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Consortium for Educational Communication Frequently asked questions (FAQs) Q.1. Define osmosis and what are its types? Ans: Osmosis is special type of diffusion of a liquid, when solvents move through a semipermeable membrane from a place of higher diffusion pressure to a place of lower diffusion pressure. In other words, when the two solutions having different osmotic concentrations are separated by means of a semipermeable membrane, the molecules of water (or solvent) move from the region of its higher chemical potential to the region of its lower chemical potential. This movement of water (or solvent) is called osmosis. Depending upon the movement of water into or outward of the cell, osmosis is of two types: • Endosmosis: The osmotic inflow of water into a cell, when it is placed in a solution, whose solute concentration is less than the cell sap, is called endosmosis e.g., swelling of resins when they are placed in water. • Exosmosis: the osmotic outflow of water from a cell, when it is placed in solution, whose solute concentation is more than the cell sap, is called exosmosis e.g., shrinkage of grapes when they are placed in strong sugar solution. Q.2. Define different types of solutions and activity of plant cell when placed in them. Ans: Hypotonic: the solution outside has lower solute concentration than inside the cell. When Plant cell is placed in this type of solution it swells up and becomes turgid. Hypertonic: the solution outside has higher solute concentration than inside the cell. When Plant cell is placed in this type of solution it shrinks and becomes flaccid. Isotonic: the solution has the same concentration of water and solutes as inside a cell. No change takes place in a plant cell when Consortium for Educational Communication placed in isotonic solution. Q.3. List several factors that influence the rate of diffusion. Ans: Factors affecting the rate of diffusion: 1. Gradient of Concentration 2. Permeability of membrane 3. Temperature 4. Pressure 5. Density 6. Diffusion pressure gradient Q.4. Explain briefly the diffusion pressure deficit. Ans: Each liquid has a specific diffusion pressure. Pure water or pure solvent has the maximum diffusion pressure. If some solute dissolved into it, the water or solvent in the resulting solution comes to attain less diffusion pressure than that of pure water or pure solvent. In other words, diffusion pressure of a solvent, in a solution is always lower than that in the pure solvent. ‘The amount by which the diffusion pressure of water or solvent in a solution is lower than that of pure water or solvent is known as diffusion pressure deficit (DPD)’. Because of the presence of the diffusion pressure deficit, a solution will always tend to make up the deficit by absorbing water. Hence, diffusion pressure deficit is the water absorbing capacity of a solution. Therefore, DPD can also be called suction pressure (SC). Q.5. In what ways diffusion is important to a plant? Ans: Diffusion is important to a plant in following ways: i). Gaseous exchange during the process of photosynthesis and Consortium for Educational Communication respiration takes place by the principal of independent diffusion. ii). The process of diffusion is involved in the transpiration of water vapours. iii). The ions are absorbed by the simple diffusion during passive salt uptake. iv). Diffusion is an effective means of transport over very short distances and helps in translocation of food materials. Q.6. What are the main applications of osmosis? Ans: Osmosis is of immense importance to plants. i). The phenomenon of osmosis is important in the absorption of water by plants. ii). Cell to cell movement of water occurs through out the plant body due to osmosis. iii). The rigidity of plant organs (i.e., shape and form of organisms) is maintained through osmosis. iv). Leaves become turgid and expand due their osmotic pressure. v). Growing point of root remain turgid because of osmosis, and are thus able to penetrate the soil particles. vi). The resistance of plants to drought and frost is brought about by osmotic pressure of their cells. vii). Movement of plants and plant parts, for example, movement of leaflets of Indian telegraph plant, bursting of many fruits and sporangia, etc. involve changes in turgor which are brought about by osmosis. Consortium for Educational Communication viii). Opening and closing of stomata is affected by osmosis. ix). Growth of young cells is brought about by the osmotic pressure and turgor pressure of these cells. Q.7. Distinguish between Diffusion and Osmosis. Ans: The main differences between diffusion and osmosis are: Diffusion Osmosis 1. Diffusion is a movement of a 1. Osmosis is a special type of diffusion given substance from the place of its of solvent molecules such as water higher concentration to an area of its from lower lesser concentration. concentration to higher concentration of solution when the two are separated by a semi permeable membrane. 2. The diffusion may occur in any medium. 2. It occurs in liquid medium and only the solvent molecules such as water The moving particles may be solid, move from one place to another . liquid 3. Presence of semipermeable or gas. membrane in between the two solutions 3. Presence of semipermeable is required. membrane is not required. Q.8. Describe briefly the main pathways of movement of water in plants. Ans: Water in the root moves through three pathways such as apoplast pathway, symplast pathway and transmembrane pathways. i. Apoplast pathway: The apoplastic movement of water occurs exclusively through the cell wall without crossing any membrane. ii.Symplast pathway: The symplastic movement of water occurs from cell to cell through the plasmodesmata. Consortium for Educational Communication iii. Transmembrane pathway: Water after passing through cortex is blocked by casparian strips present on endodermis. However, some of the endodermal cells located opposite to protoxylem elements are found to be free from casparian thickening and they act as free passage cells. Thus water ultimately finds its way into xylem elements. In this pathway, water enters a cell on one side and then moves into the next cell. It means that water has to pass through two membranes in each cell i.e., once while entering the cell and the second time while leaving the cell. Here, water may also enter through tonoplast surrounding the vacuole i.e., also called as vacuolar pathway. Q.9. Explain why pure water has the maximum water potential. Ans: Water molecules possess kinetic energy. In liquid and gaseous form they are in random motion that is both rapid and constant. The greater the concentration of water in a system, the greater is its kinetic energy or ‘water potential’. Hence, it is obvious that pure water will have the greatest water potential. If two systems containing water are in contact, random movement of water molecules will result in net movement of water molecules from the system with higher energy to the one with lower energy. Thus water will move from the system containing water at higher water potential to the one having low water potential. This process of movement of substances down a gradient of free energy is called diffusion. Water potential is denoted by the Greek symbol Psi or Ψ and is expressed in pressure units such as pascals (Pa). By convention, the water potential of pure water at standard temperatures, which is not under any pressure, is taken to be zero. Q.10. Briefly describe water potential. What are the factors affecting it? Ans: Water potential is the potential energy of water relative to Consortium for Educational Communication pure free water (e.g. deionized water) in reference conditions. It quantifies the tendency of water to move from one area to another due to osmosis, gravity, mechanical pressure, or matrix effects including surface tension. Water potential is measured in units of pressure and is commonly represented by the Greek letter Ψ (Psi). This concept has proved especially useful in understanding water movement within plants, animals, and soil. Typically, pure water at standard temperature and pressure (or other suitable reference condition) is defined as having a water potential of 0. The addition of solutes to water lowers its potential (makes it more negative), just as the increase in pressure increases its potential (makes it more positive). If possible, water will move from an area of higher water potential to an area that has lower water potential. One very common example is water that contains a dissolved salt, like sea water or the solution within living cells. These solutions typically have negative water potentials, relative to the pure water reference. If there is no restriction on flow, water molecules will proceed from the locus of pure water to the more negative water potential of the solution. Water potential of a cell is affected by both solute and pressure potential. The relationship between them is as follows: Ψw = Ψs + Ψp Q. 11. Discuss briefly the role of water in plant life. Ans: water palys a great role in plant life, they may be discussed as follows: a)Nearly 80% of the fresh weight of the plant tissues is comprised of water and it is vital for the structural integrity of biological molecules participating either directly or indirectly in all metabolic activities of plants. Consortium for Educational Communication b)Water also serve as vital function as a solvent for the various molecules transported within the plant and is involved in the development and maintenance of cell turgidity on which organism’s growth and development depend. c)Water serves as a medium for the movement of various dissolved substances like gases, minerals, organic solutes, etc., through the xylem and phloem. d)Cell turgidity is maintained by water. e)Water takes part in various condensing and hydrolyzing reactions, as for example, in the formation and breakdown of starch. Q. 12. Describe the active absorption of water in plants. Ans: Active absorption of water: It is absorption of water by roots with the help of metabolic energy generated by the root respiration. The force for water absorption originates from the cells of root due to root respiration. As the root cells actively take part in the process so it is called Active absorption. According to Renner, active absorption takes place in low transpiring and wellwatered plants and 4% of total water absorption is carried out in this process. The active absorption is carried out by two theories which are: a. Active osmotic water absorption, b. Active non-osmotic water absorption. Active osmotic water absorption: This theory was given by Atkins (1916) and Priestley (1921). According to this theory, the root cells behave as ideal osmotic system through which water moves up from soil solution to root xylem along an increasing gradient of D.P.D. (suction pressure which is the real force for water Consortium for Educational Communication absorption). If solute concentration is high and water potential is low in the root cells, water can enter from soil to root cells through endosmosis. Mineral nutrients are absorbed actively by the root cells due to utilization of ATP. As a result, the concentration of ions in the xylem vessels is more in comparison to the soil water. A concentration gradient is established between the root and the soil water. Hence, the solute potential of xylem water is more in comparison to that of soil and correspondingly water potential is low than the soil water. Otherwise stated, water potential is comparatively positive in the soil water. This gradient of water potential causes endosmosis. The endosmosis of water continues till the water potential both in the root and soil becomes equal. It is the absorption of minerals that utilize metabolic energy, but not water absorption. Hence, absorption of water is indirectly an active process. Active non-osmotic water absorption: This theory was given by Thimann (1951) and Kramer (1959). According to the theory, sometimes water is absorbed against concentration gradient. This requires expenditure of metabolic energy released from respiration of root cells. There is no direct evidence, but some scientists suggest involvement of energy from respiration. In conclusion it is said that, the evidences supporting active absorption of water are themselves poor. Q.13. what are the various forms of water present in soil? Ans: The plants absorb water through the root hairs from the soil. The soil contains water in following forms: • Gravitational water: When the water enters the soil and passes the spaces between the soil particles and reaches the water table, the type of soil water is called gravitational water. In fact Consortium for Educational Communication gravitational water is surplus to the water retaining capacity of soil and drains from it to reach in deep saturated zone of earth i.e., ground water, upper surface of which is called water table. • Capillary water: It is the water which is held around soil particles in the capillary space present around them due to force like cohesion and surface tension. This is the water which can be utilised by the plants. It is also called growth water. It occurs in the form of films coating smaller soil particle. The availability of capillary water to the plant depend upon its diffusion pressure deficit which is termed as the soil moisture stress. The plant cells much have a DPD more than the soil moisture stress for proper absorption of water. • Hygroscopic water: This is the form of water which is held by soil particles of soil surfaces. The water is held tightly around the soil particles due to cohesive and adhesive forces. Hygroscopic water cannot be easily removed by the plants. Cohesive and adhesive forces greatly reduce the water protential (Ψw) and thus this type of water in soil is not available to plants. • Run away water: After the rain, water does not enter the soil at all, but drained of along the slopes. It is called run away water. The quantity of runaway water is controlled by factors like permeability of soil, moisture content of soil, degree of slope and number of ditches present in that area. Plants fail to avail this water. • Chemically combined water: Some of the water molecules are chemically combined with soil minerals (e.g., silicon, iron, aluminium, etc.). This water is not available to the plants. Q.14. Describe the main areas of Root Involved in Absorption and Translocation of Water. Ans: The zone of rapid water absorption usually lies some 20 – Consortium for Educational Communication 200mm from the root tip behind the meristem, where the xylem is not fully mature and the epiblema as well as the endodermis are still permeable. This area is usually characterized by the presence of root hairs which serve to increase the area of contact between the root surface and soil. However, presence of root hair is not essential for water absorption. Some roots, such as adventitious roots of bulbs, corms and rhizomes and those of some aquatic plants and gymnosperms do not have root hairs. The zone of rapid water absorption moves along with the growth of root, as the older cells become suberized and lose their ability to absorb water. Q.15. Highlight the various factors affecting the rate of water absorption in plants. Ans: The factors affecting the rate of transpiration, water potential of root system and that of the soil, influence the rate of the water absorption. The rate of water absorption by land plants is affected by the following external and internal factors: 1. External factors: a)Available soil water b)Concentration of soil solution c)Soil aeration d)Soil temperature 2. Internal factors a)Efficiency of root system b)Metabolic activity of root c)Osmotic potential of root hair d)Transpiration