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chapter 14 liquid and solids

Discover why liquids and solids behave the way they do, including their intermolecular forces, phase changes, and energy requirements. Explore the unique properties of water and its phase changes. Learn about evaporation and vapor pressure.

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chapter 14 liquid and solids

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  1. chapter 14liquid and solids

  2. what is the deal with liquids and solids? why do they do the things they do? • unlike gases, why do they cling? and why are they so dense? and why do solids keep their shape? • and, it takes a little E to melt things (sl) but a lot of E to boil (lg); why???

  3. liquids and solids are not too much different from each other • when a liquid becomes a solid it becomes denser (except water!)

  4. 14.1 intermolecular forces • but why is water a liquid? • intermolecular forces! forces between - not within - molecules • there are three types…

  5. polar molecules get together b/c of mutual attraction • the ∂+ of one is attracted to the ∂- of the other

  6. they’ll find the best orientation, too, for maximum “stickiness” • called dipole-dipole attraction • only about 1% as strong as covalent

  7. hydrogen bonding • the HeMan of intermolecular forces, a special breed of dipole-dipole, is hydrogen bonding • guess which element plays a big role here? • hydrogen! but only when hooked up to certain other atoms…

  8. when H is hooked up to N, O, or F poor little H is so small that it nearly loses its electron • this makes it an extra strong ∂+ • this makes an really strong dipole-dipole…

  9. then the water molecules, in this case, have a strong attraction for each other • their attraction is called an H-bond • represented by------ lines • [not true bonds, just really strong attractions]

  10. happens also with molecules which have N-H and F-H bonds • above: water, ethanol, ammonia are all H-bonding • it’s the reason they all are liquids when they aren’t suppose to be (i.e. their friends w/o H-bonding are all gases)

  11. it has a great affect on the properties of those H-bonded things by making them cling to each other stronger • so, e.g. boiling points shoot through the roof b/c it is so hard to separate them

  12. londondispersionforces • what about nonpolar substances? how can they be attracted to each other and form a liquid? • they are attracted by london dispersion forces • some atoms, although nonpolar overall can experience temporary, instantaneous dipoles…

  13. this is unbelievably short-lived and extremely weak but it adds up (like Velcro!)

  14. can happen to nonpolar molecules, too • they have to be slooow and close for any significant effect, but… • large critters (e.g. I2) can do it more easily b/c of all the electrons involved

  15. 14.2 water and its phase changes • dang if water ain’t… like… everywhere! • oceans, land, atmosphere, life… • it’s colorless, odorless, tasteless • on Earth it is a solid, liquid, & gas

  16. one can heat water and its T rises (duh.) • but when its T reaches 100˚C its T rise stops! • when 1 atm of air is pressing on the water @ 100˚C, it begins to boil • = normal boiling point • what’s this got to do with i/m forces?patience!

  17. this heating thing can be shown on a heating/cooling curve

  18. notice the water follows a left to right path when it is heated • when it is cooled, it goes right to left

  19. notice when cooling that as the water reaches 0˚C its T levels out again (called a plateau) • this is normal freezing point • ice and liquid can co-exist at this T • but take the Tbelow O˚C,it freezes • above, it melts

  20. freezing water takes on unique shape; further apart than liquid •  density of ice is less than liq water • explains potholes, weathering of rocks, water pipes, antifreeze, ice on lakes, etc., etc.

  21. 14.3 energy requirements for the changes of state • remember phase changes are physical, not chemical, changes

  22. heating curves can help us keep an inventory on all the energy used to change phases…

  23. let’s pretend! • a piece of ice at-10˚C can be warmed! (A) • notice as it reaches 0˚C, the line goes flat even though energy is still being pumped in… (B) • hmmmm… where is the E going?

  24. water T stays cnst at O°C b/c E is being used to overcome H bonding! • = phase change! • the E required to change 1 mol ice to 1 mol liquid = molar heat of fusion • when all water is melted T begins to rises again... (C)

  25. @ 100 ° C, boiling occurs, T remains cnst (D) • molar heat of vaporization = E to turn 1 mol water liquid to 1 mol vapor • = phase change! • much greater value b/c takes a lot of E to move waters from each other b/c of H-bonding • when all liquid gone, water vapor gets heated…(E)

  26. heating curve = all physical changes! • cooling curve is exact reverse • sweating for cooling & harmful steam burns explained by all these “heats of…”

  27. water absorbs a lot of heat for a given raise in temp - a lot! • heat capacity = thermal energy required to raise temp of one kg of a substance one kelvin • water’s h/c is so great b/c it takes a lot of E to overcome H-bonding •  water takes a longtime to give off heatwhen cooling, a longtime to absorb heatwhen warming • ( nicer weathernear ocean)

  28. 14.4 evaporation and vapor pressure • open a container of liquid and the liquid can evaporate • it overcomes the i/m forces and escapes to the atm • this process is called vaporization (aka evaporation)

  29. evaporation can’t “just happen,” molecules need a minimal amt of E • see how there is a whole range of KE above

  30. in a cooler liquid sample a few have enough E to leave • at higher T more have the E to leave

  31. if those critters with enough E happen to be at the surface they go to vapor! • as the higher E molecules leave, the avg E of the leftovers is less, so it is cooler • meaning, evaporation causes cooling (e.g. sweating, fingernail polish on skin, etc.)

  32. vapor pressure • OK, now if we close that sample (aka closed system) it still evaporates, but! • as time goes on some just eventually return - condensation

  33. finally there will come a time when# leaving =# coming back • to our eyes it’s over (macroscopic) • really it’s very dynamic (microscopic) • but all these new guys cause a P

  34. this pressure is called vapor pressure • the greater the i/m force the less likely it is to be a vapor and the smaller the vp

  35. a barometer can be used to measure it

  36. high vp’s are called volatile and have wimpy im forces • lower vp’s mean strong attraction, strong im forces • as to im forces:H-bond > dipole-dipole > london • so as to vp:london > dipole-dipole > H-bond

  37. imf is diff here • water has hiimf • ethanol lower • diethyl ether lowest

  38. example • which has largest VP? H2O or CH3OH • H2O has two OH bonds, methanol just one • so H2O sticks better and loses! • CH3OH has the higher VP

  39. example • which has largest VP? CH3OH or CH3CH2CH2CH2OH • both have OH, but! the big guy has all that london force going for it with all those extra atoms • so CH3CH2CH2CH2OH sticks better and loses! • CH3OH has the higher VP

  40. 14.5 boiling point & vapor pressure • what is going on when water boils? • why do the bubbles form? where are they coming from? • remember the atmosphere is pushing down hard on the water…

  41. water has some gas dissolved in it • imagine water molecules “evaporating” into the tiny air bubble which is acting as a “birth place” for the bubble • if it is hot enough (i.e. enough KE) the water molecules can keep pressing out into a bigger bubble

  42. so boiling pointdepends on Tand P • BP is T at which vp = external P on liq • increased P will force them to stay together longer •  harder to boil •  BP goes up (and vise versa) • (like a radiator or pressure cooker!)

  43. so how does elevation affect BP? • the higher you go the less P • the less P, the less E water needs to make a bubble •  water boils at lower T at high altitudes…

  44. for freezing point P has little effect here, mostly a T thing • (reverse of freezing = melting; fp is same as mp) • wussy imf don’t hold the particles together well ( lo MP) • stronger imf hold the particles together longer ( hi MP) • (reverse of freezing =fusion)

  45. 14.6 the solid state:types of solids • solids are everywhere; some are cmpds, some elements • some mixtures, some pure • when a solid has a regular, patterned arrangement = crystalline solid • what makes up the crystals and how they are held together determines properties

  46. put together with ions and held by ionic bonds = ? • ionic solid! • when dissolved in water, they often break into ions

  47. molecular solids are molecules held together by i/m forces • when broken up they split into their molecules (not atoms!)

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