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Osmotic pressure

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Osmotic pressure is generated in a solution when a semipermeable membrane is present. This membrane allows the solvent to pass through while retaining the solute on one side, creating a pressure imbalance. As a result, there is a reduction in pressure on the solvent side, driving the solvent to move through the membrane toward the side containing the solute.

This process continues until the pressure on the solute side increases enough to balance the initial pressure reduction or until the solute becomes diluted enough that the pressure difference is eliminated, reaching osmotic equilibrium.

>Model

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Mechanisms

Iframe

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Code
Concept

Mechanisms

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Osmotic pressure and U tube

Image

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When a semipermeable membrane is placed at the bottom of a U-shaped tube and water is added, it can be observed that adding dissolved material causes the column with the solute to rise:

This phenomenon is due to the negative pressure generated by osmotic pressure.

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Model

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Parameters

Symbol
Text
Variable
Value
Units
Calculate
MKS Value
MKS Units
p_0
p_0
Atmospheric pressure
Pa
N_A
N_A
Avogadro's number
-
g
g
Gravitational Acceleration
m/s^2
\rho_w
rho_w
Liquid density
kg/m^3
M
M
Mass
kg
M_m
M_m
Molar Mass
kg/mol
N_s
N_s
Number of ions
-
n
n
Número de Moles
mol
\Psi
Psi
Osmotic pressure
Pa
R
R
Universal gas constant
J/mol K
\Delta p
Dp
Variación de la Presión
Pa

Variables

Symbol
Text
Variable
Value
Units
Calculate
MKS Value
MKS Units
T
T
Absolute temperature
K
\Delta h
Dh
Height of liquid column
m
h_1
h_1
Height or depth 1
m
h_2
h_2
Height or depth 2
m
p_1
p_1
Pressure in column 1
Pa
p_2
p_2
Pressure in column 2
Pa
V
V
Volume
m^3

Calculations


First, select the equation: to , then, select the variable: to

Calculations

Symbol
Equation
Solved
Translated

Calculations

Symbol
Equation
Solved
Translated

Variable Given Calculate Target : Equation To be used




Equations

#
Equation

\Delta h = h_2 - h_1

Dh = h_2 - h_1


\Delta p = p_2 - p_1

Dp = p_2 - p_1


\Delta p = \rho_w g \Delta h

Dp = rho_w * g * Dh


n = \displaystyle\frac{ M }{ M_m }

n = M / M_m


n \equiv\displaystyle\frac{ N_s }{ N_A }

n = N / N_A


\Psi =\displaystyle\frac{ N_s }{ V } R T

Psi = N_s * R * T / V


p_1 = p_2 - \Psi

p_1 = p_2 - Psi


p_1 = p_0 + \rho_w g h_1

p_t = p_0 + rho_w * g * h


p_2 = p_0 + \rho_w g h_2

p_t = p_0 + rho_w * g * h

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Behavior of the Solute as Gas Ideal

Equation

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The osmotic pressure (\Psi) behaves like the pressure of an ideal gas of the number of ions (N_s) in the volume (V) at the absolute temperature (T), using the universal gas constant (R) as described by:

\Psi =\displaystyle\frac{ N_s }{ V } R T

T
Absolute temperature
K
5177
N_s
Number of ions
-
9850
\Psi
Osmotic pressure
Pa
6608
R
Universal gas constant
8.4135
J/mol K
4957
V
Volume
m^3
5226

Como la energía molar libre de Gibbs es

dg = - s dT + v dp + \mu dN



se tiene que para el equilibrio entre un sistema con y sin material disuelto (dg=0) e igual temperatura (dT=0) que

\displaystyle\frac{V}{N_A}dp=\displaystyle\frac{V}{N_A}(p - \Phi)=\mu dN=\mu (N-N_s)



Como sin material disuelto se debe asumir que el vapor satisface la ecuación de los gases se tiene que

\mu\sim \displaystyle\frac{R}{N_A} T



con lo que se obtiene que

\Psi =\displaystyle\frac{ N_s }{ V } R T

ID:(12820, 0)



Osmotic pressure and water column

Equation

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If two columns of water are separated at their base by a semipermeable membrane that allows water to pass through but blocks the solute present in one of them, the columns will exhibit different heights. This is because the presence of a solute reduces the osmotic pressure, leading to an adjustment in the height of the column to balance the pressure difference.

If the pressure in the first column is the pressure in column 1 (p_1), the pressure in the second column (without solute) is the pressure in column 2 (p_2), and the osmotic pressure is the osmotic pressure (\Psi), we can express the relationship as follows:

p_1 = p_2 - \Psi

\Psi
Osmotic pressure
Pa
6608
p_1
Pressure in column 1
Pa
6261
p_2
Pressure in column 2
Pa
6262

ID:(12827, 0)



Pressure difference between columns

Equation

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The height difference, denoted by the height difference (\Delta h), implies that the pressure in both columns is distinct. In particular, the pressure difference (\Delta p) is a function of the liquid density (\rho_w), the gravitational Acceleration (g), and the height difference (\Delta h), as follows:

\Delta p = \rho_w g \Delta h

g
Gravitational Acceleration
9.8
m/s^2
5310
\Delta h
Height of liquid column
m
5819
\rho_w
Liquid density
kg/m^3
5407
\Delta p
Variación de la Presión
Pa
6673

If there is the pressure difference (\Delta p) between two points, as determined by the equation:

\Delta p = p_2 - p_1



we can utilize the water column pressure (p), which is defined as:

p_t = p_0 + \rho_w g h



This results in:

\Delta p=p_2-p_1=p_0+\rho_wh_2g-p_0-\rho_wh_1g=\rho_w(h_2-h_1)g



As the height difference (\Delta h) is:

\Delta h = h_2 - h_1



the pressure difference (\Delta p) can be expressed as:

\Delta p = \rho_w g \Delta h

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Height difference

Equation

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When two liquid columns are connected with the height of liquid column 1 (h_1) and the height of liquid column 2 (h_2), a the height difference (\Delta h) is formed, which is calculated as follows:

\Delta h = h_2 - h_1

\Delta h
Height of liquid column
m
5819
h_1
Height or depth 1
m
6259
h_2
Height or depth 2
m
6260



the height difference (\Delta h) will generate the pressure difference that will cause the liquid to flow from the higher column to the lower one.

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Pressure difference

Equation

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When two liquid columns are connected with the pressure in column 1 (p_1) and the pressure in column 2 (p_2), a the pressure difference (\Delta p) is formed, which is calculated according to the following formula:

\Delta p = p_2 - p_1

p_1
Pressure in column 1
Pa
6261
p_2
Pressure in column 2
Pa
6262
\Delta p
Variación de la Presión
Pa
6673



the pressure difference (\Delta p) represents the pressure difference that will cause the liquid to flow from the taller column to the shorter one.

ID:(4252, 0)



Number of moles

Equation

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The number of moles (n) corresponds to the number of particles (N) divided by the avogadro's number (N_A):

n \equiv\displaystyle\frac{ N_s }{ N_A }

n \equiv\displaystyle\frac{ N }{ N_A }

N_A
Avogadro's number
6.02e+23
-
9860
N
N_s
Number of ions
-
9850
n
Número de Moles
mol
6679

ID:(3748, 0)



Number of moles with molar mass

Equation

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The number of moles (n) is determined by dividing the mass (M) of a substance by its the molar Mass (M_m), which corresponds to the weight of one mole of the substance.

Therefore, the following relationship can be established:

n = \displaystyle\frac{ M }{ M_m }

M
Mass
kg
5183
M_m
Molar Mass
kg/mol
6212
n
Número de Moles
mol
6679

The number of moles (n) corresponds to the number of particles (N) divided by the avogadro's number (N_A):

n \equiv\displaystyle\frac{ N_s }{ N_A }



If we multiply both the numerator and the denominator by the particle mass (m), we obtain:

n=\displaystyle\frac{N}{N_A}=\displaystyle\frac{Nm}{N_Am}=\displaystyle\frac{M}{M_m}



So it is:

n = \displaystyle\frac{ M }{ M_m }

The molar mass is expressed in grams per mole (g/mol).

ID:(4854, 0)



Atmospheric pressure column pressure (1)

Equation

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The water column pressure (p) is with the liquid density (\rho_w), the column height (h), the gravitational Acceleration (g) and the atmospheric pressure (p_0) equal to:

p_1 = p_0 + \rho_w g h_1

p_t = p_0 + \rho_w g h

p_0
Atmospheric pressure
Pa
5817
h
h_1
Height or depth 1
m
6259
g
Gravitational Acceleration
9.8
m/s^2
5310
\rho_w
Liquid density
kg/m^3
5407
p_t
p_1
Pressure in column 1
Pa
6261

ID:(4250, 1)



Atmospheric pressure column pressure (2)

Equation

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The water column pressure (p) is with the liquid density (\rho_w), the column height (h), the gravitational Acceleration (g) and the atmospheric pressure (p_0) equal to:

p_2 = p_0 + \rho_w g h_2

p_t = p_0 + \rho_w g h

p_0
Atmospheric pressure
Pa
5817
h
h_2
Height or depth 2
m
6260
g
Gravitational Acceleration
9.8
m/s^2
5310
\rho_w
Liquid density
kg/m^3
5407
p_t
p_2
Pressure in column 2
Pa
6262

ID:(4250, 2)