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関連する概念動画

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...
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.
Modeling with Differential Equations01:25

Modeling with Differential Equations

Population dynamics can be described mathematically by considering the population size P(t) as a function of time. The rate of change of the population is then represented by the derivative of P(t). A simple assumption is that the rate of growth is proportional to the size of the population itself. This leads to an exponential growth model, where the population increases rapidly without bound. While this is a useful first approximation, it does not reflect realistic long-term...
Linear Approximations01:23

Linear Approximations

For a differentiable function of two variables, linear approximation estimates values near a known point by replacing the curved surface with its tangent plane. Consider the function\begin{equation*}f(x,y)=x^2+3y^2\end{equation*}near the point (2, 1). The exact value at this point is f(2, 1) = 22 + 3(1)2 = 4 + 3 = 7.The linear approximation of f(x, y)) near (a, b) is\begin{equation*}L(x,y)=f(a,b)+f_x(a,b)(x-a)+f_y(a,b)(y-b)\end{equation*}First, compute the partial derivatives: fx(x, y) = 2x and...
Theories of Dissolution: The Danckwerts' Model and Interfacial Barrier Model01:09

Theories of Dissolution: The Danckwerts' Model and Interfacial Barrier Model

Various dissolution theories provide insight into the factors that influence the dissolution rate. Danckwerts' Model suggests that turbulence, rather than a stagnant layer, characterizes the dissolution medium at the solid-liquid interface. In this model, the agitated solvent contains macroscopic packets that move to the interface via eddy currents, facilitating the absorption and delivery of the drug to the bulk solution. The regular replenishment of solvent packets maintains the concentration...
Simpson's Rule II01:28

Simpson's Rule II

In warehouse roofing applications, corrugated or curved metal sheets are commonly used to improve structural strength, water drainage, and ventilation efficiency. To accurately estimate material requirements and optimize design parameters, engineers must determine the curved surface area of these sheets. Because the sheet profiles often repeat smoothly along their length, they can be effectively approximated by parabolic curves, enabling the use of numerical integration techniques for area...

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関連する実験動画

Updated: Jul 12, 2026

Laboratory and Field Protocol for Estimating Sheet Erosion Rates from Dendrogeomorphology
07:20

Laboratory and Field Protocol for Estimating Sheet Erosion Rates from Dendrogeomorphology

Published on: January 7, 2019

スカルプの劣化のための拡散方程式モデルから推定された年齢.

S M Colman, K Watson

    Science (New York, N.Y.)
    |July 15, 1983
    PubMed
    まとめ

    この研究では,斜面の拡散方程式をスカープ侵食に適用し,スカープの年齢と形態学から侵食率を直接計算することができます. この方法は,凝固されていない材料の地質学的特徴の年代測定のための新しいツールを提供します.

    科学分野:

    • ジオモルフォロジー ジオモルフォロジー
    • 地球の表面のプロセス 地球の表面のプロセス
    • 定量モデリング

    背景:

    • 斜面の侵食は,基本的な地形的なプロセスです.
    • スカープの形態学は,侵食のダイナミクスへの手がかりを提供します.
    • 斜面の正確な年代測定は,景観の進化を理解するために不可欠です.

    研究 の 目的:

    • 斜面浸食分析のための丘面拡散方程式を適応する.
    • スカップ年齢と侵食率を計算する方法を開発する.
    • 凝固されていない材料のスカープを年代測定するためのツールを提供するために.

    主な方法:

    • 斜面の連続性方程式から拡散方程式を導出する.
    • 派生式をスカープ侵食に適用する.
    • 計算のためにスカルプ形態学の測定を用いる.

    主要な成果:

    • 形状学から率係数とスカープ年齢の積を直接計算する.
    • この方法は,レート係数が知られている場合の未知のスカープ年齢の推定を可能にします.
    • スカップの形と時間との間の定量的なつながりを提供します.

    さらに関連する動画

    Measuring and Modeling Contractile Drying in Human Stratum Corneum
    08:00

    Measuring and Modeling Contractile Drying in Human Stratum Corneum

    Published on: March 1, 2017

    Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
    11:19

    Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

    Published on: October 21, 2016

    関連する実験動画

    Last Updated: Jul 12, 2026

    Laboratory and Field Protocol for Estimating Sheet Erosion Rates from Dendrogeomorphology
    07:20

    Laboratory and Field Protocol for Estimating Sheet Erosion Rates from Dendrogeomorphology

    Published on: January 7, 2019

    Measuring and Modeling Contractile Drying in Human Stratum Corneum
    08:00

    Measuring and Modeling Contractile Drying in Human Stratum Corneum

    Published on: March 1, 2017

    Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
    11:19

    Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

    Published on: October 21, 2016

    結論:

    • 拡散方程式は,スカープ侵食を定量化するための実行可能なアプローチを提供します.
    • この方法は,スカルプの直接的な年齢決定を容易にする.
    • このアプローチは,凝固されていない材料に適用され,ジオクロノロジックツールを強化します.