Solute Potential Equation:
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Solute potential (Ψs) is the component of water potential that results from the presence of solute particles. It is always negative or zero and represents the reduction in water potential due to dissolved solutes.
The calculator uses the solute potential equation:
Where:
Explanation: The equation shows that solute potential becomes more negative with increasing solute concentration and temperature.
Details: Solute potential is crucial in plant physiology for understanding water movement, osmosis, and turgor pressure. It helps explain how plants absorb water from soil and maintain cell structure.
Tips: Enter the ionization constant (1 for non-electrolytes, >1 for salts), concentration in mol/L, and temperature in Kelvin. All values must be positive.
Q1: What is a typical solute potential value for plant cells?
A: Most plant cells have solute potentials between -0.5 to -2.5 MPa, depending on the cell type and environmental conditions.
Q2: How does solute potential differ from water potential?
A: Water potential (Ψ) is the sum of solute potential (Ψs) and pressure potential (Ψp). Solute potential is only one component.
Q3: What is the ionization constant (i) for common solutes?
A: For sucrose (non-electrolyte) i=1, for NaCl (fully dissociated) i≈2, for CaCl2 i≈3.
Q4: Why is solute potential always negative or zero?
A: Solutes reduce the free energy of water, making the potential lower than pure water (which has Ψs=0).
Q5: How does temperature affect solute potential?
A: Higher temperatures make the solute potential more negative because thermal energy increases molecular activity.