Outline for revision DIFFUSION, OSMOSIS, ACTIVE TRANSPORT
SIMPLE DIFFUSION SIMPLE DIFFUSION (or just diffusion) is a PASSIVE PROCESS requires no outside energy, using KINETIC ENERGY in SOLUTES Solutes move from a region of HIGH concentration to a region of LOW concentration (along a concentration gradient) A difference in the concentration of a substance between two places is called a concentration gradient or in this case a diffusion gradient NET movement of solutes continues until equilibrium is reached Once molecules have distributed evenly the system reaches equilibrium and diffusion stops Molecules still move but equal numbers move in each direction Diffusion can occur in open systems or across membranes
THE RATE OF DIFFUSION Is DIRECTLY proportional to the SURFACE AREA of the membrane CONCENTRATION gradient TEMPERATURE Is INVERSELY proportional to the DISTANCE (e.g. thickness of the exchange surface)
EXAMPLES OF DIFFUSION: Oxygen diffusing from the alveoli in the lungs into the red blood cells in the capillaries Oxygen diffusing from the red blood cells into the muscles Oxygen diffusing from air spaces in the soil into root hair cells Carbon dioxide diffusing from the air around leaves into the leaf for photosynthesis Oxygen produced by photosynthesis moving from the leaf into the air Carbon dioxide produced by respiration diffusing from the muscles into the red blood cells
ACTIVE TRANSPORT ACTIVE TRANSPORT (or just diffusion) is a ACTIVE PROCESS that requires energy from respiration Solutes move from a region of LOW concentration to a region of HIGH concentration (i.e. against a concentration gradient)
EXAMPLES OF ACTIVE TRANSPORT: Mineral ions are absorbed from soil water, where they are at low concentrations, into root hair cells where there are at high concentration. Oxygen in the soil is needed to the cells do aerobic respiration to provide energy for this process. Active transport is also needed in the kidney to reabsorb glucose into the blood
OSMOSIS OSMOSIS (or just diffusion) is a PASSIVE PROCESS that requires no outside energy, using only KINETIC ENERGY in WATER Is the net movement of water from a region of higher water potential to lower water potential across a semipermeable membrane. High water potential: where a solution is dilute, in other words is relatively little solute. Low water potential: resolution is concentrated, in other words as a large amount of solute.
TONICITY Hypertonic = lower water potential, more solute Isotonic = same water potential, same solute concentration Hypotonic = higher water potential, less solute
EXAMPLES OF OSMOSIS: Root hair cells have a higher concentration of minerals than the soil water around them. In other words, they are hypertonic to the soil water the soil is hypotonic (higher water potential) so water moves from the soil into the root hair cell. Vacuoles in plant cells, for example leaf palisade cells, contain cell sap, which contains a high solute concentration. Water fills the cell by osmosis to maintain turgor – making the cells stiff enough to support the leaf
TURGOR & PLASMOLYSIS TURGOR The hypertonic vacuole fills with water, pressing the cytoplasm against the cell wall. FLACCIDITY When the plant cells receive too little water, the surroundings do not have as much water potential as they did. the vacuoles are no longer hypertonic to their surroundings. The vacuoles do not absorb water and the cells lose their turgor. the cells become soft – or flaccid – and no longer support the tissues of the plant, so it wilts. PLASMOLYSIS When the vacuoles shrink extremely, the cytoplasm pulls away from the cell wall, showing gaps. The cell is now in a plasmolysed state.
OSMOREGULATION In animals (including humans), if the blood is more dilute than the tissues (is hypotonic, i.e higher water potential) water moves into the tissues from the blood. Keeping tissue and blood concentration normal is important - and is called osmoregulation (The mechanism shown for controlling the concentration of the blood comes in the section about homeostasis and the kidney)