BIOS 3755: Human Physiology - Membrane Transport
Overview
Course Code: BIOS 3755
Topic: Human Physiology
Date: January 15, 2026
Reading Material: Vander Chapter 4
Major Topics Covered
Diffusion
Magnitude and Direction of Diffusion
Diffusion Rate Versus Distance
Diffusion Through Membranes
Mediated-Transport Systems
Facilitated Diffusion
Active Transport
Osmosis
Osmolarity, Tonicity, and Cell Volume
Epithelial Transport
Cystic Fibrosis
Diffusion
General Characteristics:
Molecules in solution move at a velocity of approximately 100\text{ m/sec}.
Average center-to-center distance between water molecules is about 2.85 \text{ \AA} (2.85 \times 10^{-10} \text{ meters}).
Molecules frequently change direction upon colliding with others, leading to limited distance travel.
Definition of Diffusion:
The passive movement of particles from an area of high concentration to low concentration.
Effectiveness decreases over larger distances due to limitations in the rate of diffusion.
Diffusion Through Membranes:
Diffusion rates through membranes are significantly slower—ranging from 1,000 to 1,000,000 times compared to diffusion through an equivalent thickness of water.
The hydrophobic interior of the lipid bilayer of membranes is a primary limiting factor for diffusion.
Membrane Structure
Phospholipid Components:
Head: Hydrophilic (water-attracting)
Tails: Hydrophobic (water-repelling)
Basic structure includes choline, phosphate, and hydrocarbon chains.
Cross-Membrane Diffusion:
Small Hydrophobic Molecules: e.g., O2, CO2, N_2, benzene
Small Uncharged Polar Molecules: e.g., H_2O, glycerol, ethanol
Larger Uncharged Polar Molecules and Ions: e.g., amino acids, glucose, nucleotides (like H^+, Na^+, HCO_3^-, K^+, Ca^{2+}, Cl^-, Mg^{2+})
Types of Membrane Transport
Simple Diffusion:
Movement down an electrochemical gradient.
No energy required.
Facilitated Diffusion:
Involves pores, channels, and carriers for molecules.
Movement still occurs down electrochemical gradient, non-energy dependent.
Active Transport:
Requires transport molecules and energy input.
Movement against the electrochemical gradient.
Rate of Diffusion
Permeability Coefficient:
An experimentally determined measure reflecting how easily a molecule can move through a specific membrane.
Formula: J = PA(Co−Ci) where:
J = Flux (rate of diffusion)
P = Permeability coefficient
A = Area of the membrane
C_o = Concentration on one side
C_i = Concentration on the other side
Fick’s Law: Describes the flow of solutes in relation to concentration gradients and permeability.
Michaelis-Menten Equation for Facilitated Diffusion
Transport equation: T = ([S]⋅Tmax)/(Kt+[S])
Where:
T = Velocity of transport
T_{max} = Maximal transport velocity
[S] = Substrate concentration
Kt = Substrate concentration at ½ Tmax (indicates transporter affinity).
Ion Channels and Their Properties
Pores: Low selectivity, always open, allow flow based on size.
Channels: More selective, gated opening based on stimuli:
Ligand-gated: Open when a ligand binds.
Voltage-gated: Open with changes in electrical potential.
Tonicity and Osmolarity
Key Definitions:
Osmolarity: Total concentration of all solute particles (penetrating + non-penetrating).
Tonicity: The effect of a solution on cell volume; determined only by non-penetrating solutes.
Penetrating Solutes: e.g., urea; cross the membrane and equilibrate.
Non-penetrating Solutes: e.g., Na^+, Cl^-; cannot cross membrane, drive osmosis.
Example Problems and Breakdowns:
Scenario 1: Pure Non-penetrating Solute (NaCl)
Problem: A cell with 300\text{ mOsm} non-penetrating solutes is placed in 400\text{ mOsm} NaCl.
Breakdown: NaCl is non-penetrating. Since outside concentration (400) is greater than inside (300), the solution is hypertonic. Water moves out.
Result: Cell shrinks.
Scenario 2: Mixing Penetrating and Non-penetrating Solutes
Problem: A cell (300\text{ mOsm} non-penetrating) is placed in a solution of 300\text{ mOsm} non-penetrating solutes + 100\text{ mOsm} urea.
Breakdown: Total osmolarity is 400\text{ mOsm} (hyperosmotic). However, urea penetrates and equilibrates. Tonicity depends only on the 300\text{ mOsm} non-penetrating solutes. Since 300 = 300, there is no net water movement.
Result: Isotonic; volume remains unchanged.
Scenario 3: Hypotonic Solution
Problem: A cell (300\text{ mOsm} non-penetrating) is placed in a solution of 200\text{ mOsm} non-penetrating solutes and 200\text{ mOsm} urea.
Breakdown: Total osmolarity is 400\text{ mOsm}. However, tonicity is only 200\text{ mOsm}. Since 200 < 300, the outside is hypotonic. Water moves into the cell.
Result: Cell swells.
Cystic Fibrosis
Description: Genetic disorder causing thick mucus production due to mutations in the CFTR protein (\Delta F508).
Error of Mechanisms and Membrane Transport:
Chloride Transport Defect: Defective CFTR fails to transport Cl^- ions out of the cell.
Sodium Hyper-absorption: Dysfunction of CFTR leads to overactivity of ENaC (Epithelial Sodium Channel), causing excessive Na^+ reabsorption into the cell.
Osmotic Imbalance: The high intracellular concentration of Na^+ and lack of extracellular Cl^- creates an osmotic gradient that pulls water out of the airway surface liquid (ASL) and into the cell via osmosis.
Pathophysiology: Resulting dehydration of the ASL leads to viscous mucus that traps bacteria and impairs ciliary clearance.
Conclusion
Understanding membrane transport (diffusion, osmolarity, tonicity) is fundamental to both normal physiology and clinical conditions such as cystic fibrosis and fluid management.