Presentation is loading. Please wait.

Presentation is loading. Please wait.

Phytoremediation Plant products Biofuels

Similar presentations


Presentation on theme: "Phytoremediation Plant products Biofuels"— Presentation transcript:

1 Phytoremediation Plant products Biofuels Effects of seed spacing on seed germination Effects of nutrient deprivation Effects of stresses Climate/CO2 change Non-coding RNAs Biotechnology Plant movements: flytraps, mimosa, soybeans Carnivorous plants Stress responses/stress avoidance Plant signaling (including neurobiology) Flowering? Hormones? Plant pathology? Plant tropisms and nastic movements Root growth responses Metal toxicity? Circadian rhythms? Effects of magnetic fields? Effects of different colors of light on plant growth?

2 Assignment 1 Pick a topic that you think is worth studying Try to convince the group in 5-10 minutes why yours is best Why it is significant what is known/what isn’t known Some plants that we might use Some experiments that we could perform by the end of the semester.

3 Endomembrane system Organelles derived from the ER 1) ER 2) Golgi 3) Vacuoles 4) Plasma Membrane 5) Nuclear Envelope 6) Endosomes 7) Oleosomes

4 endosymbionts Peroxisomes Mitochondria 3) Plastids

5 cytoskeleton network of proteins which give cells their shape also responsible for shape of plant cells because guide cell wall formation left intact by detergents that extract rest of cell

6 WATER Plants' most important chemical most often limits productivity

7 Climate change will alter rainfall
Overall prediction is that crops will suffer in many parts of world

8 WATER Plants' most important chemical most often limits productivity Often >90% of a plant cell’s weight

9 WATER Plants' most important chemical most often limits productivity Often >90% of a plant cell’s weight Gives cells shape

10 WATER Plants' most important chemical most often limits productivity Often >90% of a plant cell’s weight Gives cells shape Dissolves many chem

11 WATER Dissolves many chem most biochem occurs in water Source of e- for PS

12 WATER most biochem occurs in water Source of e- for PS Constantly lose water due to PS (1000 H2O/CO2)

13 WATER most biochem occurs in water Source of e- for PS Constantly lose water due to PS Water transport is crucial!

14 WATER Water transport is crucial! SPAC= Soil Plant Air Continuum moves from soil->plant->air

15 Plant Water Uptake Water is drawn through plants along the SPAC, using its special props to draw it from the soil into the air

16 WATER Formula = H2O Formula weight = 18 daltons Structure = tetrahedron, bond angle 104.5˚

17 WATER Structure = tetrahedron, bond angle 104.5˚ polar: O is more attractive to electrons than H + on H - on O

18 Water Polarity is reason for water’s properties water forms H-bonds with polar molecules

19 Water Polarity is reason for water’s properties water forms H-bonds with polar molecules Hydrophilic = polar molecules Hydrophobic = non-polar molecules

20 Properties of water Cohesion = water H-bonded to water

21 Properties of water Cohesion = water H-bonded to water -> reason for surface tension

22 Properties of water Cohesion = water H-bonded to water -> reason for surface tension -> why water can be drawn from roots to leaves

23 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else

24 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else capillary action

25 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else capillary action why things dissolve in water

26 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else Cohesion and adhesion are crucial for water movement in plants!

27 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else Cohesion and adhesion are crucial for water movement in plants! Surface tension & adhesion in mesophyll creates force that draws water through the plant!

28 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat absorb heat when break H-bonds: cools leaves

29 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat absorb heat when break H-bonds Release heat when form H-bonds

30 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats

31 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent

32 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent Take up & transport nutrients dissolved in water

33 Properties of water 5) “Universal” solvent Take up & transport nutrients dissolved in water Transport organics dissolved in water

34 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent 6) Hydrophobic interactions

35 Properties of water 1) Cohesion = water H-bonded to water 2) Adhesion = water H-bonded to something else 3) high specific heat 4) Ice floats 5) Universal solvent 6) Hydrophobic interactions 7) Water ionizes

36 pH [H+] = acidity of a solution pH = convenient way to measure acidity pH = - log10 [H+] pH 7 is neutral: [H+] = [OH-] -> at pH 7 [H+] = 10-7 moles/l pH of cytoplasm = 7.2 pH of stroma & matrix = 8 pH of apoplast = 5.5 pH of lumen = 4.5

37 pH Plants vary pH to control many processes!

38 pH Plants vary pH to control many processes! Plants alter roots to aid uptake

39 Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Driving force?

40 Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Driving force: lowers free energy ∆G = ∆H- T∆S

41 Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient

42 Water movement Diffusion: movement of single molecules down ∆[ ] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆ [ ] !

43 Water movement Diffusion: movement of single molecules down ∆[] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆[ ] ! How water moves through xylem

44 Water movement Diffusion: movement of single molecules down [] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆ [ ] ! How water moves through xylem How water moves through soil and apoplast

45 Water movement Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆ [ ] ! How water moves through xylem Main way water moves through soil and apoplast Very sensitive to radius of vessel: increases as r4

46 Water movement Diffusion: movement of single molecules down ∆[] due to random motion until [ ] is even Bulk Flow: movement of groups of molecules down a pressure gradient Independent of ∆[ ] ! How water moves through xylem Main way water moves through soil and apoplast Very sensitive to radius of vessel: increases as r4 Osmosis: depends on bulk flow and diffusion!

47 Water movement Osmosis: depends on bulk flow and diffusion! water crosses membranes but other solutes do not water tries to even its [ ] on each side

48 Water movement Osmosis: depends on bulk flow and diffusion! water crosses membranes but other solutes do not water tries to even its [ ] on each side other solutes can’t: result is net influx of water

49 Water movement Osmosis: depends on bulk flow and diffusion! Moves through aquaporins, so rate depends on pressure and [ ] gradients!

50 Water movement Osmosis: depends on bulk flow and diffusion! Moves through aquaporins, so rate depends on pressure and [ ] gradients! Driving force = water's free energy (J/m3 = MPa)

51 Water potential Driving force = water's free energy = water potential Yw Important for many aspects of plant physiology

52 Water potential Driving force = water's free energy = water potential Yw Water moves to lower its potential

53 Water potential Driving force = water's free energy = water potential Yw Water moves to lower its potential

54 Water potential Driving force = water's free energy = water potential Yw Water moves to lower its potential Depends on: [H2O]: Ys (osmotic potential)

55 Water potential Water moves to lower its potential Depends on: [H2O]: Ys (osmotic potential) Pressure : Yp Turgor pressure inside cells

56 Water potential Water moves to lower its potential Depends on: [H2O]: Ys (osmotic potential) Pressure : Yp Turgor pressure inside cells Negative pressure in xylem!

57 Water potential Water moves to lower its potential Depends on: [H2O]: Ys (osmotic potential) Pressure Yp Gravity Yg Yw = Ys +Yp + Yg

58 Water potential Water moves to lower its potential Depends on: [H2O]: Ys (osmotic potential) Pressure Yp Gravity Yg Yw = Ys +Yp + Yg Yw of pure water at sea level & 1 atm = 0 MPA

59 Water potential Yw = Ys +Yp + Yg Yw of pure water at sea level & 1 atm = 0 MPA Ys (osmotic potential) is always negative

60 Water potential Yw = Ys +Yp + Yg Yw of pure water at sea level & 1 atm = 0 MPA Ys (osmotic potential) is always negative If increase [solutes] water will move in

61 Water potential Yw = Ys +Yp + Yg Yw of pure water at sea level & 1 atm = 0 MPA Ys (osmotic potential) is always negative If increase [solutes] water will move in Yp (pressure potential) can be positive or negative

62 Water potential Yw = Ys +Yp + Yg Yw of pure water at sea level & 1 atm = 0 MPA Ys (osmotic potential) is always negative If increase [solutes] water will move in Yp (pressure potential) can be positive or negative Usually positive in cells to counteract Ys

63 Water potential Yp (pressure potential) can be positive or negative Usually positive in cells to counteract Ys Helps plants stay same size despite daily fluctuations in Yw

64 Water potential Yw = Ys +Yp + Yg Yp (pressure potential) can be positive or negative Usually positive in cells to counteract Ys Helps plants stay same size despite daily fluctuations in Yw Yp in xylem is negative, draws water upwards

65 Water potential Yw = Ys +Yp + Yg Yp (pressure potential) can be positive or negative Usually positive in cells to counteract Ys Helps plants stay same size despite daily fluctuations in Yw Yp in xylem is negative, draws water upwards Yg can usually be ignored, but important for tall trees

66 Water potential Measuring water potential

67 Water potential Measuring water potential Ys (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells

68 Water potential Measuring water potential Ys (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells Yg (gravity potential) is easy: height above ground -0.01 Mpa/m

69 Water potential Measuring water potential Ys (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells Yg (gravity potential) is easy: height above ground YP (pressure potential) is hard! Pressure bomb = most common technique

70 Water potential Measuring water potential Ys (osmotic potential) is “easy” Measure concentration of solution in equilibrium with cells Yg (gravity potential) is easy: height above ground YP (pressure potential) is hard! Pressure bomb = most common technique Others include pressure transducers, xylem probes

71 Measuring water potential
YP (pressure potential) is hard! Pressure bomb = most common technique Others include pressure transducers, xylem probes Therefore disagree about H2O transport in xylem

72 Water transport Therefore disagree about H2O transport in xylem Driving force = evaporation in leaves (evapotranspiration) Continuous H2O column from leaf to root draws up replacement H2O from soil (SPAC)

73 Water transport Driving force = evaporation in leaves (evapotranspiration) Continuous H2O column from leaf to root draws up replacement H2O Exact mech controversial

74 Water transport Driving force = evaporation in leaves (evapotranspiration) Continuous H2O column from leaf to root draws up replacement H2O Exact mech controversial Path starts at root hairs

75 Water transport Path starts at root hairs Must take water from soil

76 Water transport Path starts at root hairs Must take water from soil Ease depends on availability & how tightly it is bound

77 Water transport Path starts at root hairs Must take water from soil Ease depends on availability & how tightly it is bound Binding depends on particle size & chem

78 Water transport Must take water from soil Ease depends on availability & how tightly it is bound Binding depends on particle size & chem Availability depends on amount in soil pores

79 Water transport Availability depends on amount in soil pores Saturation: completely full

80 Water transport Availability depends on amount in soil pores Saturation: completely full Field capacity: amount left after gravity has drained excess

81 Water transport Availability depends on amount in soil pores Saturation: completely full Field capacity: amount left after gravity has drained excess Permanent wilting point: amount where soil water potential is too negative for plants to take it up


Download ppt "Phytoremediation Plant products Biofuels"

Similar presentations


Ads by Google