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Conservation of mass

The law of conservation of , a fundamental principle in and physics, states that the total of all substances involved in a remains constant before and after any physical or , implying that cannot be created or destroyed. This principle, first quantitatively established through experiments, asserts that in chemical reactions, the of the reactants equals the of the products. Formulated by French chemist in the late 18th century—specifically around 1785 during his studies of and —this law marked a pivotal shift in scientific thought by disproving the prevailing , which posited that a weightless substance called phlogiston was released during burning, inconsistently explaining observed mass changes. Lavoisier's meticulous measurements, often conducted with his wife Marie-Anne as a collaborator, demonstrated that involved the combination with oxygen (then called "dephlogisticated air"), and that mass was preserved, laying the groundwork for and modern quantitative chemistry. His work, published in Traité élémentaire de chimie in 1789, emphasized precise weighing and sealed reaction vessels to ensure no matter escaped, revolutionizing chemical analysis. In , the underpins balancing chemical equations and predicting outcomes, enabling advancements in fields from synthesis to , while remaining valid for all ordinary chemical processes where energy-mass conversions are negligible. In physics, it manifests as the in , describing how mass flow remains constant in incompressible flows, essential for engineering applications like and . However, in modern relativistic physics, as articulated by in 1905, the principle extends to the conservation of mass-energy, where mass can convert to energy via E = mc^2, as seen in reactions, though the total mass-energy remains invariant. This unified conservation law integrates the classical principle with , confirming its enduring relevance across scales from atomic to cosmic.

Core Concepts

Definition and Statement

The conservation of mass is a fundamental principle in and stating that, in a , the total remains constant over time, as cannot be created or destroyed through ordinary chemical reactions or physical transformations. This law underscores the invariance of mass in processes where no enters or leaves the system, forming a for understanding material transformations. A is defined as a collection of that does not exchange with its surroundings (though may be exchanged), ensuring that any changes occur internally without external mass influence. The total in such a system represents the aggregate of all individual masses of its components, which stays unchanged regardless of internal rearrangements or conversions between forms of . Intuitively, this aligns with everyday observations; for example, when boils, the liquid seems to vanish, but its is preserved in the form of that disperses into the air if the system is not fully enclosed. Likewise, burning a piece of wood appears to reduce its mass to ash, yet including the mass of released gases like and , along with the consumed oxygen, yields the same total as the original wood. These examples illustrate how mass conservation holds even when products are not immediately visible. The empirical basis of the conservation of mass derives from reproducible experiments in closed setups, where precise measurements consistently show mass before and after processes to be equal.

Mathematical Formulation

The conservation of mass principle in and is quantitatively expressed for a —where no crosses the boundaries—as the total remaining constant over time: m_{\text{initial}} = m_{\text{final}}, or equivalently, \frac{dm}{dt} = 0, with m denoting the total of the . For discrete systems, such as a involving distinct reactants and products, derives from summing the masses on both sides of the process, ensuring balance without creation or destruction of . Consider reactants with masses m_A and m_B transforming into products with masses m_C and m_D; the conservation equation is m_A + m_B = m_C + m_D, which extends to any finite number of components where the total initial mass equals the total final mass. In continuous systems, such as those analyzed in or , the principle manifests as a equation. For a (one with impermeable boundaries and no internal sources or sinks of mass), the rate of change of mass is zero: \frac{dm}{dt} = 0. More generally, the differential form, known as the , accounts for mass flow across boundaries: \frac{\partial \rho}{\partial t} + \nabla \cdot (\rho \mathbf{u}) = 0, where \rho is the mass density and \mathbf{u} is the velocity field, implying that local density changes are balanced by the net flux of mass. This formulation relies on key assumptions valid in classical contexts: non-relativistic speeds (where velocities are much less than the ), absence of nuclear reactions (which involve mass-energy conversion), and closed or isolated boundaries preventing external .

Historical Development

Early Observations and Precursors

The concept of mass conservation has roots in , where (c. 460–370 BCE) developed , positing that all consists of eternal, indestructible atoms that undergo rearrangement but never creation or destruction during natural changes. This view implied a fundamental constancy of , contrasting with earlier ideas of elemental transformation and providing an early intuitive precursor to quantitative preservation principles. During the medieval and early modern periods, alchemists from the 13th to 17th centuries documented puzzling mass discrepancies in experiments, such as the apparent weight gain of metals during when heated in air, which contradicted expectations of matter loss and remained unexplained within their qualitative frameworks. These observations, often recorded in treatises on metallic refinement and elixir production, highlighted inconsistencies in 's behavior without resolving them, as alchemists attributed changes to mystical principles like the rather than measurable constancy. In the mid-18th century, Russian polymath conducted unpublished experiments around 1748, sealing metals like lead in glass vessels and heating them to induce or reaction with air, consistently finding that the total mass before and after remained unchanged, thus demonstrating preservation in a controlled setting. Underpinning these empirical insights were philosophical developments in Cartesian mechanics, where (1596–1650) described matter as an immutable quantity of extension filling space, with its total "quantity of motion" (size times velocity) conserved by divine immutability across all interactions. This framework treated matter as inherently persistent, influencing later thinkers to view it as a conserved entity rather than subject to arbitrary alteration. These precursors collectively built toward more rigorous formulations in the late .

Formulation in Chemistry

In the 1770s, conducted pivotal experiments on and using sealed glass s to precisely measure changes. In 1774, he heated tin and lead in closed containers filled with air, observing that while the volume of air decreased and a () formed, the total of the and contents remained unchanged before and after the reaction. These results indicated that a constituent of the air, which Lavoisier later identified as oxygen (or "dephlogisticated air"), combined with the metal, rather than any substance being lost or gained from the system. Building on these findings, Lavoisier published his oxygen theory of combustion in 1777, proposing that burning involved the combination of substances with oxygen, a process that conserved mass overall. This directly challenged the prevailing , developed by in the early , which posited that combustible materials contained phlogiston—a hypothetical fire-like —released during or . Stahl's model struggled to explain the observed weight gain in calx formation, as it implied phlogiston had to account for the increase; Lavoisier resolved this by demonstrating that the gain resulted from oxygen absorption, aligning with quantitative mass measurements. Lavoisier's ideas culminated in his seminal 1789 work, Traité Élémentaire de Chimie, where he explicitly articulated the law of conservation of mass, stating that "in every operation an equal quantity of matter exists both before and after the operation." This text not only named and formalized the principle but also redefined chemical elements and rejected alchemical notions of . Earlier precursors, such as Mikhail Lomonosov's 18th-century observations on mass preservation in reactions, provided an independent demonstration without the widespread recognition or experimental rigor that Lavoisier later employed. The immediate impact of Lavoisier's formulation was profound, establishing precise as the standard for chemical investigations and eliminating concepts of or destruction in reactions. Chemists thereafter prioritized accurate weighing and closed-system experiments, fostering a shift toward empirical, reproducible that underpinned modern and reaction analysis.

Developments in Physics

In the , physicists integrated the conservation of into Newtonian , treating as an invariant property essential to the laws of motion. Newton's second law, F = ma, posits as constant for a given body, enabling derivations of momentum conservation in isolated systems, such as elastic collisions where total remains unchanged despite velocity alterations. This framework assumed no creation or destruction of , aligning with empirical observations in mechanical experiments and providing a foundation for analyzing dynamic systems without mass variability. Hermann von Helmholtz advanced this integration in his 1847 paper Über die Erhaltung der Kraft (On the Conservation of Force), which established across mechanical, thermal, and electrical domains while relying on constancy in processes like collisions and motion. Helmholtz demonstrated that force (energy) transformations preserve quantitative relations only if remains fixed, linking invariance to broader physical invariances in . John Dalton's 1808 reinforced mass conservation by modeling matter as composed of indestructible atoms that combine in fixed proportions, enabling the calculation of relative atomic weights from conserved total mass in combinations. This physical model explained why mass ratios in compounds remain constant, bridging atomic structure with Newtonian principles of invariance. During the 1850s, thermodynamic developments by and William Thomson (Lord Kelvin) affirmed mass constancy amid energy transformations and entropy considerations. Clausius's mechanical theory of heat treated mass as fixed in closed systems, ensuring that heat-to-work conversions obey conservation without mass alteration. Thomson's parallel work on entropy as a dissipative measure similarly presupposed unchanging mass, solidifying the principle in analyses of irreversible processes. By the late 1800s, Becquerel's 1896 discovery of in compounds hinted at potential exceptions to strict mass conservation, as salts emitted penetrating rays spontaneously without accounting for mass loss in classical terms, though these anomalies lacked resolution until subsequent atomic insights.

Applications

In Chemical Reactions

The principle of conservation of mass is fundamental to in chemical reactions, where balanced equations ensure that the total mass of reactants equals the total mass of products. For instance, in the formation of from and oxygen, the balanced equation is $2\mathrm{H_2} + \mathrm{O_2} \rightarrow 2\mathrm{H_2O} Using atomic masses of hydrogen (1 g/mol) and oxygen (16 g/mol), 4 g of hydrogen reacts with 32 g of oxygen to produce 36 g of water, demonstrating exact mass equality. This balancing process relies on the conservation law to maintain atomic proportions, allowing chemists to predict reaction outcomes quantitatively. In closed systems, where no matter enters or leaves, conservation of mass is directly observable, as in laboratory setups like sealed flasks for reactions. For example, burning magnesium in a sealed with oxygen yields , with the system's total mass remaining unchanged before and after the reaction. In contrast, open systems can create apparent violations; during rusting of iron in air, oxygen from the environment combines with the metal to form , increasing the mass of the but dispersing the added oxygen mass if not accounted for in a closed setup. Antoine Lavoisier's 18th-century experiments with sealed vessels first rigorously demonstrated this distinction in . The conservation principle underpins practical applications in chemistry, such as determining relative molecular weights through stoichiometric ratios and calculating reaction yields. In the 19th century, used mass conservation alongside the to assign relative atomic weights, forming the basis for modern tables; for example, analyzing compound formation ratios allowed him to propose hydrogen's weight as 1 relative to oxygen's 7 (later revised). Today, it enables by comparing actual product masses to theoretical yields from balanced equations, as in the reduction of with : the expected yield informs efficiency assessments in industrial processes. A common misconception arises in reactions producing gases, such as the baking soda and demonstration, where reacts with acetic acid to form , , and , leading some to believe has vanished as the solid "disappears" and fizzing occurs. However, in a closed like a sealed soda bottle, the total remains constant, with the gas contributing to the unchanged weight. This illustrates that is conserved across phases, countering the illusion of loss in open setups.

In Physical Processes

In physical processes, the principle of conservation of mass asserts that the total mass of a remains constant, even as undergoes changes in form, motion, or state without nuclear reactions. This invariance is fundamental to , , and , enabling predictive models for systems ranging from colliding objects to flowing fluids and phase transitions. Unlike , which may convert between forms, mass itself is neither created nor destroyed in these non-chemical contexts, providing a stable quantity for analysis. In mechanical interactions, such as elastic and inelastic collisions, the total mass of the involved bodies stays constant, allowing momentum conservation to rely on the unchanging product of mass and velocity. For example, in an elastic collision between two billiard balls of equal mass, the balls exchange velocities while the combined mass before and after impact remains identical, preserving the system's total momentum as m_1 \mathbf{v}_1 + m_2 \mathbf{v}_2 = m_1 \mathbf{v}_1' + m_2 \mathbf{v}_2', where primes denote post-collision values. In inelastic collisions, like a bullet embedding in a block, kinetic energy dissipates as heat or deformation, but the fused mass equals the initial sum, underscoring mass invariance as a prerequisite for momentum analysis in isolated systems. This principle, rooted in Newtonian mechanics, applies universally to macroscopic collisions where relativistic effects are negligible. Fluid dynamics exemplifies mass conservation through the , derived from the requirement that mass inflow equals outflow in a . For steady, incompressible flows—common in pipes or channels—the equation simplifies to \rho A v = \constant, where \rho is fluid , A is cross-sectional area, and v is . This relation ensures preserved ; for instance, in a constricted , velocity increases inversely with area to compensate, preventing mass accumulation. The general form, \frac{\partial \rho}{\partial t} + \nabla \cdot (\rho \mathbf{v}) = 0, extends to compressible and unsteady cases, forming the basis for Navier-Stokes equations in modeling phenomena like flows or systems. Thermodynamic processes uphold mass conservation during transfers and state changes, particularly in open systems where enters or exits. In transitions, such as at 0°C, the mass of solid precisely equals the mass of resulting liquid water, with absorbed without altering total mass. This equality holds because the process involves molecular rearrangement rather than matter addition or removal. In heat engines, like steam cycles, requires that the working 's inflow mass rate matches outflow, ensuring steady operation; for a , \dot{m}_{in} = \dot{m}_{out}, where \dot{m} is , preventing imbalances that could disrupt efficiency. Such balances are critical in analyzing cycles like the Rankine engine, where changes ( and ) occur without net mass loss. Engineering designs leverage conservation for reliability and efficiency in fluid transport and . In pipeline networks, the continuity principle dictates flow distribution to maintain pressure stability; for a junction, sum of incoming mass flows equals outgoing, modeled as \sum \rho A v = 0, guiding sizing of diameters to avoid surges in or systems. In classical rocket , treated as a variable- system, the rocket's initial (structure plus ) equals the final plus ejected exhaust , conserving total for the isolated rocket-exhaust . This underpins the , \Delta v = v_e \ln \left( \frac{m_0}{m_f} \right), where v_e is exhaust , m_0 initial , and m_f final , emphasizing as the driver of change without relativistic variation.

Modern Interpretations

Relativistic Framework

In the framework of , the classical notion of mass conservation is extended and modified by the principle of mass- equivalence, recognizing that mass is a concentrated form of . Albert Einstein's seminal 1905 paper, "Does the of a Body Depend Upon Its Content?", derived this relation through analysis of emission in different inertial frames, culminating in the equation E = mc^2, where E is the rest , m is the rest mass, and c is the in vacuum. This equivalence implies that isolated systems conserve total , including contributions from mass, rather than mass alone; any conversion between mass and other forms, such as kinetic or , preserves the overall invariant. Einstein employed thought experiments to illustrate this, such as a body at rest emitting two equal pulses of in opposite directions, resulting in a momentum balance but a net loss of energy L that reduces the body's mass by \Delta m = L / c^2. A concrete manifestation occurs in and processes where photons are emitted; for example, the release of in reactions like or leads to a measurable mass defect, where the total mass of the products is slightly less than the reactants, with the difference accounting for the emitted via E = \Delta m c^2. This mass decrease, though minuscule on atomic scales (e.g., about 0.1% in uranium ), underscores how energy emission directly alters rest mass. For closed systems in relativity, conservation is governed by the four-momentum vector p^\mu = (E/c, \mathbf{p}), where \mathbf{p} is three-momentum and the invariant mass is given by m = \sqrt{(E/c)^2 - p^2}/c; this four-vector is conserved in interactions, ensuring that rest mass can vary with internal energy configuration or velocity while total mass-energy remains frame-invariant. In relativistic mechanics, the effective or relativistic mass m_{\text{rel}} = \gamma m (with \gamma = 1/\sqrt{1 - v^2/c^2}) increases with speed, reflecting added kinetic energy, but modern formulations emphasize invariant rest mass, with variations arising from energy exchanges. Post-1905 experimental confirmations in particle accelerators have robustly validated these principles, observing direct mass-to-energy conversions such as (where gamma rays create electron-positron pairs) and (where particles convert to photons). A high-precision 2005 experiment at the Institut Laue-Langevin (ILL) and National Institute of Standards and Technology (NIST), measuring gamma-ray wavelengths from excited nuclei of silicon-28 and sulfur-32, verified E = mc^2 to within 0.0004% accuracy, aligning emitted energy precisely with predicted mass differences. Such results from accelerators like CERN's further demonstrate conservation through the routine creation of particles from collision energies exceeding rest masses.

Quantum and Particle Physics

In quantum field theory (QFT), the classical notion of mass conservation is superseded by the framework of fields and particles, where virtual particles—intermediate states in interactions—temporarily violate the on-shell condition E^2 = p^2 c^2 + m^2 c^4, allowing their effective masses to deviate from observed rest masses without contradicting overall energy-momentum conservation. These virtual particles, governed by the Heisenberg uncertainty principle, contribute to processes like vacuum fluctuations but do not lead to net mass creation or destruction; instead, conservation is enforced through global symmetries corresponding to quantum numbers such as B and L. For instance, in electron-positron annihilation, the rest masses of the and (m_e \approx 0.511 MeV/c^2 each) are fully converted into the energy of two or more photons, preserving total while the total rest mass becomes zero. A classic example of how quantum effects challenge apparent mass conservation arises in , where a (m_n \approx 939.57 MeV/c^2) decays into a proton (m_p \approx 938.27 MeV/c^2), , and antineutrino, resulting in a rest mass deficit of about 0.78 MeV/c^2 that manifests as of the products. This process initially appeared to violate due to the continuous energy spectrum observed in the , prompting in 1930 to hypothesize a massless, neutral "" to carry away the missing energy and , a proposal formalized by in 1934 as part of theory. The 's subsequent detection in 1956 confirmed that total energy-momentum is conserved, with the apparent mass change attributable to the creation of new particles rather than a loss of mass. Within the of , mass conservation applies strictly to stable particles but is relaxed for unstable ones through decays and interactions mediated by gauge bosons, where additional conserved quantum numbers like B and L prevent processes such as in . , assigned as B = 1/3 for quarks and thus B = 1 for baryons like protons and neutrons, remains conserved in all known strong, electromagnetic, and weak interactions, while (L = 1 for electrons and neutrinos, L = -1 for positrons and antineutrinos) similarly safeguards against unphysical flavor-changing processes. However, effects, such as processes at high temperatures, can violate B + L but conserve B - L, illustrating that mass-energy equivalence from integrates with these quantum symmetries to maintain overall balance. High-energy experiments at CERN's (LHC) further illuminate this by revealing that fundamental particle masses originate not from intrinsic properties but from couplings to the Higgs field, as evidenced by the 2012 discovery of the with mass m_H \approx 125 GeV/c^2. In proton-proton collisions reaching \sqrt{s} = 13 TeV, processes like Higgs production via fusion create new particles whose total rest mass exceeds that of the initial protons, yet holds through the field's (v \approx 246 GeV) that "breaks" electroweak symmetry and generates masses dynamically. ATLAS and detectors have measured Higgs decays, such as to bottom quarks or W/Z bosons, confirming that interaction rates align with predictions where rest mass is not conserved individually but emerges from field interactions, underscoring QFT's resolution of mass conservation at subatomic scales.

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