Question

The solute potential can be determined in a simple manner by
A. Water potential
B. DPD
C. Osmotic pressure
D. Suction pressure

Answer 1

Hint: Solute potential (Ψs), additionally called osmotic potential, is negative in a plant cell and zero in refined water. Commonplace qualities for cell cytoplasm are – 0.5 to – 1.0 MPa. Solutes decrease water potential (bringing about a negative Ψw) by burning-through a portion of the potential energy accessible in the water.

Complete answer:
Solute atoms can break up in water since water particles can tie to them through hydrogen bonds; a hydrophobic atom like oil, which can't tie to water, can't go into arrangement. The energy in the hydrogen connections between solute particles and water is not, at this point, accessible to accomplish work in the framework since it is tied up in the bond. At the end of the day, the measure of accessible potential energy is diminished when solutes are added to a fluid framework. In this manner, Ψs diminishes with expanding solute focus. Since Ψs is one of the four segments of Ψsystem or Ψtotal, an abatement in Ψs will cause a reduction in Ψtotal. The inside water capability of a plant cell is more negative than unadulterated water in light of the cytoplasm's high solute content. Due to this distinction in water potential, water will move from the dirt into a plant's root cells through the cycle of assimilation. This is the reason solute potential is now and then called osmotic potential.
Plant cells can metabolically control Ψs (and by augmentation, Ψtotal) by adding or eliminating solute atoms. Along these lines, plants have power over Ψtotal through their capacity to apply metabolic authority over Ψs.

So, the Correct Option: - (C) Osmotic pressure

Note: Solute potential is the likely evolved because of solute particles. More the solute particles, higher the solute potential. Solute potential is a part of water potential. As far as dissemination pressure shortfall, solute potential is the same as osmotic weight. Osmotic weight is the weight because of which assimilation happens. The osmotic weight is caused because of broken up solute particles in the arrangement.