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Physical quantity

A physical quantity is a property of a , , or substance that can be quantified for the purpose of comparison, calculation, or communication, and is expressed as the product of a numerical and a . In physics and , physical quantities form the foundation for describing natural phenomena and building mathematical models, enabling precise measurements and predictions. They are broadly classified into base quantities, which are considered dimensionally independent and defined through fundamental standards, and derived quantities, which are calculated from combinations of base quantities. The (SI) establishes seven base physical quantities—, , time, , , , and —each associated with a corresponding base : meter (m), (kg), second (s), (A), (K), (mol), and (cd), respectively. Examples of derived quantities include (derived from and time), (from , , and time), and (from , squared, and time squared), with their units formed coherently from the base units to ensure consistency in scientific equations. This systematic framework, maintained by international standards organizations, ensures uniformity in measurements across disciplines and facilitates global scientific collaboration.

Fundamentals

Definition

According to the International Vocabulary of Metrology (VIM), a physical quantity, or simply , is "a of a , body, or substance, where the property has a that can be expressed as a number and a reference." This sets it apart from purely qualitative descriptions. Examples include , , and , which describe observable attributes in numerical form rather than vague terms like "large" or "hot." This quantification enables the formulation of scientific laws and predictions based on empirical data. Key attributes of physical quantities include their measurability using standardized procedures, reproducibility under controlled conditions, and expression in numerical terms, often with associated units. These ensure that measurements can be compared across experiments and contexts, forming the foundation of scientific . A physical quantity typically consists of a expressed numerically alongside a , though the focus here is on the conceptual essence rather than structural breakdown. The concept originated in classical physics, where pioneers like Galileo and Newton emphasized the importance of quantification to describe natural phenomena precisely, moving away from qualitative Aristotelian explanations. Galileo advocated for mathematical descriptions of motion through experiments, while Newton formalized these ideas in his laws of motion, integrating measurement into the core of mechanics. This approach evolved into modern physics, where physical quantities underpin theories from to , always rooted in empirical validation. Unlike mathematical quantities, which are abstract constructs like pure numbers or variables defined axiomatically without reference to the physical world, physical quantities are intrinsically linked to real-world phenomena and thus subject to inherent uncertainties arising from measurement limitations and experimental variability. These uncertainties reflect the probabilistic nature of observations, distinguishing physical science from pure mathematics where exactness prevails.

Components

A physical quantity is fundamentally composed of a numerical value, which represents its , and a , which specifies the scale relative to a defined ; in some contexts, a or kind of may also be included to categorize the being measured. The numerical value can be a simple scalar number for quantities like or , or it may take a more complex form, such as multiple components for directional quantities like , though the core idea remains a quantifiable measure of size or extent. Units play a crucial role by providing a standardized reference that scales the numerical value to ensure comparability across measurements; for instance, the unit meter defines the reference length such that a numerical value of 1 corresponds to that exact span. This scaling allows physical quantities to be expressed consistently within agreed-upon systems, facilitating communication and in science and . The concept of quantity calculus formalizes this decomposition, treating physical quantities as products of their numerical values and units, independent of specific choices of units. In this framework, a physical Q is expressed as Q = [Q] \times \{Q\}, where [Q] denotes the numerical value (a dimensionless number) and \{Q\} the unit (a quantity of one in the chosen system). This relation arises because the full quantity Q must remain invariant under changes in the unit; if the unit \{Q\} is altered by a factor, the numerical value [Q] adjusts inversely to preserve Q. For example, a of 5 is written as Q = 5 \times \{ \mathrm{m} \}, where 5 is the numerical value and (\mathrm{m}) the unit; equivalently, the same could be 500 centimeters, with Q = 500 \times \{ \mathrm{cm} \}. This product structure underpins algebraic operations on quantities, ensuring dimensional consistency in equations. Dimensions serve as an abstract framework for these components, classifying quantities by their fundamental attributes like or time, though detailed of dimensions is covered separately.

Notation

Symbols and Nomenclature

In physical sciences, standard symbols for quantities are typically single uppercase or lowercase letters from the Latin or alphabets, printed in an italic font to distinguish them from units and constants. For instance, the symbol m denotes , v represents , and t indicates time, as recommended in the ISO 80000 series, which provides comprehensive guidelines for quantities across disciplines like , , and . These conventions ensure clarity and consistency in scientific communication by avoiding ambiguity in notation. Nomenclature rules emphasize a clear distinction between symbols for physical quantities and those for units: quantity symbols are italicized variables, while unit symbols are upright (roman) type and often derived from proper names or abbreviations. For example, t (italic) symbolizes the quantity of time, whereas s (roman) denotes the unit second; similarly, m (italic) for mass contrasts with kg (roman) for . This separation prevents misinterpretation, as quantity symbols represent variables that can take numerical values, whereas unit symbols are fixed and invariant. International standards from organizations like the International Bureau of Weights and Measures (BIPM) and the International Union of Pure and Applied Physics (IUPAP) promote uniform usage to facilitate cross-disciplinary and global collaboration. The BIPM's SI Brochure outlines base and derived quantity symbols aligned with the (SI), while IUPAP's recommendations in its "" extend these to advanced physics contexts, ensuring symbols like E for or p for are consistently applied. These guidelines are harmonized with ISO 80000 to cover all major fields, reducing variability in publications and education. Common pitfalls in nomenclature include confusion between similar symbols, such as using u for scalar speed versus v (or bold v) for the velocity vector, which can lead to errors in interpreting directionality or magnitude. Adherence to standards mitigates such issues by reserving v primarily for velocity and advising explicit vector notation where needed. The evolution of nomenclature transitioned from ad hoc notations in 19th-century physics—where figures like James Clerk Maxwell employed inconsistent symbols across treatises—to unified systems following the 1960 adoption of the by the General Conference on Weights and Measures (CGPM). This standardization, bolstered by the series (precursor to ISO 80000) in the , addressed fragmentation from competing systems like CGS and MKS, establishing a coherent framework that persists today.

Typography

In scientific writing, symbols representing physical quantities are conventionally printed in italic type to distinguish them from surrounding text, such as the velocity symbol v or mass m. In contrast, symbols for units are set in upright Roman typeface, as in the expression for speed v = 5 m/s, where "m/s" remains upright. For vectors, common conventions include boldface italic type, such as v, or an arrow diacritic in handwritten or inline contexts, denoted as \vec{v}. Tensors are typically represented using boldface , often bold italic for higher-order tensors to differentiate them from vectors, though double boldface or other extensions may be employed in specialized fields. Subscripts and superscripts follow specific rules based on their semantic role: those denoting quantities, variables, or indices, such as component xi, are italicized, while descriptive labels, such as the molar subscript m in the heat capacity C_{p,m}, appear in upright . Powers and exponents representing mathematical operations are also upright when they are constants or labels, ensuring clarity in expressions like or calculations. The (ISO) outlines these conventions in ISO 80000 and related directives, recommending italic serif fonts for quantities in print media, with bold italics for vectors and tensors, and consistent spacing around symbols to enhance readability in both print and formats. The (AMS) aligns closely in its style guide, favoring boldface for vectors over arrows in typeset to streamline production, while advising upright fonts for units and labels across and print contexts. These typographic standards evolved from 19th-century handwritten scripts, where arrows and underlining denoted vectors, to standardized printed conventions in the , facilitated by advances in technologies like linotype machines that enabled italic and bold variants for precise mathematical expression.

Mathematical Representation

Scalars

In physics, a scalar quantity is defined as a physical quantity that possesses only and no direction, remaining unchanged regardless of the observer's . Such quantities are under coordinate transformations, including rotations, meaning their value does not depend on the or of the reference frame. Scalar quantities exhibit properties of additivity and scalar , allowing them to be combined through basic arithmetic operations when dimensionally compatible. For instance, the sum of two scalars q_1 and q_2 is given by q = q_1 + q_2, and their product by q = q_1 \cdot q_2, provided the principle of dimensional homogeneity is satisfied—ensuring that all terms in an equation share the same dimensions to maintain physical consistency. Common examples include (m), (T), and (E), each describable by a single numerical value with appropriate units. These quantities form the foundational building blocks for many derived physical quantities in physics, such as work or , which emerge from scalar operations on more complex forms. In contrast to non-scalar quantities like vectors, scalars alone cannot capture directional aspects of phenomena. Their primary limitation lies in their inability to represent oriented physical effects, such as the motion of an object, which requires additional directional information.

Vectors

In physics, a vector quantity is defined as a physical entity that possesses both and , and transforms in a specific manner under spatial rotations, maintaining its directional integrity relative to the . Unlike scalar quantities, which have only and remain invariant under rotations, vectors such as or change their components predictably when the is rotated. Classic examples include \vec{v}, which describes the rate of change of position with direction, and \vec{F}, which imparts directional influence on an object's motion. Vector quantities obey specific algebraic properties that enable their manipulation in physical equations. Vector addition follows the , where the resultant vector \vec{c} is obtained by placing the tail of one vector at the head of the other and drawing the diagonal of the parallelogram formed by them, such that \vec{a} + \vec{b} = \vec{c}. Additionally, vectors can be combined using the , which yields a scalar representing the projection of one vector onto another (e.g., work as \vec{F} \cdot \vec{d}), and the cross product, which produces a vector perpendicular to both operands, useful for quantities like torque (\vec{\tau} = \vec{r} \times \vec{F}). These operations are foundational for resolving forces and motions in multi-dimensional systems. Vectors are typically represented in a chosen basis, such as the , where a three-dimensional vector \vec{v} is expressed as a linear combination of unit vectors: \vec{v} = v_x \hat{i} + v_y \hat{j} + v_z \hat{k}, with v_x, v_y, and v_z as its scalar components along the respective orthogonal axes. This decomposition allows vectors to be analyzed component-wise, simplifying calculations in Newtonian mechanics and beyond. The magnitude of a vector, which is its length and a scalar quantity, is computed using the Euclidean norm: |\vec{v}| = \sqrt{v_x^2 + v_y^2 + v_z^2} derived from the Pythagorean theorem applied to the right triangle formed by its components. Vector quantities are indispensable in various domains of physics, particularly kinematics, where they describe directional motion (e.g., velocity \vec{v} = \frac{d\vec{r}}{dt}), and electromagnetism, where fields like the electric field \vec{E} and magnetic field \vec{B} govern charged particle interactions through directional forces. A notable subclass includes pseudovectors, or axial vectors, which transform like ordinary vectors under rotations but acquire an opposite sign under spatial inversion (parity); angular momentum \vec{L} = \vec{r} \times \vec{p} exemplifies this, distinguishing it from polar vectors like linear momentum.

Tensors

In physics, tensors are mathematical objects that generalize scalars and to represent physical quantities with multiple directions or orientations, defined as multi-linear maps from vector spaces to scalars or, equivalently, as multi-dimensional arrays whose components transform according to specific rules under changes of coordinates. They are characterized by contravariant and covariant indices, where upper indices denote contravariant components and lower indices denote covariant ones, allowing tensors to describe quantities like forces or stresses that depend on the choice of basis. Tensors are classified by their rank, which is the number of indices required to specify a component; a rank-0 tensor is a scalar, a rank-1 tensor is a , a rank-2 tensor has two indices (e.g., the stress tensor \sigma_{ij} or the inertia tensor I_{ij}), and higher-rank tensors have more indices, such as the rank-4 R^\rho_{\sigma\mu\nu}. Vectors, as rank-1 tensors, are special cases that handle quantities with a single direction, but tensors extend this to multi-directional interactions essential for complex physical laws. Under a coordinate from x to x', tensor components obey precise transformation laws to ensure the physical quantity remains ; for a rank-2 covariant tensor like the stress tensor, the components transform as \sigma'_{kl} = \frac{\partial x^m}{\partial x'^k} \frac{\partial x^n}{\partial x'^l} \sigma_{mn}, where the partial derivatives form the matrix of the transformation. Contravariant tensors transform , using the , while mixed tensors combine both. Key properties of tensors include , where components satisfy \sigma_{ij} = \sigma_{ji} for many physical tensors like or , reducing the number of independent components from 9 to 6 for rank-2 cases, and the , defined as the of diagonal elements \operatorname{tr}(\sigma) = \sigma_{ii}, which often represents an isotropic part such as hydrostatic in the tensor. The exhibits additional antisymmetries, such as R^\rho_{\sigma\mu\nu} = -R^\rho_{\sigma\nu\mu}, reflecting the oriented nature of . Tensors play a crucial role in , where the stress tensor \sigma_{ij} describes internal forces within materials, quantifying how force acts across surfaces in different directions. In , the inertia tensor I_{ij} governs rotational motion by relating to via \mathbf{L} = I \boldsymbol{\omega}, capturing the distribution's on . In , the Riemann tensor measures , encoding gravitational s as forces in Einstein's field equations. These applications highlight tensors' necessity for formulating covariant physical laws beyond the limitations of scalars and vectors.

Dimensions and Measurement

Dimensions

In physics, the dimension of a physical quantity provides an abstract classification of its fundamental nature, expressed as a product of powers of the seven base dimensions in the (SI). These base dimensions correspond to the SI base quantities and are denoted by symbols such as for , for , T for time, I for , Θ for , N for , and J for . Any derived dimension is then a combination of these, such as the dimension of , denoted , which is L T^{-1}, indicating one power of length and negative one power of time. A core principle governing the use of dimensions is dimensional homogeneity, which mandates that every valid physical or must balance dimensionally on both sides, ensuring all terms share identical dimensions. For example, in the for v = s / t, where s is and t is time, the dimensions satisfy = ^{-1} = L T^{-1}, confirming homogeneity across the . This principle extends to additive terms as well, requiring each to possess the same dimensions, thereby preventing nonsensical combinations like adding lengths to masses. The formalizes the role of dimensions in analyzing complex physical systems by reducing them to dimensionless groups. Introduced by Edgar Buckingham in , the theorem asserts that if a problem involves n physical variables expressible in terms of m fundamental dimensions, the solution can be reformulated as a relation among at most n - m independent dimensionless π parameters. These π groups, formed by combinations that eliminate dimensions, enable scaling analysis, such as predicting fluid flow behavior across different sizes without solving full equations. Dimensions find practical applications in verifying the consistency of physical equations and conducting for model scaling. By checking dimensional homogeneity, researchers can detect errors in derived formulas, as mismatched dimensions immediately signal an inconsistency. In engineering and scientific modeling, leverages the to identify key dimensionless numbers—like the in —that govern system behavior, facilitating efficient predictions from scaled prototypes to full-scale systems.

Units

A unit is a particular physical quantity, defined and adopted by convention, with which other quantities of the same kind are compared to express their magnitudes relative to that unit. For example, the metre (m) is defined as the length of the path travelled by light in vacuum during a time interval of $1/299792458 of a second. The (SI), established in 1960 and coordinated by the International Bureau of Weights and Measures (BIPM), comprises seven base units from which all other units are derived: (s) for time, (m) for length, kilogram (kg) for mass, ampere (A) for electric current, kelvin (K) for thermodynamic temperature, (mol) for amount of substance, and (cd) for luminous intensity. Derived units are formed by combining these base units through multiplication and division; for instance, the (N), the unit of , is defined as \mathrm{kg \cdot m \cdot s^{-2}}. Historically, SI units relied on physical artifacts for realization, such as the platinum-iridium bar deposited in and the international prototype kilogram maintained at the BIPM since . Over time, definitions shifted toward natural phenomena for greater stability: the was redefined in 1983 using the , and the second in 1967 using caesium-133 hyperfine transition frequency. The 2019 revision, effective from 20 May 2019, anchored all seven base units to fixed values of fundamental constants—such as the c, h, and e—eliminating artifact dependencies entirely and ensuring universal reproducibility. In the SI, coherent units form a system where derived units are exact products or quotients of base units without additional numerical factors other than unity, preserving the form of physical equations when expressed numerically. This coherence simplifies calculations; for example, the joule (J) for energy is simply \mathrm{kg \cdot m^2 \cdot s^{-2}}, requiring no conversion coefficients in formulas like kinetic energy E = \frac{1}{2}mv^2. Unit conversions between systems rely on , ensuring consistency by treating units as algebraic quantities that cancel appropriately. For instance, to convert miles to kilometres, multiply by the factor $1.609344\ \mathrm{km/mile}, yielding $1\ \mathrm{mile} = 1.609344\ \mathrm{km}.

Quantity Kinds

In the (ISQ) as defined by ISO 80000, quantity kinds represent semantic categories that classify based on their intrinsic , grouping those with comparable properties while distinguishing them from even if they share the same dimensional structure. A quantity kind specifies the type of measurable , such as , , or , enabling consistent interpretation across scientific disciplines; for instance, all lengths—whether , width, or —belong to the same kind despite varying contexts. This classification ensures that quantities within a kind can be directly compared or combined mathematically, while those of different kinds require careful consideration to avoid misapplication. The distinction between quantity kinds and dimensions is crucial, as quantities of the same may belong to different kinds, reflecting their unique physical interpretations. According to ISO 80000-1, quantities of different dimensions are always of different kinds, but the converse does not hold: for example, (or moment of force) and both possess the dimension ML²T⁻² yet are conventionally regarded as distinct kinds, preventing the use of the joule for despite dimensional compatibility. Similarly, and work share the same dimension but are treated as separate kinds to preserve conceptual clarity in thermodynamic processes. Another illustration is and , both quantified in joules per (J/K) with dimension ML²T⁻²Θ⁻¹, but representing fundamentally different properties—disorder versus per change—thus requiring kind-specific handling in equations. Quantity kinds play a vital role in international standards by promoting precise communication and avoiding ambiguities in measurement and calculation. In fields like engineering, this separation ensures that interchangeable units do not imply physical equivalence; for example, while specific units apply to particular kinds, such as the farad for capacitance, the framework discourages conflating dimensionally similar but semantically distinct quantities like certain electrical susceptibilities and mechanical flexibilities. This structured typology underpins the ISQ's coherence, facilitating error-free applications in complex systems. Dimensionless kinds form a special category within this system, encompassing pure numbers or ratios that lack dimensional exponents but still require kind-specific identification to convey meaning. As outlined in ISO 80000-11, these are physical quantities of unit one, often called characteristic numbers, such as the Reynolds number, which characterizes fluid flow regimes as a ratio of inertial to viscous forces. Distinguishing these kinds prevents misinterpretation in analyses where, for instance, the Reynolds number (flow dynamics) differs from the Mach number (compressibility effects), both dimensionless yet contextually unique. In modern applications, quantity kinds are integral to and data standards, enabling robust software implementations for simulations and . Libraries like mp-units enforce kind-based type checking to catch errors in unit conversions and equation validations, ensuring that dimensionally compatible but kind-distinct quantities, such as and , are not erroneously equated in numerical models. This approach supports high-fidelity data exchange in interdisciplinary fields, from climate modeling to engineering design.

Classification

Base Quantities

Base quantities represent the fundamental, irreducible physical entities chosen as the independent foundations of a measurement system, from which all other physical quantities can be derived through mathematical combinations such as products and quotients of powers. These quantities are selected to ensure mutual dimensional independence, meaning no base quantity can be expressed in terms of the others, while collectively providing a complete framework for describing the full range of observable physical phenomena. In the International System of Units (SI), established by the General Conference on Weights and Measures, seven base quantities form this foundation, each associated with a specific as standardized in the SI Brochure. These are: The selection of these quantities reflects historical development and practical utility in science, , and , ensuring they capture the core aspects of , , , , and . The definitions of SI base units underwent a significant revision effective 20 May 2019, shifting from artifact-based or observational standards to exact numerical values of seven defining constants of nature. This redefinition ties the to the h, the to the e, the to the k, and the to the N_A, while the , second, and remain linked to the c, caesium frequency \Delta \nu_{\text{Cs}}, and luminous efficacy K_{\text{cd}}, respectively. This change enhances the SI's stability, universality, and alignment with fundamental physics, eliminating reliance on physical prototypes and enabling more precise realizations worldwide. Other systems employ different base quantities to suit specific domains. For instance, the centimeter-gram-second (CGS) system, developed in the late for mechanical and electromagnetic applications, contrasts with the by using only three base quantities: (centimeter), (gram), and time (second), emphasizing simplicity in Gaussian or electrostatic variants for .

Derived Quantities

Derived quantities are physical quantities that cannot be measured directly but are instead obtained through mathematical combinations—such as products, quotients, powers, or sums—of base quantities or other derived quantities. For instance, emerges as the ratio of (a ) to time. This construction allows derived quantities to represent more complex aspects of physical phenomena while remaining rooted in the fundamental base quantities. The dimensional expression for a derived quantity Q takes the general form [Q] = \mathrm{L}^a \mathrm{M}^b \mathrm{T}^c \mathrm{I}^d \mathrm{\Theta}^e \mathrm{N}^f \mathrm{J}^g, where \mathrm{L}, \mathrm{M}, \mathrm{T}, \mathrm{I}, \mathrm{\Theta}, \mathrm{N}, and \mathrm{J} denote the base dimensions of length, mass, time, electric current, thermodynamic temperature, amount of substance, and luminous intensity, respectively, and the exponents a, b, c, \dots, g are real numbers determined by the defining operations. This formulation captures how the dimensions of the inputs dictate those of the output, ensuring traceability to the seven SI base quantities. A key governing derived quantities is dimensional homogeneity, which requires that all terms in a physically meaningful possess identical dimensions; or is only valid between quantities of the same dimensional type, while and yield new dimensions from the factors involved. This upholds the consistency of physical equations, preventing nonsensical operations like adding to . Derived quantities fall into general categories, such as those expressing rates (e.g., speed) or intensities (e.g., pressure), and specific ones tailored to particular contexts, but their diversity is theoretically infinite despite the finite set of base quantities, as any combination of exponents and operations can produce novel forms./02%3A_Comparing_Model_and_Experiment/2.02%3A_Units_and_dimensions) They are indispensable for articulating intricate physical laws; for example, in Newton's second law, force is a derived quantity defined as F = ma, with dimensions [\mathrm{M} \mathrm{L} \mathrm{T}^{-2}], linking mass and acceleration to describe motion. This framework enables the systematic modeling of interactions across scales in physics./05%3A_Newtons_Laws_of_Motion/5.02%3A_Newtons_First_Law)

Examples of Derived Quantities

Derived physical quantities are formed by combining base quantities through multiplication and division, illustrating how fundamental dimensions yield more complex properties observable in nature. Spatial quantities provide foundational examples: position, often treated as a displacement vector, has the dimension of length [L], while velocity, the rate of change of position, possesses the dimension [L T^{-1}], and acceleration, the rate of change of velocity, has [L T^{-2}]. These demonstrate the progression from static to dynamic spatial descriptions in kinematics. Densities, flows, gradients, and moments further exemplify derived quantities across various physical domains. Density, such as mass density, combines and to yield [M L^{-3}], quantifying how mass is distributed in space. Flux quantities, like , involve mass per unit time with dimension [M T^{-1}], essential for describing . Gradients, for instance, the , express change in over distance as [\Theta L^{-1}], where \Theta denotes temperature, highlighting spatial variations in scalar fields. Moments, such as the , arise from charge separation over distance, resulting in dimension [I T L], where I is electric current, capturing asymmetry in charge distributions. Other prominent derived quantities include and , with (e.g., kinetic or potential) having dimension [M L^{2} T^{-2}] and , the rate of energy transfer, [M L^{2} T^{-3}]. , while a base quantity in some historical systems, is derived in the SI as current integrated over time, yielding [I T]. Thermodynamic , measuring or unavailable , combines and to give [M L^{2} T^{-2} \Theta^{-1}]. These underscore the interplay of mechanical, electrical, and thermal base quantities in forming quantities central to and the second law of . Dimensionless derived quantities emerge when dimensions cancel out, providing scale-invariant ratios useful in comparative analyses. The , defined as the ratio of flow velocity to the , is dimensionless and classifies flow regimes from subsonic to supersonic. The fine-structure constant \alpha, approximately $1/137, quantifies the strength of electromagnetic interactions between elementary charged particles and is also dimensionless. Such quantities are pivotal in , as their unitless nature allows universal applicability across different measurement systems.

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