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Wave equation analysis is a numerical method of analysis for the behavior of driven foundation piles. It predicts the pile capacity versus blow count relationship
Wave_equation_analysis
Differential equation for the description of waves or standing wave
The wave equation is a second-order linear partial differential equation for the description of waves or standing wave fields such as mechanical waves (e
Wave_equation
Sudden movement of the Earth's crust
the P- and S wave arrival times, multiplied by 8. Slight deviations are caused by inhomogeneities of subsurface structure. By such analysis of seismograms
Earthquake
Wave shaped like the sine function
Least-squares spectral analysis Oscilloscope Phasor Pure tone Simple harmonic motion Sinusoidal model Wave (physics) Wave equation ∿ the sine wave symbol (U+223F)
Sine_wave
Eigenvalue problem for the Laplace operator
separation of variables to reduce the complexity of the analysis. For example, consider the wave equation ( ∇ 2 − 1 c 2 ∂ 2 ∂ t 2 ) u ( r , t ) = 0. {\displaystyle
Helmholtz_equation
Excavation or structure to provide access to groundwater
{\displaystyle F=A{\frac {dz}{dt}}} Combining the above three equations yields a simple differential equation in z: R A d z d t = ρ g ( z T − z ) {\displaystyle
Well
Fine grained natural soil
B.; Williams, Frank; Deocampo, Daniel (1 December 2012). "Portable XRF analysis of zoomorphic figurines, "tokens," and sling bullets from Chogha Gavaneh
Clay
Granular material composed of finely divided rock and mineral particles
years, rocks are eroded near the shoreline from the constant motion of waves and the sediments build up. Weathering and river deposition also accelerate
Sand
Classification of soil or sediment
Exploration geophysics Crosshole sonic logging Pile integrity test Wave equation analysis Laboratory testing Soil classification Atterberg limits California
Silt
Set of partial differential equations on fluid flow
Saint-Venant equations (aka Dynamic wave equation), we get the also classical Diffusive wave equation and Kinematic wave equation. For the diffusive wave it is
Shallow_water_equations
Mathematical description of quantum state
Schrödinger equation determines how wave functions evolve over time, and a wave function behaves qualitatively like other waves, such as water waves or waves on
Wave_function
Narrow shaft bored in the ground
can be effectively "inverted" (a mathematical formula to solve a matrix equation) to help estimate historic surface temperatures. Clusters of small-diameter
Borehole
Dynamic disturbance in a medium or field
Griffiths, G.; Schiesser, W.E. (2010). Traveling Wave Analysis of Partial Differential Equations: Numerical and Analytical Methods with Matlab and Maple
Wave
Relativistic wave equation in quantum mechanics
In particle physics, the Klein–Gordon equation is a relativistic wave equation for spinless particles. It was discovered 1926 as the relativistic generalization
Klein–Gordon_equation
Type of differential equation
functional analysis are often used in this field of study. Some common PDEs Acoustic wave equation Burgers' equation Continuity equation Heat equation Helmholtz
Partial_differential_equation
Ratio of void volume and total volume of a porous material
depth is the decreasing exponential function given by the Athy (1930) equation: ϕ ( z ) = ϕ 0 e − k z {\displaystyle \phi (z)=\phi _{0}e^{-kz}\,} where
Porosity
Accumulation of partially decayed vegetation
to Sphagnum recolonization. In the summer of 2010, an unusually high heat wave of up to 40 °C (104 °F) ignited large deposits of peat in Central Russia
Peat
Change in viscosity of a gel or fluid caused by stress
two-phase mixture to model to allow the mixture to continue without added equations entering when thixotropy is working through its process on the different
Thixotropy
Natural hazard involving ground movement
(e.g. after a wildfire); erosion of the top of a slope by rivers or sea waves; physical and chemical weathering (e.g. by repeated freezing and thawing
Landslide
Branch of mathematics
include complex analysis, functional analysis, measure theory, harmonic analysis, and the theory of ordinary and partial differential equations. Mathematical
Mathematical_analysis
Approximation valid for weakly non-linear and fairly long waves
Russell of the wave of translation (also known as solitary wave or soliton). The 1872 paper by Joseph Valentin Boussinesq introduces the equations now known
Boussinesq approximation (water waves)
Boussinesq_approximation_(water_waves)
Measure of the ability of a porous material to allow fluids to pass through it
more generally, by application of various solutions to the diffusion equation for unsteady flow conditions. Permeability needs to be measured, either
Permeability_(porous_media)
Excavated channel in ground
Exploration geophysics Crosshole sonic logging Pile integrity test Wave equation analysis Laboratory testing Soil classification Atterberg limits California
Trench
Device used to measure density of liquids
freezing point. A hydrometer analysis is the process by which fine-grained soils, silts and clays, are graded. Hydrometer analysis is performed if the grain
Hydrometer
Nonlinear and exact periodic wave solution of the Korteweg–de Vries equation
In fluid dynamics, a cnoidal wave is a nonlinear and exact periodic wave solution of the Korteweg–de Vries equation. These solutions are in terms of the
Cnoidal_wave
Equation for force on an object in sea waves
Schaaf—of the 1950 paper in which the equation was introduced. The Morison equation is used to estimate the wave loads in the design of oil platforms and
Morison_equation
Procedure to assess particle size distribution
A sieve analysis (or gradation test) is a practice or procedure used in geology, civil engineering, and chemical engineering to assess the particle size
Sieve_analysis
Partial differential equation in mathematics
"Fisher-KPP Equation" (PDF). Fisher 2. Griffiths, Graham W.; Schiesser, William E. (2011). "Fisher–Kolmogorov Equation". Traveling Wave Analysis of Partial
KPP–Fisher_equation
Soil material that is ordinarily a solid behaving like a thick liquid
Retrieved 26 May 2026. Sassa, Shinji; Sekiguchi, Haruko (1 March 2001). "Analysis of wave-induced liquefaction of sand beds". Géotechnique. 51 (2): 115–126.
Soil_liquefaction
Ability of water to flow through a porous material
relationship into the above, and taking the limit as Δt → 0, the differential equation d h d t = − K L h {\displaystyle {\frac {dh}{dt}}=-{\frac {K}{L}}h} has
Hydraulic_conductivity
Movement of rock or soil down slopes
Exploration geophysics Crosshole sonic logging Pile integrity test Wave equation analysis Laboratory testing Soil classification Atterberg limits California
Mass_wasting
Nonlinear form of the Schrödinger equation
the equation appears in the studies of small-amplitude gravity waves on the surface of deep inviscid (zero-viscosity) water; the Langmuir waves in hot
Nonlinear Schrödinger equation
Nonlinear_Schrödinger_equation
Type of mathematical model
solutions of reaction–diffusion equations display a wide range of behaviours, including the formation of travelling waves and wave-like phenomena as well as
Reaction–diffusion_system
Mix of crumbled stones
Exploration geophysics Crosshole sonic logging Pile integrity test Wave equation analysis Laboratory testing Soil classification Atterberg limits California
Gravel
Fundamental principle of physics
affect the wave) and initial conditions of the system. In many cases (for example, in the classic wave equation), the equation describing the wave is linear
Superposition_principle
Partial differential equation describing the evolution of temperature in a region
specifically thermodynamics), the heat equation is a parabolic partial differential equation. The theory of the heat equation was first developed by Joseph Fourier
Heat_equation
Equation in physics
wave equation, or nonhomogeneous electromagnetic wave equation, is one of a set of wave equations describing the propagation of electromagnetic waves
Inhomogeneous electromagnetic wave equation
Inhomogeneous_electromagnetic_wave_equation
Quantity of water contained in a material
1016/c2011-0-06101-x. ISBN 978-0-12-398530-9. van Genuchten, M.Th. (1980). "A closed-form equation for predicting the hydraulic conductivity of unsaturated soils". Soil Science
Water_content
Equations of light transmission and reflection
Fresnel equations give the ratio of the reflected wave's electric field to the incident wave's electric field, and the ratio of the transmitted wave's electric
Fresnel_equations
Works that re-shape the earth's surface
Exploration geophysics Crosshole sonic logging Pile integrity test Wave equation analysis Laboratory testing Soil classification Atterberg limits California
Earthworks_(engineering)
Short "burst" or "envelope" of restricted wave action that travels as a unit
component wave function, and hence the wave packet, are solutions of a wave equation. Depending on the wave equation, the wave packet's profile may remain constant
Wave_packet
Type of partial differential equations
of substantial contemporary interest. The model hyperbolic equation is the wave equation. In one spatial dimension, this is ∂ 2 u ∂ t 2 = c 2 ∂ 2 u ∂
Hyperbolic partial differential equation
Hyperbolic_partial_differential_equation
Technique to solve differential equations
homotopy analysis method (HAM) is a semi-analytical technique to solve nonlinear ordinary/partial differential equations. The homotopy analysis method employs
Homotopy_analysis_method
Semi-analytic method of computational electromagnetism
Rigorous coupled-wave analysis (RCWA), also known as Fourier modal method (FMM), is a semi-analytical method in computational electromagnetics that is
Rigorous coupled-wave analysis
Rigorous_coupled-wave_analysis
Mathematical model of how solid objects deform
used extensively in structural analysis and engineering design, often with the aid of finite element analysis. Equations governing a linear elastic boundary
Linear_elasticity
the three-wave equations, sometimes called the three-wave resonant interaction equations or triad resonances, describe small-amplitude waves in a variety
Three-wave_equation
Unexpectedly large transient ocean surface wave
rogue waves. Among other causes, studies of nonlinear waves such as the Peregrine soliton, and waves modeled by the nonlinear Schrödinger equation (NLS)
Rogue_wave
Type of functional equation (mathematics)
one-dimensional wave equation, and within ten years Euler discovered the three-dimensional wave equation. The Euler–Lagrange equation was developed in
Differential_equation
Equations describing classical electromagnetism
Maxwell's equations are a set of coupled partial differential equations that describe how electric and magnetic fields are generated by electric charges
Maxwell's_equations
The Benjamin–Bona–Mahony equation (BBM equation, also regularized long-wave equation; RLWE) is the partial differential equation u t + u x + u u x − u x
Benjamin–Bona–Mahony_equation
Measure of arterial stiffness
Pulse wave velocity (PWV) is the velocity at which the blood pressure pulse propagates through the circulatory system, usually an artery or a combined
Pulse_wave_velocity
Class of partial differential equations
In mathematics, an elliptic partial differential equation is a type of partial differential equation (PDE). In mathematical modeling, elliptic PDEs are
Elliptic partial differential equation
Elliptic_partial_differential_equation
Physical model of propagating energy
differentiable to conform to the wave equation). As with any time function, this can be decomposed by means of Fourier analysis into its frequency spectrum
Electromagnetic_radiation
Technique in quantum mechanics for solving scattering problems
Partial-wave analysis, in the context of quantum mechanics, refers to a technique for solving scattering problems by decomposing each wave into its constituent
Partial-wave_analysis
roughness. This definition has been applied in several research to alter flow equations or measure the fluid-fluid interfacial area. The fundamental idea of fractal
Pore_structure
Civil engineering technique
undertaken based on bending moment and shear envelope obtained from the stress analysis. In the design of such underground walls, width of the unit is considered
Slurry_wall
Analysis of the dimensions of different physical quantities
dimensional analysis, serving as a plausibility check on derived equations and computations. It also serves as a guide and constraint in deriving equations that
Dimensional_analysis
Branch of physics and acoustics
sound waves of sufficiently large amplitudes. Large amplitudes require using full systems of governing equations of fluid dynamics (for sound waves in liquids
Nonlinear_acoustics
Techniques in mathematical analysis
Microlocal analysis is a branch of mathematical analysis that studies functions, generalized functions and partial differential equations by localizing
Microlocal_analysis
Interpretation of quantum mechanics
particles is defined by a guiding equation. The evolution of the wave function over time is given by the Schrödinger equation. The interpretation is named
De_Broglie–Bohm_theory
Applied branch of geophysics and economic geology
Spectral-Analysis-of-Surface-Waves (SASW) method is another non-invasive technique, which is widely used in practice to detect the shear wave velocity
Exploration_geophysics
Manner in which fluids behave when flowing through a porous medium
q)}{dx}}={\frac {d(\rho \phi )}{dt}}~~~~(i)} In three dimensions, the equation can be written as d ( ρ q ) d x + d ( ρ q ) d y + d ( ρ q ) d z = − d (
Fluid flow through porous media
Fluid_flow_through_porous_media
Mathematical model of waves on a shallow water surface
the Korteweg–De Vries (KdV) equation is a partial differential equation (PDE) which serves as a mathematical model of waves on shallow water surfaces.
Korteweg–De_Vries_equation
Method in the dynamics of blood flow
the separation obtained using Fourier analysis methods. Wave intensity analysis is based on the 1-D equations for the conservation of mass and momentum
Wave_intensity_analysis
wave; Electrokinetic effects analogous to streaming potentials are created by the seismic wave; Piezoelectric effects are created by the seismic wave;
Seismoelectrical_method
Formulation of classical mechanics
mechanics. The Hamilton–Jacobi equation is a formulation of mechanics in which the motion of a particle can be represented as a wave. In this sense, it fulfilled
Hamilton–Jacobi_equation
Special type of functions in mathematics
shape). Related are the oblate spheroidal wave functions (pancake shaped ellipsoid). Solve the Helmholtz equation, ∇ 2 Φ + k 2 Φ = 0 {\displaystyle \nabla
Prolate spheroidal wave function
Prolate_spheroidal_wave_function
E. (2012). "Introduction to Traveling Wave Analysis". Traveling Wave Analysis of Partial Differential Equations. Amsterdam: Elsevier/Academic Press. doi:10
Tzitzeica_equation
Equation in fluid dynamics
a discontinuity at the peak in the wave slope. The Camassa–Holm equation can be written as the system of equations: u t + u u x + p x = 0 , p − p x x
Camassa–Holm_equation
The Hirota–Satsuma equation is a mathematical model of interactions of two long waves with different dispersion relations, expressed as a set of three
Hirota–Satsuma_equation
Aspect of relativity in physics
frequency of a gravitational wave are related by the equation c = λf, just like the equation for a light wave. For example, the animations shown here oscillate
Gravitational_wave
Equations of motion for viscous fluids
the design of power stations, the analysis of pollution, and many other problems. Coupled with Maxwell's equations, they comprise the fundamentals of
Navier–Stokes_equations
Dimensionless quantity related to porosity
parameter. Because of this, in soil science and geotechnics, these two equations are usually presented using η {\displaystyle {\eta }} for porosity: e
Void_ratio
Amount of water an aquifer releases while staying saturated
{\displaystyle \sigma _{e}} is the effective stress (N/m2 or [MLT−2/L2]) These equations relate a change in total or water volume ( V t {\displaystyle V_{t}} or
Specific_storage
Area of mathematical analysis
theorems. Harmonic analysis overlaps substantially with Fourier analysis, real analysis, functional analysis, partial differential equations, potential theory
Harmonic_analysis
Second-order partial differential equation
In mathematics and physics, Laplace's equation is a second-order partial differential equation named after Pierre-Simon Laplace, who first studied its
Laplace's_equation
Gardner equation. Korteweg–de Vries equation Polyanin & Zaitsev 2003. Griffiths, Graham W.; Schiesser, W. E. (2011). Traveling Wave Analysis of Partial
Modified Korteweg–De Vries equation
Modified_Korteweg–De_Vries_equation
Study of classical optics using Fourier transforms
Substituting this expression into the scalar wave equation above yields the time-independent form of the wave equation, Re { ( ∇ 2 + k 2 ) ψ ( r ) } = 0 {\displaystyle
Fourier_optics
Quantum mechanical waves describing matter
1926, Schrödinger published the wave equation that now bears his name – the matter wave analogue of Maxwell's equations – and used it to derive the energy
Matter_wave
Method of analysis applied to problems wave propagation
diffraction, based on the wave equation. The arbitrary assumptions made by Fresnel to arrive at the Huygens–Fresnel equation emerge automatically from
Huygens–Fresnel_principle
Earthquake probability in a specific area and time
seismic risk analysis, Bulletin of the Seismological Society of America, 58, 1583-1606 McGuire, R. 2008, Probabilistic seismic hazard analysis: Early history
Seismic_hazard
Quantum mechanical phenomenon
The analysis of a rectangular barrier by means of the Schrödinger equation can be adapted to these other effects provided that the wave equation has travelling
Quantum_tunnelling
Ruze's equation is an equation relating the gain of an antenna to the root mean square (RMS) of the antenna's random surface errors. The equation was originally
Ruze's_equation
Physics phenomenon and formula
fluid dynamics, the mild-slope equation describes the combined effects of diffraction and refraction for water waves propagating over bathymetry and
Mild-slope_equation
Model of electrically conducting fluids
solar wind. The wave modes derived from the MHD equations are called magnetohydrodynamic waves, or MHD waves. There are three MHD wave modes that can be
Magnetohydrodynamics
Branch of physics
solutions to Maxwell's equations to calculate antenna performance, electromagnetic compatibility, radar cross section and electromagnetic wave propagation when
Computational electromagnetics
Computational_electromagnetics
Elastic waves propagating in solid plates or spheres
Testing Encyclopedia Lamb Wave Analysis of Acousto-Ultrasonic Signals in Plate by Liu Zhenqing: an article which includes the complete Lamb wave equations.
Lamb_waves
Response of a structure to oscillation
systems), although they are only accurate for low levels of damping. Modal analysis is performed to identify the modes, and the response in that mode can be
Response_spectrum
Australian and American mathematician (born 1975)
in 2006 for his contributions to partial differential equations, combinatorics, harmonic analysis, and additive number theory. He is a professor of mathematics
Terence_Tao
Describe the partitioning of seismic wave energy at an interface
reflection seismology, the Zoeppritz equations are a set of equations that describe the partitioning of seismic wave energy at an interface, due to mode
Zoeppritz_equations
Description of the ground state of a quantum system
the Schrödinger equation with the addition of an interaction term. The coupling constant g {\displaystyle g} is proportional to the s-wave scattering length
Gross–Pitaevskii_equation
Wave that remains in a constant position
have constant amplitude. Equation (1) still describes the standing wave pattern that can form on this string, but now Equation (1) is subject to boundary
Standing_wave
Equation that calculates gas diffusion across membranes
Clarke's equation is a third-order nonlinear partial differential equation, first derived by John Frederick Clarke in 1978. The equation describes the
Clarke's_equation
Equation known for chaotic behavior
mathematics, the Kuramoto–Sivashinsky equation (also called the KS equation) is a partial differential equation used to model complex patterns and chaotic
Kuramoto–Sivashinsky_equation
counterpart of the Ishimori equation is the Davey-Stewartson equation. Nonlinear Schrödinger equation Heisenberg model (classical) Spin wave Landau–Lifshitz model
Ishimori_equation
Class of partial differential equations
classical wave equation. This has led to a number of developments concerning its characteristics, one of which is due to Fritz John: the John equation. In 2008
Ultrahyperbolic_equation
Type of wave
The equations for sound in a fluid given above also apply to acoustic waves in an elastic solid. Although solids also support transverse waves (known
Longitudinal_wave
System where changes of output are not proportional to changes of input
methods of solution or analysis are problem dependent. Examples of nonlinear differential equations are the Navier–Stokes equations in fluid dynamics and
Nonlinear_system
Richard A.; Kitts, Christopher A. (2014-08-01). "Tsunami-generated sediment wave channels at Lake Tahoe, California-Nevada, USA". Geosphere. 10 (4): 757–768
List_of_landslides
Davey–Stewartson equation (DSE) was introduced in a paper by A. Davey and Keith Stewartson to describe the evolution of a three-dimensional wave-packet on water
Davey–Stewartson_equation
WAVE EQUATION-ANALYSIS
WAVE EQUATION-ANALYSIS
Boy/Male
English
Alert.
Boy/Male
American, British, Christian, Danish, Dutch, English, French, German, Hebrew, Hindu, Indian, Jamaican, Punjabi, Scottish, Sikh, Swiss
Beloved; David's Son; Form of David
Boy/Male
Anglo Saxon English
Wise.
Boy/Male
Australian, Finnish
Permanent
Surname or Lastname
English (of Norman origin) and northern French
English (of Norman origin) and northern French : nickname for a bald man, from Anglo-Norman French cauf ‘bald’. Compare Chaffee.English : habitational name from a place in East Yorkshire called Cave, apparently from a river name derived from Old English cÄf ‘swift’.French : metonymic occupational name for someone employed in or in charge of the wine cellars of a great house, from Old French cave ‘cave’, ‘cellar’ (Latin cavea, a derivative of cavus ‘hollow’).French, possibly also English : topographic name for someone who lived in or near a cave, from the same word as in 3 in an older sense.
Male
English
 English topographical surname transferred to forename use, WADE means "lives near the river crossing." Middle English form of Anglo-Saxon Wada (the name of a sea giant), meaning "to go," in the sense of going forward, proceeding.
Boy/Male
Anglo Saxon American English Scandinavian
Moving.
Boy/Male
Hebrew American Scottish Welsh
Cherished; Beloved.
Girl/Female
Irish
Joy.
Surname or Lastname
English
English : occupational name for a servant, from Middle English knave ‘boy’, ‘youth’, ‘servant’.English : possibly a metonymic occupational name for a maker of wheel-hubs, Middle English nave (from Old English nafa, nafu).German (also Näve) : variant of Neff (see Neve).Dutch (de Nave) : variant of Naef 1.In some cases possibly Portuguese : topographic name from nave ‘plain’ (a variant of nava), or a habitational name from a place named with this word. Compare Nava.
Boy/Male
Hindu
Variant of David beloved
Surname or Lastname
English
English : from a Germanic personal name Walo, either a byname meaning ‘foreigner’ (see Wallace), or else a short form of the various compound names with this first element.English : nickname for a well-liked person, from Middle English wale ‘good’, ‘excellent’ (originally meaning ‘choice’).English : topographic name for someone who lived near an embankment, Middle English wale (Old English walu).
Boy/Male
Anglo, British, English, Jamaican
Wise; Watchful; Aware; Watchman; Careful
Surname or Lastname
English
English : variant spelling of Way.
Female
Irish
Variant spelling of Irish Maeve, MAVE means "intoxicating."Â
Male
English
English short form of Hebrew David, DAVE means "beloved."
Surname or Lastname
English
English : from the Middle English personal name Wade, Old English Wada, from wadan ‘to go’. (Wada was the name of a legendary sea-giant.)English : topographic name for someone who lived near a ford, Old English (ge)wæd (of cognate origin to 1), or a habitational name from a place named with this word, as for example Wade in Suffolk.Dutch and North German : occupational name or nickname from Middle Dutch, Middle Low German wade ‘garment’, ‘large net’.Jonathan Wade emigrated from Norfolk, England, to Medford, MA, in 1632. Benjamin Franklin Wade (1800–1878), born near Springfield, MA, was a prominent U.S. senator from OH during the Civil War.
Girl/Female
Slavic
Stranger. Pet name formed from Varvara; the Russian form of Barbara.
Surname or Lastname
English
English : topographic name for someone who lived by a dam or weir on a river (Old English wær, wer), or a habitational name from a place named with this word, such as Ware in Hertfordshire.English : nickname for a cautious person, from Middle English war(e) ‘wary’, ‘prudent’ (Old English (ge)wær).English : Robert Ware came to Dedham, MA, from England in or before 1642. Henry Ware (1764–1845), born in Sherborn, MA, was a Unitarian clergyman and theologian and father of the physician John Ware (b. 1795) and two clergymen, Henry (b. 1794) and William (b. 1797).
Boy/Male
Anglo, British, English
Alert; Watchman
WAVE EQUATION-ANALYSIS
WAVE EQUATION-ANALYSIS
Girl/Female
Tamil
Mohanadhvani | மோஹநாதவாநீ
Name of a Raga
Boy/Male
Australian, German, Swedish
Spear
Boy/Male
Hindu, Indian, Tamil
Courageous
Male
Hebrew
Contracted form of Hebrew Shemuwel, SHMUEL means "heard of God," "his name is El," or "name of God."Â
Boy/Male
Hindu, Indian
Winner
Boy/Male
Hindu, Indian, Traditional
The Greatest God
Surname or Lastname
English
English : patronymic from a pet form of the personal name Rollo or Rolf.
Biblical
the God of my eyes
Boy/Male
Australian, Indian
Sun
Boy/Male
Hindu
Princess, Noble woman
WAVE EQUATION-ANALYSIS
WAVE EQUATION-ANALYSIS
WAVE EQUATION-ANALYSIS
WAVE EQUATION-ANALYSIS
WAVE EQUATION-ANALYSIS
a.
Rising or swelling in waves; full of waves.
v. i.
A vibration propagated from particle to particle through a body or elastic medium, as in the transmission of sound; an assemblage of vibrating molecules in all phases of a vibration, with no phase repeated; a wave of vibration; an undulation. See Undulation.
v. i.
To fluctuate; to waver; to be in an unsettled state; to vacillate.
v. t.
To move like a wave, or by floating; to waft.
imp.
of Weave
n.
The act or process of educating; the result of educating, as determined by the knowledge skill, or discipline of character, acquired; also, the act or process of training by a prescribed or customary course of study or discipline; as, an education for the bar or the pulpit; he has finished his education.
n.
A wave.
a.
Exhibiting a wavelike form or outline; undulating; intended; wavy; as, waved edge.
v. i.
To dwell in a cave.
Indic. present
of Have
n.
The process of separating, by heat, an easily fusible metal from one less fusible; eliquation.
n.
A wale knot, or wall knot.
v. t.
See Waive.
v. i.
To play loosely; to move like a wave, one way and the other; to float; to flutter; to undulate.
imp. & p. p.
of Wave
n.
A wave.
v. i.
Fig.: A swelling or excitement of thought, feeling, or energy; a tide; as, waves of enthusiasm.
n.
An expression of the condition of equality between two algebraic quantities or sets of quantities, the sign = being placed between them; as, a binomial equation; a quadratic equation; an algebraic equation; a transcendental equation; an exponential equation; a logarithmic equation; a differential equation, etc.