Key PointsOsmosis is identified as the flow of water/solvent molecules via a semipermeable membrane from an area of low to high solute concentration, until equilibrium is established.To respond to osmotic circulation, some press must be applied to the solution in order to prevent pure solvent from going via the semipermeable membrane separating the two liquids; this is recognized as the osmotic press.The osmotic pressure is the press compelled to counter, not sustain, osmosis.The osmotic press have the right to be approximated by making use of the complying with formula: Pi = i M R T .

You are watching: The best definition of osmotic pressure is


Termsideal solutionA solution through thermodynamic properties analogous to those of a mixture of appropriate gases.osmosisThe net activity of solvent molecules from an area of high solvent potential to an area of lower solvent potential with a partly permeable membrane.osmotic pressureThe hydrostatic press exerted by a solution across a semipermeable membrane from a pure solvent; the pressure necessary to counteract osmosis.semipermeable membraneOne that will enable particular molecules or ions to pass through it by diffusion.

A solution is characterized as a homogeneous mixture of both a solute and also solvent. Solutions mainly have different properties than the solvent and solute molecules that create them. Some one-of-a-kind properties of options are dependent solely on the amount of dissolved solute molecules, regardmuch less of what that solute is; these properties are recognized as colligative properties.

Osmosis is characterized as the net circulation or activity of solvent molecules via a semipermeable membrane through which solute molecules cannot pass. If a solution consisting of both solute and also solvent molecules is placed on one side of a membrane and also pure solvent is put on the other side, tbelow is a net flow of solvent right into the solution side of the membrane.

Imagine osmosis ensuing in an upideal U-tube. The elevation of the solution will continue to increase due to a net circulation of solvent until the added pressure of the elevation will certainly reason the flow of solution to soptimal. The height difference between the 2 sides have the right to be be converted right into pressure to find the osmotic push exerted on the solution by the pure solvent.

*
U-Tube mirroring osmotic pressureOn the left side of the U-tube is an aqueous solution, and on the right side is pure water. The pure water is trying to dilute the solution by travelling through the semipermeable membrane. At some point the added weight of the added water on the left reasons sufficient push to sheight osmosis.

Osmotic pressure is the pressure that requirements to be used to a solution to proccasion the inward flow of water across a semipermeable membrane. Osmotic push can also be explained as the press crucial to nullify osmosis. One method to soptimal osmosis is to boost the hydrostatic press on the solution side of the membrane; this inevitably squeezes the solvent molecules closer together, increasing their “escaping tendency.” The escaping tendency of the solution have the right to be increased until it ultimately equates to that of the molecules in the pure solvent; at this point, osmosis will cease. The osmotic press is the push required to accomplish osmotic equilibrium.

Osmotic pressureOsmotic pressure is the push compelled to soptimal osmosis.

See more: Why Does Sims 4 Take So Long To Download On Origin Take So Long To Install?

The osmotic press (II) of a perfect solution can be approximated by the Morse equation:

Pi = i M R T

Here, i is the van ‘t Hoff factor, M is the molarity of the solution, R is the gas continuous, and also T is the absolute temperature in Kelvin. We can check out from this equation that the amount of solute existing in the solution will certainly directly affect the osmotic pressure of the device.

Example

What is the osmotic pressure of a 1.35 M solution of NaCl at 25 oC?

First, fill in all of the vital information, and also then solve:

i = 2 (NaCl breaks into 2 particles)

M = 1.35 fracmolesL

R = 0.0821 fracL imes atmK imes mol fracL imes atmK imes mol

T = 25 oC + 273 = 298 K

Pi = 2 imes 1.35 imes 0.0821 imes 298

Pi = 66.1 atm


Boundless vets and curates high-quality, openly licensed content from roughly the Internet. This particular resource provided the following sources: