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The potential difference between the fixed and mobile part of double layer in soil colloids is known as
Question

The potential difference between the fixed and mobile part of double layer in soil colloids is known as

A.

Total water potential

B.

Theta potential

C.

Gravitational potential

D.

Zeta potential

Correct option is D

The correct answer is (D) Zeta potential

Explanation:
• Soil colloids (clay and humus) possess a negative surface charge. In a soil solution, they attract a layer of counter-ions (cations).
• This creates an "Electric Double Layer" consisting of a Stern layer (fixed ions tightly bound to the surface) and a Diffuse layer (mobile ions in the solution).
• The Zeta potential is the electrokinetic potential at the slipping plane (the boundary where the mobile part of the solution starts moving relative to the particle surface).
• It is a measure of the magnitude of the electrostatic or charge repulsion/attraction between particles and is one of the fundamental parameters known to affect stability (flocculation vs. dispersion).

Information Booster:
• A high zeta potential (positive or negative) indicates that the particles will repel each other, leading to a dispersed (stable) suspension.
• A low zeta potential (near zero) means the repulsive forces are weak, and particles will clump together (flocculate).
• The point at which the zeta potential is zero is called the Isoelectric Point.

Additional Knowledge:
• Total water potential (Option A): The sum of various forces (matric, osmotic, gravitational) acting on soil water.
• Gravitational potential (Option C): Potential energy of water due to its elevation in the Earth's gravitational field.
• Theta potential (Option B): Likely a distractor, though "Theta" is often used to represent volumetric water content in soil physics.

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