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Welcome to GCSE Edexcel Science revision.

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Unit C B 6: Plant structures and their functions.

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Plants and algae use photosynthesis to produce food and therefore biomass.

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They are producers, forming the starting point of many food chains.

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Photosynthesis transfers light energy into chemical energy stored in glucose.

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It is an endothermic process because it takes in energy.

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The word equation is carbon dioxide + water to glucose + oxygen.

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Light energy and chlorophyll are needed, but are not substances consumed in the equation.

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The balanced symbol equation is six C O two plus six H two O produces C six H twelve O six plus six O two.

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The carbon in glucose comes from carbon dioxide, rather than from soil minerals.

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Photosynthesis takes place in chloroplasts.

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Chlorophyll is a pigment that absorbs light energy; it is not the name of the organelle.

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Plants respire as well as photosynthesise.

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Respiration occurs in both light and dark, while photosynthesis requires light.

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Glucose can be used in respiration to transfer energy for cell processes, including active transport and growth.

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Plants join glucose molecules together to make starch for storage.

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Starch is insoluble, so it does not build up as dissolved sugar in the cell and draw in extra water by osmosis.

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Plants convert sugars into sucrose for transport to other parts of the plant.

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Stored starch can be broken down and the sugars used or converted for transport.

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Sugars transported to storage organs, such as potato tubers, can be converted into starch and used later.

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Glucose can supply material for cellulose in cell walls and for lipid production.

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Plants also combine carbon-containing substances with nitrogen from nitrate ions to make amino acids and proteins.

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Glucose, starch and sucrose have different roles: glucose is useful in respiration, starch is a storage carbohydrate, and sucrose is a transported sugar.

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Palisade cells near the upper surface of many leaves contain numerous chloroplasts.

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Their position and chloroplasts help them absorb light for photosynthesis.

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A stoma is a pore in the leaf surface; stomata is the plural.

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In many land plants, numerous stomata occur on the lower leaf surface.

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A pair of guard cells controls each stoma.

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When guard cells take up water by osmosis and become turgid, their shape changes and the pore opens.

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Guard-cell water content changes the pore opening; schematic surface views.

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When guard cells lose water and become less turgid, the pore closes.

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Their opening depends on environmental signals and water availability, rather than simply on water flow starting or stopping in the stem.

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During net photosynthesis, carbon dioxide diffuses into the leaf and oxygen diffuses out through stomata.

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These gases move down their concentration gradients.

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Water vapour can also diffuse out through an open stoma.

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Opening pores allows gas exchange but can increase water loss.

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Stomata commonly open in the light and close in darkness, but this is not an absolute rule for every plant or condition.

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Water transport does not simply stop at night.

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A limiting factor is the factor restricting the rate under the current conditions.

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The main factors considered here are light intensity, carbon dioxide concentration and temperature.

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Increasing light intensity increases the rate of photosynthesis while light is the limiting factor.

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When the graph levels off (forms a plateau), another factor, such as carbon dioxide or temperature, is limiting the rate.

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Increasing light raises the rate only while light is limiting.

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Increasing carbon dioxide concentration can increase the rate when carbon dioxide is limiting.

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Increasing a factor already in sufficient supply may have little effect.

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Photosynthesis involves enzyme-controlled reactions.

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Increasing temperature initially speeds reactions, but above an optimum the rate may fall as enzymes lose activity or denature.

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The limiting factors work together.

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For example, adding carbon dioxide may let the rate rise above a previous plateau, until another factor becomes limiting.

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Use the evidence in the question to identify the limiting factor.

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For a suitable small light source, light intensity is proportional to 1  divided by  distance squared.

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If the distance doubles, intensity becomes one quarter; if it triples, intensity becomes one ninth.

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The second light intensity divided by the first light intensity equals the first distance divided by the second distance, all squared.

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Moving a lamp from ten centimetres to twenty centimetres gives the intensity ratio of ten divided by twenty, all squared, which equals zero point two five.

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Photosynthesis rate is approximately proportional to light intensity only while light is limiting.

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Do not assume that halving distance always quadruples the rate at an existing plateau.

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Place a suitable piece of pondweed in water or a dilute sodium hydrogencarbonate solution, which supplies carbon dioxide.

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Use a lamp at measured distances to vary light intensity.

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Vary lamp distance while controlling other conditions; measure oxygen production over time.

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Estimate photosynthesis rate by counting bubbles released in a fixed time, or collect the gas and measure its volume per unit time.

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Oxygen production provides an indicator of photosynthesis rate.

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Allow the plant to adjust at each distance before measuring.

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Repeat readings and calculate a mean to reduce the effect of random variation.

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Keep temperature, carbon dioxide supply, pondweed species and size, and measurement time controlled.

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A lamp can also heat the water; monitor temperature and use an appropriate heat-control arrangement.

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Bubble counts are an estimate because bubbles can differ in size.

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Measuring gas volume is usually a better comparison than assuming that every bubble contains the same amount of gas.

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Rate  equals  gas volume  divided by  time.

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For example, 3 cubic centimetres of oxygen collected in 2 minutes gives a rate of 1.5 cubic centimetres per minute.

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Plot rate against light intensity, or use 1  divided by  distance squared as an estimate of relative intensity when appropriate.

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Interpret any plateau using limiting factors.

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Follow school practical instructions for handling glass, cutting pondweed and using electrical equipment near water.

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Keep the apparatus and procedure consistent between readings.

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A root hair cell has a long projection that provides a large surface area for absorbing water and mineral ions from the soil.

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A thin cell wall gives a short movement distance.

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A large surface area relative to volume helps exchange, but the cell membrane still controls what enters the cell.

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Water enters across the partially permeable cell membrane by osmosis when the surrounding solution has a higher water concentration than the cell contents.

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Mineral ions can be absorbed by active transport when their concentration is lower in the soil than inside the cell.

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Carrier proteins use energy transferred by respiration.

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Nitrate ions supply nitrogen for making amino acids and proteins.

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Water and mineral ions pass through root tissues into the xylem for transport through the plant.

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Water can move through cell-wall spaces as well as across cell membranes on its way through root tissues.

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Do not describe every step as osmosis; osmosis specifically involves a partially permeable membrane.

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Xylem carries water and mineral ions mainly upwards from roots to stems and leaves.

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Mature xylem vessel elements are dead and have no cytoplasm obstructing the passage.

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The vessel elements join end to end with their end walls lost or broken down, making a continuous hollow tube.

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Lignin strengthens xylem vessel walls and supports the plant.

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It also stops the vessels collapsing as water is pulled upwards under tension.

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Water evaporates from moist cell surfaces inside the leaf and water vapour diffuses through stomata into the surrounding air.

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This loss of water vapour is transpiration.

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Evaporation from leaves creates a pull on the continuous water column in the xylem.

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Water is drawn upwards to replace what is lost, creating the transpiration stream.

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Water arriving at leaves supplies photosynthesis, carries mineral ions and helps keep cells turgid.

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Evaporation can also contribute to cooling.

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If a plant loses water faster than it takes it up, its cells become less firm (lose turgor) and it may wilt.

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Closing stomata reduces water loss but also lets less carbon dioxide enter.

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Higher temperature usually increases evaporation and the rate of water loss, provided the plant has enough water and stomata remain open.

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Air movement removes humid air near the leaf, maintaining a steep water-vapour concentration gradient.

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Wind can therefore increase transpiration.

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Low humidity gives a steeper gradient between moist air inside the leaf and drier external air.

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High humidity generally reduces water loss.

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Light often promotes stomatal opening, increasing gas exchange and water loss.

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Drought responses or other limiting conditions can change this pattern.

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Compare conditions while controlling other variables.

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Explain each effect using evaporation, stomatal opening or the concentration gradient, rather than just stating that a plant drinks more.

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Phloem transports sucrose from sources (where sugar is made or released) to sinks (where sugar is used or stored).

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This movement of sugar is called translocation.

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A leaf carrying out photosynthesis can be a source.

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Growing roots, fruits and storage organs can be sinks.

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A storage organ becomes a source when its stored carbohydrate is broken down and released as sugar.

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Phloem contains living sieve-tube elements joined together.

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Sieve plates have pores allowing sap to pass between elements; companion cells support their activity.

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Companion cells contain mitochondria and use energy in sugar loading and unloading.

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Phloem transport depends on living cells, unlike the water-conducting elements of xylem.

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Different phloem tubes can carry sugars upwards or downwards according to source and sink locations.

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Do not treat phloem as an exclusively downward flow.

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Compare tissues clearly: xylem transports water and mineral ions through lignified dead vessels; phloem transports sucrose using living tissue and energy.

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Phloem direction varies between tubes and source–sink arrangements; arrows compare possible directions, not simultaneous opposite flow in one tube.

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A potometer measures water uptake by a leafy shoot.

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Uptake can estimate transpiration because much of the water is lost through leaves, but some is used or retained by the plant.

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In a bubble potometer, measure how far an air bubble moves along a capillary tube in a known time.

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Keep the apparatus airtight and watertight and allow conditions to stabilise.

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Movement rate  equals  distance divided by time.

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A bubble moving 30 millimetres in 5 minutes has a rate of 6 millimetres per minute.

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If the capillary cross-sectional area is known, water volume taken up  equals  area times distance moved.

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Use consistent units before dividing the volume by time.

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For a capillary area of 0.5 square millimetres and a bubble movement of 20 mm, uptake is 10 cubic millimetres.

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Over 2 minutes, the volume uptake rate is 5 cubic millimetres per minute.

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Repeat readings under each condition and calculate a mean.

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Reset the bubble consistently and compare one environmental variable at a time; use results as uptake estimates, not exact direct measurements of evaporation.

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That completes Plant structures and their functions.

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Revisit the notes and test yourself on the revision website.
