Plasma Membrane
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Transcript Plasma Membrane
The Plasma Membrane and
Homeostasis
FLUID MOSAIC MODEL
Homeostasis – Maintaining
a Balance
Cells must keep the proper
concentration of nutrients and water
and eliminate wastes.
The plasma membrane is selectively
permeable – it will allow some things
to pass through, while blocking other
things.
Amphipathic: hydrophobic & hydrophilic
regions
Singer-Nicolson: fluid mosaic model
COMPONENTS OF CELL MEMBRANE
Phospholipids: membrane
fluidity
Cholesterol: membrane
stabilization
“Mosaic” Structure:
Integral proteins:
transmembrane proteins
Peripheral proteins: surface
of membrane
Membrane carbohydrates :
cell to cell recognition;
oligosaccharides (cell
markers); glycolipids;
glycoproteins
Structure of the Plasma
Membrane
Lipid bilayer – two sheets of lipids
(phospholipids).
Found around the cell, the nucleus,
vacuoles, mitochondria, and
chloroplasts.
Embedded with proteins and
strengthened with cholesterol
molecules.
What’s a Phospholipid?
It’s a pair of fatty acid chains and a
phosphate group attached to a glycerol
backbone.
Polar (water-soluble) heads face
out and the nonpolar fatty acids
hang inside.
Membrane Proteins
Transport: what
can enter/leave
cell.
Serve as enzymes
Signal transduction
(ie. Hormones)
Intercellular joining
Cell-cell recognition
(T-cells)
ECM attachment
Cellular Transport
Diffusion – movement of particles from
an area of high concentration to an area
of low concentration.
Caused by Brownian motion (movement of
particles because of the movement of their
atoms).
Continues until an equilibrium is reached (no
gradient).
Dynamic equilibrium – particles move freely
and are evenly distributed.
Osmosis
Diffusion of
water across a
selectively
permeable
membrane.
Occurs until
water is balanced
on both sides of
the membrane.
Cell Concentrations
Hypertonic solutions – more
dissolved solute. (less water)
Hypotonic solutions – less dissolved
solute. (more water)
Isotonic solutions – the same
dissolved solute.
QUESTION: What happens to the cell
in each situation?
Osmoregulation
Osmoregulation: control of
water balance
Hypertonic: higher
concentration of solutes
Hypotonic: lower
concentration of solutes
Isotonic: equal
concentrations of solutes
Cells with Walls:
Turgid (very firm)
Flaccid (limp)
Plasmolysis: plasma
membrane pulls away from
cell wall
Overcoming Osmosis
Contractile vacuoles – expel
excess water from bacterial
cells that live in water.
Turgor pressure – water
pressure in a plant cell. Loss
of turgor pressure causes
wilting (plasmolysis).
Cellular Transport
Passive transport – (also known as
passive diffusion) no energy is
needed to move particles.
Facilitated diffusion – embedded
proteins act as tunnels allowing
particles to “fall” through.
Requires the use of transport
proteins
Ion channels: specialized
transport proteins
Many ions are not soluble in lipids
To enter the cell, they need to go through a protein
“tunnel” to get into the cell
Examples: Na+, K+, Ca+2, Cl-
These protein “tunnels” have “gates” that open or close
to allow ions into the cell or to leave the cell
Again, this depends on the concentration gradient
Stimuli in the cell determine when the gates open or
close
Cellular Transport
Active transport – energy is
needed to move particles.
Carrier proteins –
embedded proteins
change shape to open
and close passages
across the membrane.
This system allows the
cell to move substances
from a lower
concentration to a higher
concentration
Example: Sodium-potassium pump
The sodium-potassium pump is one of the active
transport mechanisms used in the conduction of a
nerve impulse.
How it works: (open book to pg. 135)
Three Na+ ions (inside the cell) bind to a protein in the
cell membrane
2. You must use energy to move the Na+ ions out of the
cell so an ATP molecule is used (energy molecule) to
change the shape of the carrier protein
3. With a phosphate is bound to the carrier protein it has
“space” for two K+ to bind to the protein
1.
Sodium-potassium pump
4. When the two K+ bind to the carrier protein, the
protein again changes shape by releasing the
phosphate and allows the K+ to enter the cell
NOTE: Another driving force for the pump is an
attempt to maintain a balanced electric charge
You lose 3+ so it’s easier to add + into the cell
SHOWS HOW YOU CAN COUPLE TRANSPORTS
TO SAVE ENERGY
Sodium-potassium pump
ENDOCYTOSIS VS EXOCYTOSIS
There are two other ways to move substances into and
out of the cell:
Endocytosis: the cell ingests external substances
(macromolecules, external fluid, other cells)
The cell membrane engulfs the substance and forms a
vesicle
The substance inside the vesicle is kept separate from
the rest of the cell by the phospholipid bilayer of the
vesicle
These substances can be transported to the lysosome for
digestion or other membrane-bound organelles for
other functions
ENDOCYTOSIS – CONT.
Types of endocytosis
Pinocytosis: this creates a vesicle that is transporting
fluids
Phagocytosis: creates a vesicle that transports large
particles or other cells
Example: Your immune system creates a type of
phagocyte (cell that digests foreign bacteria) called a
macrophage that helps to fight off bacterial infections
Receptor-mediated endocytosis: ligands (molecules that
bind to a specific receptor site) induce endocytosis
EXOCYTOSIS
Exocytosis: when a substance is released from the cell by
binding a vesicle to the plasma membrane
This process is basically the reverse of endocytosis
This process is used for
Elimination of large molecules from the cell (they are
large enough that they would damage the cell
membrane if allowed to leave through the plasma
membrane)
Elimination of toxins that need to be kept separate
from cell interior
Many endocrine cells use this method to release
hormones
WATER POTENTIAL
On the AP Exam, you will have to understand a couple
of formulas that deal with water potential:
Ψ = ΨP + ΨS
Ψ = Free energy associated with water potential
ΨP = Pressure potential (force from water pressure)
ΨS = Potential dependent on the solute concentration
(how many particles of material are in solution
WATER POTENTIAL
Water always moves from an area of high water
potential to low water potential (osmosis)
In an open beaker (atmospheric pressure only) of PURE
water, the water potential is zero (Ψ = 0)
No difference is solute concentration
No external pressure (gravity, turgor pressure, etc)
Increasing the ΨP (pressure potential), increases the
water potential (Ψ > 0)
The water wants to “move” to an area of lower pressure
(potential)
WATER POTENTIAL
Increasing the ΨS (solute potential), lowers the water
potential
If you put more particles in solution, you make the
solution hypertonic
The water wants to enter the system to equalize the water
potential (Ψ < 0)
The total water potential results from a combination of
water pressure and solute concentration
SOLUTE POTENTIAL
Solute potential (ΨS) has its own formula
ΨS = -iCRT
i = ionization constant (different based on the
material used for the solute)
C = the molar concentration (molarity = moles/L)
R = pressure constant (0.0831 liters*bars/mole*K)
T = temperature in Kelvin (K = ̊C + 273)
Bar = 1 atm (at sea level)
EXAMPLE PROBLEM
A sample of 0.15M sucrose at atmospheric pressure
(ΨP = 0) and 25 ̊C has what water potential? Since
sucrose dose not break apart into ions (i = 1).
SOLUTION
Ψ=?
Ψ = ΨP +ΨS
ΨP = 0
ΨS = -iCRT
i=1
C = 0.15M
R = 0.0831
liters*bars/mole*K
T = 25 ̊C + 273 = 298K
Ψ = o +ΨS
ΨS = -iCRT
ΨS = - (1)(0.15M)(0.0831)(298K)
ΨS = -3.7 bars
Ψ = o +ΨS
Ψ = o -3.7bars
Ψ = -3.7bars