Osmosis
Osmosis is the movement of water molecules through a selectively-permeable membrane down a water potential gradient.[1] More specifically, it is the movement of water across a selectively permeable membrane from an area of high water potential (low solute concentration) to an area of low water potential (high solute concentration). It may also be used to describe a physical process in which any solvent moves, without input of energy, across a semipermeable membrane (permeable to the solvent, but not the solute) separating two solutions of different concentrations.[2] Osmosis releases energy, and can be made to do work,[3] but is a passive process, like diffusion.
Net movement of solvent is from the less-concentrated (hypotonic) to the more-concentrated (hypertonic) solution, which tends to reduce the difference in concentrations. This effect can be countered by increasing the pressure of the hypertonic solution, with respect to the hypotonic. The osmotic pressure is defined to be the pressure required to maintain an equilibrium, with no net movement of solvent. Osmotic pressure is a colligative property, meaning that the osmotic pressure depends on the molar concentration of the solute but not on its identity.
Osmosis is important in biological systems, as many biological membranes are semipermeable. In general, these membranes are impermeable to organic solutes with large molecules, such as polysaccharides, while permeable to water and small, uncharged solutes. Permeability may depend on solubility properties, charge, or chemistry, as well as solute size. Water molecules travel through the plasma cell wall, tonoplast (vacuole) or protoplast in two ways, either by diffusing across the phospholipid bilayer directly, or via aquaporins (small transmembrane proteins similar to those in facilitated diffusion and in creating ion channels). Osmosis provides the primary means by which water is transported into and out of cells. The turgor pressure of a cell is largely maintained by osmosis, across the cell membrane, between the cell interior and its relatively hypotonic environment.[4]
The first recorded observation of osmosis was in 1748 by Jean-Antoine Nollet.[5] The word "osmosis" descends from the words "endosmose" and "exosmose", which were coined by French physician René Joachim Henri Dutrochet (1776-1847) from the Greek words ένδον (endon : within), έξο (exo : outside), and ωσμος (osmos : push, impulsion).[6][7][8][9]
Er ikke det som Rasmus siger.
Basic explanations
Osmosis may occur when there is a partially permeable membrane, such as a cell membrane. Impermeable means that the object doesn't allow things through it, so a membrane has to be permeable so food gets in and waste gets out. When a cell is submerged in water, the water molecules pass through the cell membrane from an area of low solute concentration (outside the cell) to one of high solute concentration (inside the cell); this is called osmosis. The cell membrane is selectively permeable, so only necessary materials are let into the cell and wastes are left out.[4]
When the membrane has a volume of pure water on both sides, water molecules pass in and out in each direction at exactly the same rate; there is no net flow of water through the membrane.
In a solution, the water is diluted (i.e., the concentration of water is lowered) by the presence of solute particles. If there is a solution on one side, and pure water on the other, there will be a higher concentration of water molecules on the pure water side of the membrane. Therefore, water molecules pass through the membrane from the pure water side toward the solution side more frequently than from the solution side going to the pure water side. This will result in a net flow of water to the side with the solution. Assuming the membrane does not break, this net flow will slow and finally stop as the pressure on the solution side becomes such that the movement in each direction is equal: dynamic equilibrium. This could either be due to the water potential on both sides of the membrane being the same, or due to osmosis being inhibited by factors such as pressure potential or osmotic pressure.
Osmosis can also be explained using the notion of entropy, from statistical mechanics. Suppose a permeable membrane separates equal amounts of pure solvent and a solution. Since a solution possesses more entropy than pure solvent, the second law of thermodynamics states that solvent molecules will flow into the solution until the entropy of the combined system is maximized. Notice that, as this happens, the solvent loses entropy while the solution gains entropy. Equilibrium, hence maximum entropy, is achieved when the entropy gradient becomes zero, and dissolution takes place.
Pure water is more ordered than water in a solution; thus, from an entropic standpoint it takes some net energy to move a water molecule from a disordered solution and "pack it in" with pure water. This is the same explanation as to why the disordered air does not spontaneously separate and order into oxygen and nitrogen, it would take energy for this to happen. Additionally, particle size has no bearing on osmotic pressure, as this is the fundamental postulate of colligative properties.[10]
Examples of osmosis
Osmotic pressure is the main cause of support in many plants. The osmotic entry of water raises the turgor pressure exerted against the cell wall, until it equals the osmotic pressure, creating a steady state.
When a plant cell is placed in a hypertonic solution, the water in the cells moves to an area higher in solute concentration and the cell shrinks, and in doing so, becomes flaccid. This means the cell has become plasmolysed - the cell membrane has completely left the cell wall due to lack of water pressure on it; the opposite of turgid.
Also, osmosis is responsible for the ability of plant roots to draw water from the soil. Since there are many fine roots, they have a large surface area, and water enters the roots by osmosis.
Osmosis can also be seen when potato slices are added to a high concentration of salt solution. The water from inside the potato moves to the salt solution, causing the potato to shrink and to lose its 'turgor pressure'. The more concentrated the salt solution, the bigger the difference in size and weight of the potato slice.
In unusual environments, osmosis can be very harmful to organisms. For example, freshwater and saltwater aquarium fish placed in water of a different salinity than that to which they are adapted to will die quickly, and in the case of saltwater fish, dramatically. Another example of a harmful osmotic effect is the use of table salt to kill leeches and slugs.
Suppose an animal or a plant cell is placed in a solution of sugar or salt in water.
- If the medium is hypotonic — a dilute solution, with a higher water concentration than the cell — the cell will gain water through osmosis.
- If the medium is isotonic — a solution with exactly the same water concentration as the cell — there will be no net movement of water across the cell membrane.
- If the medium is hypertonic — a concentrated solution, with a lower water concentration than the cell — the cell will lose water by osmosis.
Essentially, this means that if a cell is put in a solution which has a solute concentration higher than its own, then it will shrivel up, and if it is put in a solution with a lesser solute concentration than its own, the cell will expand and burst. Electronucleal exchange is the passive diffusion of cations and anions across a semi-permeable membrane according to electrical charge.
Chemical gardens demonstrate the effect of osmosis in inorganic chemistry.
Factors
Osmotic pressure
As mentioned before, osmosis may be opposed by increasing the pressure in the region of high solute concentration with respect to that in the low solute concentration region. The force per unit area, or pressure, required to prevent the passage of water through a selectively permeable membrane and into a solution of greater concentration is equivalent to the osmotic pressure of the solution, or turgor. Osmotic pressure is a colligative property, meaning that the property depends on the concentration of the solute, but not on its identity.
Osmotic gradient
The osmotic gradient is the difference in concentration between two solutions on either side of a semipermeable membrane, and is used to tell the difference in percentages of the concentration of a specific particle dissolved in a solution.
Usually the osmotic gradient is used while comparing solutions that have a semipermeable membrane between them allowing water to diffuse between the two solutions, toward the hypertonic solution (the solution with the higher concentration). Eventually, the force of the column of water on the hypertonic side of the semipermeable membrane will equal the force of diffusion on the hypotonic (the side with a lesser concentration) side, creating equilibrium. When equilibrium is reached, water continues to flow, but it flows both ways in equal amounts as well as force, therefore stabilizing the solution.
Variation
Reverse osmosis
Reverse osmosis is a separation process that uses pressure to force a solvent through a semipermeable membrane that retains the solute on one side and allows the pure solvent to pass to the other side. More formally, it is the process of forcing a solvent from a region of high solute concentration through a membrane to a region of low solute concentration by applying a pressure in excess of the osmotic pressure.
Forward osmosis
Osmosis may be used directly to achieve separation of water from a "feed" solution containing unwanted solutes. A "draw" solution of higher osmotic pressure than the feed solution is used to induce a net flow of water through a semipermeable membrane, such that the feed solution becomes concentrated as the draw solution becomes dilute. The diluted draw solution may then be used directly (as with an ingestible solute like glucose), or sent to a secondary separation process for the removal of the draw solute. This secondary separation can be more efficient than a reverse osmosis process would be alone, depending on the draw solute used and the feedwater treated. Forward osmosis is an area of ongoing research, focusing on applications in desalination, water purification, water treatment, food processing, etc.
See also
- Active Transport
- Diffusion
- Homeostasis
- Osmoregulation
- Osmotic shock
- Osmotic power
- Plasmolysis
- Salinity gradient power
- Water potential
- Brining
- Reverse osmosis plant
References
- ^ Haynie, Donald T. (2001). Biological Thermodynamics. Cambridge: Cambridge University Press. pp. 130–136. ISBN 0521795494.
- ^ "Osmosis".
- ^ "Statkraft to build the world's first prototype osmotic power plant".
- ^ a b Maton, Anthea (1997). Cells Building Blocks of Life. Upper Saddle River, New Jersey: Prentice Hall. pp. 66–67.
{{cite book}}: Unknown parameter|coauthors=ignored (|author=suggested) (help) - ^ L’Abbé Nollet (June 1748) “Recherches sur les causes du bouillonnement des liquides” (Researches on the causes of the boiling of liquids) Mémoires de Mathématique et de Physique, tirés des registres de l’Académie Royale des Sciences de l’année 1748, pages 57-104; see especially pages 101-103. The Mémoires (1748) were printed in: Histoire de l’Académie Royale des Sciences Année 1748, which was published in 1752 and which contains a condensed version of Nollet's article on pages 10-19.
Original text:Avant que de finir ce Mémoire, je crois devoir rendre compte d’un fait que je dois au hasard, & qui me parut d’abord ... singulier ....
... j’en avois rempli une fiole cylindrique, longue de cinq pouces, & d’un pouce de diamètre ou environ ; & l’ayant couverte d’un morceau de vessie mouillée & ficelée au col du vaisseau, je l’avois plongée dans un grand vase plein d’eau, afin d’être sûr qu’il ne rentrât aucun air dans l’esprit de vin. Au bout de cinq ou six heures, je fus tout surpris de voir que la fiole étoit plus pleine qu’au moment de son immersion, quoiqu’elle le fût alors autant que ses bords pouvoient le permettre ; la vessie qui lui servoit de bouchon, étoit devenue convexe & si tendue, qu’en la piquant avec une épingle, il en sortit un jet de liqueur qui s’éleva à plus d’un pied de hauteur.
Translation:Before finishing this memoir, I think I should report an event that I owe to chance and which at first seemed to me ... strange ....
... I filled [with alcohol] a cylindrical vial, five inches long and about one inch in diameter; and [after] having covered it with piece of damp bladder [which was] tied to the neck of the vial, I immersed it in a large bowl full of water, in order to be sure that no air re-entered the alcohol. At the end of 5 or 6 hours, I was very surprised to see that the vial was fuller than at the moment of its immersion, although it [had been filled] as far as its sides would allow ; the bladder that served as its cap, bulged and had become so stretched that on pricking it with a needle, there came from it a jet of alcohol that rose more than a foot high. - ^ Henri Dutrochet, L'Agent Immédiat du Movement Vital Dévoilé dans sa Nature et dans son Mode d'Action chez les Végétaux et chez les Animaux [The immediate agent of living movement, its nature and mode of action revealed in plants and animals] (Paris, France: Dentu, 1826), pages 115 and 126.
- ^ The intermediate word "osmose" and the word "osmotic" were coined by Scottish chemist Thomas Graham. See: Thomas Graham (1854) "VII. The Bakerian Lecture -- On Osmotic Force," Philosophical Transactions of the Royal Society (London), vol. 144, pages 177-288; see especially pages 177, 178, and 227. See also: Thomas Graham and Henry Watts, Elements of Chemistry: Including the Applications of the Sciences in the Arts, 2nd ed. (London, England: Hippolyte Bailliere, 1858), vol. 2, page 616
- ^ The word "osmosis" first appeared in: Jabez Hogg, The Microscope: Its History, Construction, and Application..., 6th ed. (London, England: George Routledge and Sons, 1867), page 226.
- ^ The etymology of the word "osmosis" is discussed in: Homer W. Smith (May 1960) "I. Theory of Solutions: A knowledge of the laws of solutions," Circulation, vol. 21, pages 808-817; see especially page 810. Available on-line at: http://circ.ahajournals.org/cgi/reprint/21/5/808.pdf .
- ^ Borg, Frank (2003). "What is osmosis? Explanation and understanding of a physical phenomenon". Jyväskylä University, Chydenius Institute, Karleby, Finland: 1–39.
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