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Uniform Depth Channel Flow01:27

Uniform Depth Channel Flow

Uniform depth channel flow keeps fluid depth consistent along channels such as irrigation canals. In natural channels, such as rivers, approximate uniform flow is often assumed. This condition occurs when the channel’s bottom slope matches the energy slope, balancing potential energy lost from gravity with head loss due to shear stress. This balance prevents depth changes along the channel length, resulting in a steady, uniform flow.Uniform flow in open channels with a constant cross-section...
Debye–Huckel–Onsager Conductance Equation01:28

Debye–Huckel–Onsager Conductance Equation

The Debye-Hückel-Onsager equation is a cornerstone of physical chemistry, providing a method to determine the molar conductance (Λm) and molar conductance at infinite dilution (Λ°m) for uni-univalent electrolytes.Uni-univalent electrolytes are electrolytes that dissociate in solution to produce one cation with a +1 charge and one anion with a –1 charge per formula unit.This equation addresses two crucial phenomena: the asymmetry effect and the electrophoretic effect. According to this equation,...
Uniform Depth Channel Flow: Problem Solving01:18

Uniform Depth Channel Flow: Problem Solving

To calculate the flow rate for a trapezoidal channel, first, identify the bottom width, side slope, and flow depth of the channel. The cross-sectional area (A) corresponding to the depth of flow (y), channel bottom width (B), and side slope (θ) is determined by:Next, calculate the wetted perimeter, which includes the bottom width and the sloped side lengths in contact with the water. Using the values of the cross-sectional area and the wetted perimeter, determine the hydraulic radius by...
Design Example: Creating a Hydraulic Model of a Dam Spillway01:21

Design Example: Creating a Hydraulic Model of a Dam Spillway

Scaled hydraulic models of dam spillways provide a practical way to replicate and study the intricate flow dynamics of these structures. Often built to a 1:15 ratio, these models allow for observing critical water behavior, such as velocity distribution, flow patterns, and energy dissipation.
Boundary Conditions for Current Density01:25

Boundary Conditions for Current Density

Current density becomes discontinuous across an interface of materials with different electrical conductivities. The normal component of the current density is continuous across the boundary.
Major Losses in Pipes01:28

Major Losses in Pipes

When a fluid flows through a pipe, it experiences energy losses due to frictional resistance along the pipe walls, known as major losses. These energy losses result in a pressure drop, which varies based on the flow conditions — whether laminar or turbulent — and the specific physical properties of the fluid and pipe.
Fluid flow can be classified as laminar or turbulent, primarily based on the Reynolds number. This dimensionless number reflects the relative influence of inertial to viscous...

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Related Experiment Video

Updated: May 9, 2026

Wastewater Irrigation Impacts on Soil Hydraulic Conductivity: Coupled Field Sampling and Laboratory Determination of Saturated Hydraulic Conductivity
08:09

Wastewater Irrigation Impacts on Soil Hydraulic Conductivity: Coupled Field Sampling and Laboratory Determination of Saturated Hydraulic Conductivity

Published on: August 19, 2018

Physically based closed-form expression for the bimodal unsaturated hydraulic conductivity function.

Shiyu Liu1, Noriyuki Yasufuku, Qiang Liu

  • 1Geotechnical Engineering Research Group, Faculty of Engineering, Kyushu University, Fukuoka, 819-0395, Japan. liushiyu518@gmail.com

Water Science and Technology : a Journal of the International Association on Water Pollution Research
|July 19, 2013
PubMed
Summary

Accurate soil hydraulic properties are crucial for simulating water flow and contaminant transport in complex soils. This study proposes a new physically based model for bimodal unsaturated hydraulic conductivity, showing good agreement with experimental data.

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Last Updated: May 9, 2026

Wastewater Irrigation Impacts on Soil Hydraulic Conductivity: Coupled Field Sampling and Laboratory Determination of Saturated Hydraulic Conductivity
08:09

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Measurements of Soil Water Potential and Conductivity based on a Simple Evaporation Experiment using a Hydraulic Property Analyzer
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Area of Science:

  • Environmental science
  • Soil science
  • Hydrogeology

Background:

  • Accurate parameterization of soil hydraulic properties is essential for modeling water flow and contaminant transport in the vadose zone.
  • Complex soil structures pose significant challenges for existing models.

Purpose of the Study:

  • To propose a physically based, closed-form expression for bimodal unsaturated hydraulic conductivity functions.
  • To develop a model applicable to soils with bimodal pore-size distributions.

Main Methods:

  • Combined Liu's bimodal soil-water characteristic curve (SWCC) representation with Mualem's conductivity model.
  • Defined parameters with physical significance related to material properties.
  • Validated the proposed functions using experimental data for bimodal SWCCs and hydraulic conductivity.

Main Results:

  • The proposed equations accurately represent bimodal soil hydraulic properties.
  • The model demonstrated good agreement with experimental data.
  • Physically significant parameters were identified.

Conclusions:

  • The developed functions provide an effective tool for characterizing hydraulic properties in complex soil structures.
  • Potential applications include improved vadose zone simulations and contaminant transport modeling.
  • The model aids in identifying hydraulic porosities in heterogeneous media.