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Solute Potential (Ψs) is the pressure which needs to be applied to a solution to prevent the inward flow of water across a semipermeable membrane. It represents the effect of dissolved solutes on the water potential of a system.
The calculator uses the formula:
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Explanation: The solute potential is calculated by subtracting the pressure potential from the total water potential of the system.
Details: Calculating solute potential is crucial in plant physiology and cell biology for understanding water movement across membranes, osmoregulation, and determining the direction of water flow in biological systems.
Tips: Enter water potential and pressure potential values in Pascal units. Both values must be valid numerical inputs for accurate calculation.
Q1: What is the relationship between water potential and solute potential?
A: Water potential (Ψ) is the sum of solute potential (Ψs) and pressure potential (Ψp): Ψ = Ψs + Ψp. Solute potential is always negative or zero.
Q2: Why is solute potential important in plant cells?
A: Solute potential determines the osmotic pressure and influences water uptake, turgor pressure, and overall cell hydration in plant cells.
Q3: What factors affect solute potential?
A: Solute potential is primarily affected by the concentration of dissolved solutes - higher solute concentration results in more negative solute potential.
Q4: How does temperature affect solute potential?
A: Temperature can affect solute potential indirectly by influencing solute solubility and diffusion rates, but the fundamental relationship remains based on solute concentration.
Q5: Can solute potential be positive?
A: No, solute potential is always zero or negative because solutes reduce the free energy of water molecules in the solution.