Structure: hydrophobic nonpolar tail region and hydrophilic polar head.
Form a bilayer in water, with heads interacting with water and tails forming a water-free zone.
The bilayer is stabilized by weak van der Waals bonds between tails.
Fluid Mosaic Model:
The membrane is composed of phospholipids, proteins, and cholesterol in motion.
Fluid because components move laterally.
Mosaic because it's composed of a variety of pieces.
Proteins in the Cell Membrane:
Transmembrane proteins: hydrophobic core fits into the nonpolar membrane portion, hydrophilic regions extend into the cytoplasm.
Integral proteins: nonpolar region extends into the hydrophobic membrane middle, hydrophilic region juts into the cytoplasm or cell exterior.
Peripheral proteins: attach to phospholipid heads on the cytoplasmic side of the membrane or in the cell exterior.
Membrane Transport
Diffusion:
Molecules spread out from high to low concentration.
Spontaneous and driven by kinetic energy.
Molecules flow down a concentration gradient.
Passive Transport:
Requires no cellular energy.
Simple diffusion: small nonpolar molecules (oxygen, carbon dioxide) and nonpolar substances (steroid hormones, fats) diffuse directly across the bilayer.
Facilitated diffusion: polar molecules and ions require protein channels.
Active Transport:
Pumps molecules or ions up their concentration gradient (from low to high concentration).
Requires energy expenditure (usually ATP).
Endocytosis and Exocytosis:
Both are forms of bulk transport and require energy.
Endocytosis: the membrane pinches in to surround particles or extracellular fluid, creating a vesicle.
Exocytosis: a vesicle fuses with the membrane, dumping its contents outside the cell.
Membrane Potential:
Electrical charge across a membrane that creates a voltage difference.
Created by cells expending energy to pump ions across membranes.
Example: Mitochondria pump protons from the matrix to the intermembrane space, creating a charge gradient that drives ATP synthesis.
Tonicity and Osmoregulation
Osmosis: The diffusion of water from high to low concentration.
Water flows from hypotonic (more water, less solute) to hypertonic (less water, more solute) solutions.
Osmotic pressure: The force of water being pushed up on one side due to osmosis.
Osmosis in Plant Cells:
Hypotonic environment: water leaves the cell, causing plasmolysis and wilting.
Isotonic environment: water enters and leaves at the same rate.
Hypertonic environment: water flows into the cell, causing turgor pressure and making the cell firm.
Osmosis in Animal Cells:
Hypotonic environment: water leaves the cell, causing it to shrivel.
Isotonic environment: water enters and leaves at the same rate (important for animal cells).
Hypertonic environment: water flows into the cell, causing it to burst.
Contractile Vacuole:
Freshwater protists use contractile vacuoles to osmoregulate.
The vacuole fills with water and contracts to expel water from the cell.
Leaf Stomata:
Pores on the underside of a leaf formed by two guard cells.
When water is sufficient, guard cells buckle outward, creating a pore for gas exchange.
Stomata can close in response to environmental cues, including water stress.
Guard cells are regulated by pumping potassium ions in (opening) and out (closing) in response to water availability.
Water Potential:
A measure of water's tendency to move from one area to another.
Adding solute decreases water potential, adding pressure increases it.
Water flows from areas of higher water potential to areas of lower water potential.
Formula: \Psi = \Psis + \Psip where \Psi is water potential, \Psis is solute potential, and \Psip is pressure potential.