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CivilWater Resources Management
PrevNext

Movement and filtering of fluid from porous material is called as __________

A

Percolation

B

Infiltration

C

Transpiration

D

Precipitation

Correct Answer

тЪЩя╕П TE тАв Technical Concept & PrincipleCivilWater Resources Management
Option A

Percolation

Quick Summary:

Percolation is the downward movement of water through the unsaturated zone of the soil profile, often involving the filtering of impurities as water moves through porous material. It is a fundamental process in the hydrological cycle, facilitating groundwater recharge.

тЪЩя╕ПTETechnical SolutionConcept & Principle
ЁЯТб Explanation

Percolation is the downward movement of water through the unsaturated zone of the soil profile, often involving the filtering of impurities as water moves through porous material. It is a fundamental process in the hydrological cycle, facilitating groundwater recharge.

ЁЯФв Key Formulas

v=тИТKdhdlv = -K \frac{dh}{dl}v=тИТKdldhтАЛ тАФ Darcy's Law, where vvv is discharge velocity, KKK is hydraulic conductivity, and dhdl\frac{dh}{dl}dldhтАЛ is the hydraulic gradient.

тЪЩя╕П Working Principle

The process is driven primarily by gravity and the hydraulic gradient within the soil medium. As water moves through interconnected soil pores, mechanical straining, adsorption, and biological activity act to filter suspended solids and contaminants from the fluid. The rate of flow is governed by Darcy's Law, which relates the flow velocity to the hydraulic conductivity and the hydraulic gradient.

ЁЯУМ Key Points
  • тЦ╕

    Percolation occurs primarily in the unsaturated zone, also known as the vadose zone.

  • тЦ╕

    It differs from infiltration, which is the entry of water into the soil surface.

  • тЦ╕

    The filtering action of soil makes percolation a natural water treatment process.

  • тЦ╕

    The rate of percolation is highly dependent on soil porosity, permeability, and moisture content.

тЬЕ Advantages
  • тЦ╕

    Natural purification of water as it travels through soil layers.

  • тЦ╕

    Essential for replenishment of aquifers.

тЭМ Disadvantages / Limitations
  • тЦ╕

    Can transport surface pollutants into groundwater if soil is contaminated.

  • тЦ╕

    Slow process depending on soil texture.

ЁЯЫая╕П Applications / Uses
  • тЦ╕

    Groundwater recharge estimation

  • тЦ╕

    Design of septic tank leach fields

  • тЦ╕

    Agricultural irrigation management

ЁЯФД Comparison Table
FeaturePercolationInfiltration

Definition

Movement through porous media

Entry through soil surface

ЁЯУД Additional Information
  • тЦ╕

    Infiltration represents the initial transition of water from the surface into the soil, while percolation is the subsequent movement within the soil mass.

  • тЦ╕

    Transpiration relates to water vapor loss from plants.

  • тЦ╕

    Precipitation refers to the falling of condensed water vapor as rain, snow, or hail.

ЁЯУК Diagram / Illustration
Percolation MechanismPorous SoilMatrixGravity FlowWater infiltration and downward filtration
тЬЕ

A is correct тАФ Percolation is the process of fluid moving through and being filtered by a porous medium.

Core Concepts Used
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Hydrological Cycle Soil Porosity Darcy's Law
ЁЯТб EXAM TIP

Always distinguish between infiltration (surface boundary) and percolation (subsurface movement) to avoid common mistakes in hydrology questions.

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