13. Introduction to Flux Measurement - Environmental Quality Monitoring & Analysis, - Vol 5
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13. Introduction to Flux Measurement

13. Introduction to Flux Measurement

The chapter discusses the principles of mass and energy transfer in the atmosphere, particularly focusing on the influence of moisture content and temperature gradients on flux measurements. It covers methods for calculating flux using gradient techniques and introduces important concepts such as turbulence and convective mass transfer. Additionally, it highlights the challenges and methodologies employed in measuring atmospheric parameters over various surfaces.

18 sections

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Sections

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  1. 1
    Introduction To Flux Measurement

    This section discusses the principles behind flux measurement, specifically...

  2. 1.1
    Experimental Data On Dibenzofuran

    This section discusses the experimental behavior of dibenzofuran in response...

  3. 1.2
    Measurement Techniques

    This section explores various soil moisture measurement techniques and their...

  4. 2
    Gradient Technique And Micrometeorological Technique

    This section discusses the gradient technique and micrometeorological...

  5. 2.1
    Aerodynamic Technique

    The aerodynamic technique, also known as the gradient technique, measures...

  6. 2.2
    Convective Mass Transfer

    This section discusses the principles of convective mass transfer,...

  7. 3
    Thornwaite-Holzman Equation

    The Thornwaite-Holzman Equation explains the relationship between...

  8. 3.1
    Velocity Gradient And Friction Velocity

    This section discusses the impact of moisture changes on soil flux,...

  9. 3.2
    Calculating Mass Flux

    This section explores the concept of mass flux, emphasizing its dependence...

  10. 4
    Modified Thornwaite-Holzman Equation

    The Modified Thornwaite-Holzman Equation addresses the complexities of...

  11. 4.1
    Monin-Obukhov Length Scale

    The Monin-Obukhov Length Scale is a critical concept in understanding how...

  12. 4.2
    Incorporating Thermal Forces

    This section discusses the impact of thermal forces on soil moisture and...

  13. 5
    Overall Flux Expression

    This section covers the relationships and dynamics of flux in relation to...

  14. 5.1
    Three Gradients Contribution

    This section discusses the influence of moisture content and flux in soil,...

  15. 5.2
    Limitations Of Measurements

    The limitations of measurement techniques in assessing soil moisture and...

  16. 6
    Field Experiment Setup

    This section covers the principles and methodologies involved in setting up...

  17. 6.1
    Mast Measurement For Gradient Technique

    This section discusses the gradient technique for flux measurement in soil...

  18. 6.2
    Challenges With Particle Measurements

    This section discusses the complexities of measuring particle flux in soil...

What we have learnt

  • Moisture content and temperature significantly affect flux in environmental systems.
  • Gradient techniques are essential for accurately measuring atmospheric flux when traditional enclosure methods are not feasible.
  • Turbulence and convective mass transfer dynamics play critical roles in the behavior of substances in the atmosphere.

Key Concepts

-- Abstraction
A method of simplifying complex systems in order to study them or derive formulas.
-- Flux Measurement
The process of quantifying the amount of a substance that passes through a surface in a given time period.
-- Gradient Technique
A method used to estimate flux by measuring the concentration gradient of a substance in the atmosphere.
-- Turbulence
The irregular or chaotic movement of fluid particles that impacts the transfer characteristics of gases and vapors.
-- Convective Mass Transfer
The transfer of mass caused by the movement of the fluid itself, often influenced by factors like temperature gradients and turbulence.
-- MoninObukhov Length Scale
A length scale that quantifies the influence of buoyancy on turbulence in the atmosphere.

Additional Learning Materials

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