANGES FROM LIQUID TO VAPOR. B) MORE HEAT IS REQUIRED TO RAISE THE TEMPERATURE OF WATER. C) ICE FLOATS IN LIQUID WATER. D) SALT WATER FREEZES AT A LOWER TEMPERATURE THAN PURE WATER. E) FLOATING ICE CAN INSULATE BODIES OF WATER.

13. EVAPORATIVE COOLING AS A LIQUID EVAPORATES, ITS REMAINING SURFACE COOLS, A PROCESS CALLED EVAPORATIVE COOLING EVAPORATIVE COOLING OF WATER HELPS STABILIZE TEMPERATURES IN ORGANISMS AND BODIES OF WATER

14. FROZEN WATER WATER EXPANDS AS IT SOLIDIFIES AT 0 DEGREES, HYDROGEN ATOMS LOCKED INTO CRYSTALLINE LATTICE, EACH WATER MOLECULE HYDROGEN-BONDED TO FOUR MOLECULES.

15. FIGURE 3.6 Hydrogen bond Ice: Hydrogen bonds are stable Liquid water: Hydrogen bonds break and re-form

16. FLOATING OF ICE ON LIQUID WATER ICE FLOATS IN LIQUID WATER BECAUSE HYDROGEN BONDS IN ICE ARE MORE “ORDERED,” MAKING ICE LESS DENSE WATER REACHES ITS GREATEST DENSITY AT 4°C IF ICE SANK, ALL BODIES OF WATER WOULD EVENTUALLY FREEZE SOLID, MAKING LIFE IMPOSSIBLE ON EARTH

17. WATER: THE SOLVENT OF LIFE A SOLUTION IS A LIQUID THAT IS A HOMOGENEOUS MIXTURE OF SUBSTANCES EXAMPLE: SUGAR WATER A SOLVENT IS THE DISSOLVING AGENT OF A SOLUTION THE SOLUTE IS THE SUBSTANCE THAT IS DISSOLVED AN AQUEOUS SOLUTION IS ONE IN WHICH WATER IS THE SOLVENT

18. FIGURE 3.7 Cl  Na                    

19. WATER IS A VERSATILE SOLVENT DUE TO ITS POLARITY, WHICH ALLOWS IT TO FORM HYDROGEN BONDS EASILY WHEN AN IONIC COMPOUND IS DISSOLVED IN WATER, EACH ION IS SURROUNDED BY A SPHERE OF WATER MOLECULES CALLED A HYDRATION SHELL

20. HYDROPHILIC AND HYDROPHOBIC SUBSTANCES A HYDROPHILIC SUBSTANCE IS ONE THAT HAS AN AFFINITY FOR WATER A HYDROPHOBIC SUBSTANCE IS ONE THAT DOES NOT HAVE AN AFFINITY FOR WATER OIL MOLECULES ARE HYDROPHOBIC BECAUSE THEY HAVE RELATIVELY NONPOLAR BONDS

21. SOLUTE CONCENTRATION IN AQUEOUS SOLUTIONS MOST BIOCHEMICAL REACTIONS OCCUR IN WATER CHEMICAL REACTIONS DEPEND ON COLLISIONS OF MOLECULES AND THEREFORE ON THE CONCENTRATION OF SOLUTES IN AN AQUEOUS SOLUTION

22. NUMBERS OF MOLECULES ARE USUALLY MEASURED IN MOLES, WHERE 1 MOLE (MOL) = 6.02 X 10 23 MOLECULES MOLARITY (M) IS THE NUMBER OF MOLES OF SOLUTE PER LITER OF SOLUTION M = MOLES LITER

23. FIGURE 3.UN02 2 H 2 O Hydroxide ion (OH  ) Hydronium ion (H 3 O + ) +  Hydrogen atoms between two water molecules can Shift from one to another WATER IS IN A STATE OF DYNAMIC EQUILIBRIUM IN WHICH WATER MOLECULES DISSOCIATE AT THE SAME RATE AT WHICH THEY ARE BEING REFORMED

24. ACIDS AND BASES AN ACID IS ANY SUBSTANCE THAT INCREASES THE H + CONCENTRATION OF A SOLUTION A BASE IS ANY SUBSTANCE THAT REDUCES THE H + CONCENTRATION OF A SOLUTION © 2011 Pearson Education, Inc.

25. The pH Scale In any aqueous solution at 25°C, the product of H + and OH – is constant and can be written as The pH of a solution is defined by the negative logarithm of H + concentration, written as For a neutral aqueous solution, [H + ] is 10 –7, so [H + ][OH – ] = 10 –14 pH = –log [H + ] pH = –(–7) = 7

26. FIGURE 3.10 pH Scale Battery acid Gastric juice, lemon juice Vinegar, wine, cola Beer Tomato juice Black coffee Rainwater Urine Saliva Pure water Human blood, tears Seawater Inside of small intestine Milk of magnesia Household ammonia Household bleach Oven cleaner Basic solution Neutral solution Acidic solution 0 1 2 3 4 5 6 7 8 9 10 Neutral [H + ] = [OH  ] Increasingly Basic [H + ] < [OH  ] Increasingly Acidic [H + ] > [OH  ] H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ OH  H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ 11 12 13 14 pH declines as [H + ] increases!

27. ACIDIC SOLUTIONS HAVE PH VALUES LESS THAN 7 BASIC SOLUTIONS HAVE PH VALUES GREATER THAN 7 MOST BIOLOGICAL FLUIDS HAVE PH VALUES IN THE RANGE OF 6 TO 8

28. BUFFERS THE INTERNAL PH OF MOST LIVING CELLS MUST REMAIN CLOSE TO PH 7 BUFFERS ARE SUBSTANCES THAT MINIMIZE CHANGES IN CONCENTRATIONS OF H + AND OH – IN A SOLUTION MOST BUFFERS CONSIST OF AN ACID-BASE PAIR THAT REVERSIBLY COMBINES WITH H + EX: CARBONIC ACID

29. H 2 CO 3 ↔ HCO 3 – + H + Carbonic acid Bicarbonate ion Hydrogen ion

30. https://www.polleverywhere.com/multiple_choice_polls/SFn4RO E8I9VdVH2

31. 3. THE CHEMICAL EQUILIBRIUM BETWEEN CARBONIC ACID AND BICARBONATE ACTS AS A PH REGULATOR IN OUR BLOOD. IF THE BLOOD PH BEGINS TO RISE, WHAT WILL HAPPEN? H 2 CO 3 ↔ HCO 3 – + H + CARBONIC ACID BICARBONATE ION HYDROGEN ION A) REACTION PROCEEDS TO THE RIGHT; MORE CARBONIC ACID DISSOCIATES B) REACTION PROCEEDS TO THE RIGHT; MORE CARBONIC ACID FORMS C) REACTION PROCEEDS TO THE LEFT; MORE CARBONIC ACID DISSOCIATES D) REACTION PROCEEDS TO THE LEFT; MORE CARBONIC ACID FORMS

32. 3. THE CHEMICAL EQUILIBRIUM BETWEEN CARBONIC ACID AND BICARBONATE ACTS AS A PH REGULATOR IN OUR BLOOD. IF THE BLOOD PH BEGINS TO RISE, WHAT WILL HAPPEN? H 2 CO 3 ↔ HCO 3 – + H + CARBONIC ACID BICARBONATE ION HYDROGEN ION A) REACTION PROCEEDS TO THE RIGHT; MORE CARBONIC ACID DISSOCIATES B) REACTION PROCEEDS TO THE RIGHT; MORE CARBONIC ACID FORMS C) REACTION PROCEEDS TO THE LEFT; MORE CARBONIC ACID DISSOCIATES D) REACTION PROCEEDS TO THE LEFT; MORE CARBONIC ACID FORMS

33. ACIDIFICATION: A THREAT TO WATER QUALITY HUMAN ACTIVITIES SUCH AS BURNING FOSSIL FUELS THREATEN WATER QUALITY CO 2 IS THE MAIN PRODUCT OF FOSSIL FUEL COMBUSTION ABOUT 25% OF HUMAN-GENERATED CO 2 IS ABSORBED BY THE OCEANS CO 2 DISSOLVED IN SEA WATER FORMS CARBONIC ACID; THIS PROCESS IS CALLED OCEAN ACIDIFICATION

34. FIGURE 3.11 CO 2 CO 2 + H 2 OH 2 CO 3 H + + HCO 3  H + + CO 3 2  HCO 3  CaCO 3 CO 3 2  + Ca 2+ H 2 CO 3 Ocean acidification = less coral calcification

35. AS SEAWATER ACIDIFIES, H + IONS COMBINE WITH CARBONATE IONS TO PRODUCE BICARBONATE CARBONATE IS REQUIRED FOR CALCIFICATION (PRODUCTION OF CALCIUM CARBONATE) BY MANY MARINE ORGANISMS, INCLUDING REEF-BUILDING CORALS

36. EXIT TICKET WHY DOES ICE FLOAT ON WATER? WHAT WOULD HAPPEN IF ICE SUNK? EXPLAIN. WHAT IS PH? WHAT DOES IT MEAN WHEN PH IS LESS THAN 7, EQUAL TO 7, AND GREATER THAN 7?