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A multiwire proportional chamber is a proportional counter: parallel anode wires between cathodes in a gas. Charged particle ionization frees electrons; an electric field drives them toward wires, triggering an electron avalanche read by electronic amplifiers.^[ref]

Georges Charpak's electronic readout avoided film scanning and full spark chamber discharge.^[ref]

Opposite polarities identify the avalanche wire. Positive ion motion dominates integrated signal; detection precedes complete collection. Calibrated electron travel times enable drift chambers.^[ref]

Ordinary solid sodium chloride has the rock salt structure. Choose a conventional cube of side $a$ with chlorine anions at the corners and face centers, and sodium cations at the edge centers and cube center. Corner sites are shared by eight cubes, face sites by two and edge sites by four. The unit cell counts are thereforeThere are four formula units per conventional unit cell, rather than four separate NaCl molecules.^[ref]

The Bravais lattice is a face-centered cubic lattice. One choice of primitive lattice translation vectors and atomic basis isThe determinant gives a primitive unit cell volume of $a^3/4$; that cell represents one cation and one anion. Four such volumes make the conventional cube. The union of all ion positions resembles a primitive cubic lattice of step $a/2$ only if the chemical labels are discarded: translation by $a(1,0,0)/2$ exchanges unlike ions and fails to preserve the chemical structure.

Each ion has six nearest unlike neighbors at distance $a/2$, along the positive and negative directions of the three cube axes. Thus the coordination number is six. Within either same-species face-centered cubic lattice, the nearest same-ion neighbors instead number twelve: their displacements are permutations of $(\pm a/2,\pm a/2,0)$, all of length $a/\sqrt{2}$. Since $a/\sqrt{2}>a/2$, those twelve are a more distant shell in the complete sodium chloride structure. The number twelve describes the same-ion FCC lattice neighborhood; six describes the nearest unlike-ion neighborhood.

The Nernst equilibrium potential is the inside-minus-outside membrane potential at which one ion species has equal electrochemical potential on both sides of a cell membrane. At uniform temperature $T$, using the same reference chemical potential on both sides, $z\ne 0$ is the signed ion charge number, $R$ the molar gas constant, $F$ the Faraday constant, and $a$ the dimensionless thermodynamic activity of that ion. For an ideal dilute chemical solution, the activity ratio becomes the concentration ratio. See Purves et al.: the forces that create membrane potentials and the Nernst equation.

The short derivation is to set the outside-to-inside electrochemical potential change from membrane transport to zero: $RT\ln (a_{\mathrm{inside}}/a_{\mathrm{outside}})+zFV=0$, and solve for $V$. An open pathway carrying only this species by passive transport then has this reversal potential. A balance of several nonzero ion electric currents does not establish this equilibrium condition for each species.

A net ionic equation retains the chemical species changed by a chemical reaction and cancels spectator ions present unchanged on both sides. Dissolved strong electrolytes are represented by their separated ions, while a solid product retains its chemical formula. Cancellation preserves both elemental inventories and electric charge conservation.^[ref]

For the calcium carbonate example, the complete ionic account isCanceling the sodium cations and chloride anions yields the net ionic equation above. Neither cancellation nor the conventional sodium chloride formula implies that the remaining dissolved ions have become paired molecules.

For this schematic, let $\xi$ be the amount of substance of AB formed. With no competing chemical reactions or losses,Adding each dissolved inventory to its contribution in the solid recovers its initial total. Each dissolved pair has net electric charge zero, so transferring a pair into neutral AB also preserves electric charge conservation. This is a short stoichiometry argument; choosing the actual $\xi$ additionally needs chemical equilibrium or chemical kinetics information.

The nitrate ion, ${\mathrm{NO}}_3^{-}$, is an anion with one nitrogen connected to three oxygen chemical atoms and net electric charge $-1$ in units of elementary charge. Its 24 valence electrons admit three equivalent octet resonance structures; see Lewis structure for their construction and chemical resonance for their interpretation. The N–O connections are covalent bonds within the ion. See 7.2 Covalent Bonding.

A nonelectrolyte supplies neutral molecules rather than ions on dissolving in the specified solvent, as illustrated by sucrose in water.

For example, dissolving an idealized $1\mathrm{mmol}$ sucrose inventory gives $1\mathrm{mmol}$ dissolved sucrose molecules, rather than separate cations and anions. Dissolving the same amount of substance of a fully dissociated one-to-one strong electrolyte instead gives $1\mathrm{mmol}$ of each ion. Both can disappear visibly into the solvent; the resulting chemical species distinguish them.^[ref]

A nonelectrolyte is not necessarily insoluble: sucrose provides a soluble counterexample. Nor does the label assert exactly zero measured electrical conductivity. Self-ionization of water, impurities or residual electrolyte from a probe can supply background ions. Comparing with a solvent blank and rinsing between samples, as in the strong electrolyte experiment, tests whether the dissolved substance itself produces appreciable additional mobile ions. This separates visible dissolution from ion production without treating lamp darkness as an absolute absence of electric charge.

Robert Andrews Millikan's 1911 protocol alternated electrically driven ascent with timed descent after short-circuiting the plates; a changed ascent speed signalled ion capture.^[ref]

His 1913 refinements checked voltage before and after runs, calibrated optical distance and the clock, compared independent air-dynamic viscosity measurements, and varied pressure to test slip.^[ref] His 1924 lecture describes suppressing convection, switching the electric field, neutralizing drops, and reproducing smallest observed electrical speed increments.^[ref]

Harvey Fletcher's posthumous account recalls building the first oil apparatus and measuring with Robert Andrews Millikan; priority for suggesting oil remains uncertain.^[ref]

To interpret the readout, keep one drop and one electric field polarity. Let $u_i$ be its signed upward terminal velocity in charge state $i$, and let $v_f>0$ be its field-off falling speed. Use the linear drag coefficient $k$ already defined in elementary charge, with any required gas slip correction to Stokes drag included. Provided the drop's radius, surrounding air and electric field remain fixed, its electrical speed increment isThese relations apply while the electric force points upward in every state. A drop may still descend, with $u_i<0$, when that force is too weak to support it. A held drop has $u_i=0$ and therefore $S_i=v_f$, rather than zero electrical response. A neutral drop has $S_i=0$: its signed terminal velocity agrees with field-off descent. Thus neither raw upward speed nor the ability to hold a drop is itself a count of electrons.

The ratios cancel a fixed $k/E$, even if its value is poorly known. This is why relative charge quantization and absolute measurement calibration are different questions. A changed field-off $v_f$ warns that evaporation, air motion or another change has spoiled comparison of charge states. A stable $v_f$ is useful evidence but cannot exclude every compensating change. Repeat field-off checks around a proposed jump, allow the terminal velocity under linear drag to settle after switching, and propagate measurement uncertainty in both the field-on and field-off readings. Reusing a single estimate of $v_f$ gives the different $S_i$ a shared covariance.

For propagation perpendicular to an equilibrium magnetic field, an ordinary plasma wave has its electric field parallel to that magnetic field, so the particle response involves no magnetic deflection. With immobile ions, the dispersion relation is ${\omega }^2={\omega }_{pe}^2+c^2{k}^2$. It is a transverse electromagnetic wave, despite its parallel particle motion.

In the dilute ideal particle-count description, osmolarity is the total amount of substance of independently dissolved solute particles per volume of chemical solution: $c_{\mathrm{osm}}={\sum }_j{n}_j/V$. It includes both membrane-permeating and retained solutes; specifying a particular membrane is unnecessary to count particles. A neutral undissociated solute contributes one particle per molecule, whereas separated ions are counted individually. Common units are $\mathrm{osmol}{\mathrm{L}}^{-1}$ or $\mathrm{mOsm}{\mathrm{L}}^{-1}$, with one osmole denoting one mole of the counted particles. Osmolality uses mass of solvent instead of volume of chemical solution; the two numerical values should not be identified without the appropriate mass-to-volume conversion.^[ref]

This ideal counting definition states its scope: interactions can require a thermodynamic activity description of osmotic pressure. Tonicity asks a different question, namely how that surrounding chemical solution changes a specified biological cell's volume through its particular cell membrane.

Osmotic pressure is the excess pressure needed on a chemical solution to maintain osmotic thermodynamic equilibrium with pure solvent across a semipermeable membrane. For a nearly incompressible solvent, equality of chemical potential gives $\Pi \simeq -(RT/{\bar{V}}_w)\ln a_w$. It is an equilibrium property; an observed initial swelling rate is a different measurement.^[ref]

For a dilute ideal chemical solution of retained particles,Here $n$ is the amount of substance of independently dissolved solute particles, measured in moles; $V$ is the final volume of chemical solution, not the starting volume of pure solvent. Count the resulting ions separately if a solute dissociates; do not multiply twice if $n$ already counts them. With $c_{\mathrm{osm}}$ in $\mathrm{mol}{\mathrm{m}}^{-3}$ and $R$ in $\mathrm{J}\mathrm{mo}{\mathrm{l}}^{-1}{\mathrm{K}}^{-1}$, $RT{c}_{\mathrm{osm}}$ has units $\mathrm{J}{\mathrm{m}}^{-3}=\mathrm{Pa}$. This resembles the ideal gas law, although the particles here are dissolved in a liquid.

The assumptions are uniform temperature, a dilute ideal chemical solution, a nearly incompressible solvent, and a semipermeable membrane that retains the counted solutes while passing solvent. Association, incomplete dissociation and interactions change the relation between added material and independent particles; nonideal thermodynamic activities invalidate simple particle counting. The formula does not describe a concentrated brine merely because the apparatus contains a membrane.

A short derivation explains why particles are counted. In an ideal mixture, $a_w=x_w=n_w/(n_w+n)$, with $n_w$ the amount of substance of water. If $n\ll n_w$, then $-\ln x_w=\ln (1+n/n_w)\simeq n/n_w$ and $V\simeq n_w{\bar{V}}_w$. Substitution gives $\Pi \simeq RTn/V$. This is a dilute-limit approximation, not a claim that water molecules stop moving or that dissolved particles are a gas.

An oxidation state is an electron-bookkeeping assignment to a chemical atom: its electric charge number after the ionic approximation of bonds. It helps identify oxidation and reduction and determine stoichiometry, even for covalent bonds without separate charged ions. In water, each hydrogen has oxidation state $+1$ and oxygen has $-2$; this does not assert that a water molecule contains two free protons and a free oxide ion.^[ref]

Three conventions answer different questions. Formal charge divides each bonding electron pair equally in a chosen Lewis structure. Oxidation state uses the ionic approximation of bonds. Partial atomic charge instead partitions the actual electron density and depends on that partition. In the ordinary water Lewis structure, every formal charge is zero although the oxidation states are not. Neither bookkeeping convention supplies numerical partial atomic charges.

Sum oxidation states over all chemical atoms of the specified molecule, ion or formula unit, including multiplicities:Here $q$ is the net electric charge and $e$ the positive elementary charge. For a neutral entity the sum is zero; for an ion it equals its signed electric charge number $z$. The reason is simple: the allocation assigns every valence electron exactly once, so the sum is the neutral electron budget minus the actual electron count.

For water, $2(+1)+(-2)=0$; for hydrogen peroxide, $2(+1)+2(-1)=0$. In permanganate, ${\mathrm{MnO}}_4^{-}$, assigning each oxygen $-2$ gives $x+4(-2)=-1$, so manganese has oxidation state $+7$. This is not a free ${\mathrm{Mn}}^{7+}$ ion: the entire permanganate anion has net electric charge $-e$. The sum rule supplies a constraint; without additional assignments it cannot determine every individual oxidation state.

An unoccupied oxygen site in a reference crystal structure. Removing an oxide ion gives an effective charge $+2e$ relative to the perfect lattice; the charge of the actual missing ion is $-2e$. A physical sample must satisfy overall charge neutrality through other defects, electronic carriers or changed cation valences.

A particle detector converts an interaction involving a particle into a readable signal. A cloud chamber is a particularly direct example: tiny liquid drops turn an invisible ion trail into a photographable line.

Passive transport is net movement down the transported substance's electrochemical gradient without coupling that movement to another source of free energy. Facilitated diffusion is passive transport through an ion channel or a passive carrier protein. Providing such a route can speed passage, but does not turn an uphill transfer into a downhill one. For an uncharged solute under the ideal conditions above, net passive transport runs from higher to lower concentration; for an ion, the membrane potential also matters. See Cooper, The Cell: transport of small molecules.

In the figure, stipulate eight neutral solute tracers in A and two in B, with equal fixed volumes, identical surroundings, and no imposed electric potential difference. The concentration ratio is $c_{\mathrm{A}}/c_{\mathrm{B}}=8/2=4$, so A-to-B transfer has $\Delta \tilde{\mu }=-RT\ln 4\simeq -1.38629RT$, or $-3.458\mathrm{kJ}\mathrm{mo}{\mathrm{l}}^{-1}$ at the assumed temperature $T=300\mathrm{K}$. If this solute can cross, thermodynamic equilibrium has equal expected concentrations: five tracers per side on average. Individual crossings occur in both directions; an observed ten-particle snapshot need not contain exactly five on each side. These stipulated counts illustrate a driving force, not a measured flow rate or a prediction of the time to equilibrate.

For a separate illustrative ion calculation, keep $c_{\mathrm{A}}/c_{\mathrm{B}}=4$, but assign $z=+1$ and $V_{\mathrm{A}}-V_{\mathrm{B}}=-60\mathrm{mV}$ at $300\mathrm{K}$. Using $R\simeq 8.31446\mathrm{J}\mathrm{mo}{\mathrm{l}}^{-1}{\mathrm{K}}^{-1}$ and $F\simeq 96485.33\mathrm{C}\mathrm{mo}{\mathrm{l}}^{-1}$, B-to-A transfer gives $RT\ln 4-0.060F\simeq 3.458-5.789=-2.331\mathrm{kJ}\mathrm{mo}{\mathrm{l}}^{-1}$. Thus an appropriate open ion channel can permit passive transport toward the higher concentration: the electrical contribution outweighs the opposing chemical potential contribution. This stipulated membrane potential is not inferred from the tracer counts.

Lipid diversity allows a membrane to remain a selective, mechanically coherent barrier while retaining the molecular mobility required for function. Stability and fluidity are different properties: a lipid bilayer can be well ordered yet permit rapid lateral diffusion, or be mobile yet leaky and vulnerable to rupture. The effects depend on composition, temperature, leaflet organization and interactions among components rather than on one universal ranking of “rigid” and “fluid” lipids.

The basic stability comes from amphiphilic organization. Hydrophobic chains avoid exposure to water, while polar headgroups remain hydrated. A pore exposing chains has an energetic cost, encouraging local defects to close, but stress, chain disorder or incompatible molecular shapes can make defects easier to form. Useful measurements therefore include membrane permeability, leakage and mechanical failure as well as rotational mobility, lateral diffusion and acyl-chain order. Calling all of these “fluidity” conceals distinctions relevant to cell survival.

Acyl-chain length changes the contact area between neighboring chains. Other things equal, longer chains generally strengthen attractive contacts, increase bilayer thickness and raise the tendency to form an ordered phase. Shorter chains tend to lower the chain-melting transition and can increase permeability. A double bond between carbon atoms in the cis configuration restricts the chain geometry and disrupts close packing, generally lowering the chain-melting temperature relative to a comparable saturated chain. A double bond in the trans configuration has a different geometry and commonly permits closer packing than the corresponding cis configuration. Branching also changes packing. These comparisons hold the headgroup and other variables fixed; they are not predictions that all unsaturated lipids behave identically in a complex mixture.

An immediate consequence is that composition has to be interpreted relative to the growth temperature. A membrane made mostly of long saturated chains can become too ordered on cooling, slowing membrane protein conformational changes and molecular redistribution. Greater unsaturation can preserve mobility. On heating, the converse adjustments can limit excessive disorder and leakage. The original homeoviscous adaptation experiments found temperature-dependent changes in the saturated and long-chain fatty acid content of Escherichia coli, using spin-label electron paramagnetic resonance to compare membrane-lipid viscosity at the cells' growth temperatures.^[ref] This establishes an adaptive relationship rather than a claim that every organism maintains a single invariant value by the same biosynthetic route.

Headgroup diversity changes both local interactions and preferred geometry. Phosphatidylcholine is approximately cylindrical in many common bilayer compositions, whereas phosphatidylethanolamine has a smaller headgroup relative to its chains and can favor negative monolayer spontaneous curvature. A single-chain lysophospholipid often favors curvature of the opposite sign. Mixing these shapes can support bending and membrane-fusion intermediates, while too much of a nonbilayer-forming component can destabilize a planar lipid bilayer. The amphiphile packing parameter is a useful qualitative guide, but hydrated headgroup size and chain volume depend on conditions; a molecular cartoon does not supply a quantitative phase diagram.

Headgroup charge adds another control. phosphatidylserine and phosphatidylinositol 4,5-bisphosphate contribute negative inner-leaflet charge, recruiting basic membrane-binding regions of proteins and changing local electrostatics. Ionic strength, pH and divalent ions can screen, alter or bridge those charges. A lipid-induced change in domain organization could therefore arise from ion-mediated interactions rather than acyl-chain order alone. Sphingomyelin can pack tightly through its chain structure and headgroup/backbone interactions, influencing thickness and local order. A comparison of headgroups must specify the attached chains, because changing a headgroup while simultaneously changing chain saturation confounds the interpretation.

Cholesterol is particularly effective because its small polar head and rigid ring system fit between phospholipid chains. In a relatively disordered bilayer, it often increases chain order, condenses packing and reduces permeability to small solutes. In a tendency toward a tightly packed gel, it can disrupt regular packing and inhibit the cooperative freezing transition. Thus “cholesterol decreases fluidity” is incomplete: it can reduce some local motions while preventing an immobile gel and retaining lateral mobility. Its effects depend on concentration, temperature and the surrounding lipids; excessive amounts can exceed the mixture's capacity to accommodate it.

Mixtures of saturated lipids, unsaturated lipids and cholesterol can form coexisting liquid-ordered phase and liquid-disordered phase. The former combines greater acyl-chain order with lateral mobility; it is distinct from a solid gel. fluorescence microscopy of defined giant lipid vesicles directly demonstrated domains and mapped composition- and temperature-dependent coexistence.^[ref] The result proves that lipid interactions can organize a membrane without a protein scaffold. It does not establish that living plasma membranes contain large equilibrium domains of the same sizes. Cellular crowding, cytoskeleton coupling, asymmetry, trafficking and active turnover can change or suppress those patterns.

Diversity also works across the membrane. The outer and inner membrane leaflets differ in headgroups and chain distributions; equal total composition does not imply equal surface properties. Lipidomic and packing measurements found greater unsaturation and looser packing in the cytoplasmic leaflet of the examined mammalian plasma membranes.^[ref] Such asymmetry can couple to membrane protein shape and binding preferences. flippases and scramblases change transverse lipid distribution; because spontaneous translocation of many polar phospholipids is slow, this organization can be maintained and regulated. Leaflet imbalance creates curvature stress, but the result depends on lipid exchange and mechanical constraints rather than on headgroup charge alone.

Membrane composition also sets the energetic cost of deforming the surface around a membrane protein. Longer ordered chains may increase thickness and stiffness; mismatch with a transmembrane protein's hydrophobic span can favor local deformation, changed association or altered activity. Curvature-preferring lipids can lower the cost of particular conformational or membrane-shape transitions. Greater mechanical stiffness can resist bending but need not mean a larger rupture threshold. Oxidation of polyunsaturated chains can change molecular geometry and produce defects or reactive breakdown products, making chemical stability another tradeoff alongside mobility. Appropriate experiments should measure oxidation state and leakage rather than infer stability from saturation alone.

A good causal experiment uses compositionally defined lipid vesicles, independently varying chain saturation, chain length, headgroup and cholesterol. Keep vesicle size, temperature, ionic strength and osmotic conditions controlled. differential scanning calorimetry identifies cooperative transitions; spin-label electron paramagnetic resonance or calibrated fluorescence anisotropy probes local order and rotational freedom; fluorescence recovery after photobleaching measures lateral redistribution. Recovery also depends on geometry, immobile fractions and probe partitioning, so distinguish these from the diffusion coefficient. Test barrier stability by entrapped-dye leakage with dye-quenching and complete-release controls, and mechanical behavior with defined membrane-tension measurements. Repeat key comparisons with different probes because a probe can partition preferentially into one phase. In living biological cells, combine lipidomics with targeted biosynthetic perturbation, rescue and viability measurements to separate compositional effects from secondary stress responses.

Lipid diversity stabilizes useful combinations of properties: a sealed barrier, adaptable curvature, controlled local order and sufficient mobility. It also allows different compartments and leaflets to satisfy different physical demands; no single lipid composition maximizes all of those properties simultaneously.

Write $e=q>0$ for the elementary charge and $ϵ={ϵ}_0{ϵ}_r$ for the permittivity. Taking the bulk electric potential as zero, the Boltzmann distribution of point ions gives $c_i(x)=c_i^{\infty }\exp [-e{z}_i\varphi (x)/(k_{B}T)]$. Here $c_i$ is a number density, not a molar concentration. Combining this with Poisson's equation gives the planar Poisson-Boltzmann equationMultiplying by ${\varphi }^{\prime }$ and integrating from the neutral bulk, where $\varphi ={\varphi }^{\prime }=0$, yieldsFor the solution occupying $x>0$, with the field on the other side neglected, Gauss's law gives $\sigma =-ϵ{\varphi }^{\prime }(0)$. On the branch that decays to zero without crossing it,Source sign qualification: the unsigned square root printed in the paper gives $|\sigma |$. A negative wall electric potential, such as the next part's $-73\mathrm{mV}$, has ${\varphi }^{\prime }(0)>0$ and hence $\sigma <0$, providing a concrete counterexample to interpreting that printed expression as signed surface charge density. This is the planar Grahame equation, with an explicit sign convention.

Including both flat ends of the cylindrical cell, its membrane surface area isThe capacitance is $C=(0.01\mathrm{F}{\mathrm{m}}^{-2})A=6.34602\mathrm{pF}$. The electric charge needed for the specified depolarization is thereforeIgnoring the ends gives $3.33\times 10^6$, only about one percent smaller. Inward movement of positive ions, or outward movement of negative ions, produces the stated positive change in the inside-minus-outside membrane potential.

The cell volume is $\pi r^2\ell =3.14159\times 10^{-16}{\mathrm{m}}^3$. Distributed over this volume, the transferred number would correspond to only $0.0177955\mathrm{mM}$. Relative to an illustrative, not source-specified, $100\mathrm{mM}$ internal ionic pool, that is a fraction $1.78\times 10^{-4}$. Thus a substantial change in membrane potential requires movement of only a tiny fraction of bulk ions; it does not require wholesale depletion of the intracellular solution. The separated electric charge is concentrated near the two membrane surfaces.

An ion channel is a selective permeation pathway, not simply an aqueous hole of fixed diameter. A hydrated ion entering a narrow selectivity filter must lose or reorganize some hydration water. The energetic cost can be offset by interactions with charged or polar groups in the pore. Different ionic radii, valences, hydration free energies, and coordination geometries therefore produce different permeation barriers and binding affinities.

A classical potassium selectivity filter presents oxygen ligands that stabilize relatively dehydrated potassium in configurations resembling its aqueous coordination. Smaller sodium does not automatically pass more easily: its hydration is stronger and the filter need not provide a compensating configuration at equally low free energy. Filter flexibility and multi-ion occupancy matter, so the explanation is an energetic balance, not the assertion that a rigid hole simply blocks every larger or smaller sphere. Ion-ion interactions and coupled displacement can permit rapid conduction while maintaining selectivity.^[ref]

Other ion channels use different arrangements. Fixed negative groups can strongly favor divalent calcium over monovalent ions; occupancy and competition then influence both selectivity and throughput. Selectivity is distinct from activation or ion-channel inactivation, which control access or availability. Selective passive flux follows an electrochemical potential gradient; it does not by itself pump ions uphill. Selectivity allows cells to establish particular membrane potentials, generate action potentials, regulate calcium signals, and control solute balance without dissipating every ionic gradient whenever one pathway opens.

Treat the membrane as a capacitor, and count the additional positive charge on its inner surface. With radius $r=10^{-6}$ m and length $\ell =10^{-4}$ m, including both end caps givesThe membrane capacitance is $C=C_{m}A=6.3460$ pF. Thus $\Delta Q=C\Delta V=5.3941\times 10^{-13}$ C, corresponding to $\Delta N=\Delta Q/e=3.3667\times 10^6$ monovalent sodium ions. Converting charge to amount of substance using the Faraday constant,Omitting the ends changes the answer to $0.01762$ mM, a one-percent correction. A large membrane potential change therefore requires only about $0.12\%$ of the intracellular sodium population to enter. The bulk liquid remains nearly electrically neutral; excess charge resides chiefly near the cell membrane. This explains why an action potential need not exhaust the concentration difference that drives it, and why fixed reversal potentials are a useful approximation during one spike. This membrane capacitive ion budget assumes sodium supplies the minimum net charging requirement. Simultaneous opposing electric currents can require more sodium entry; repeated spikes eventually require the sodium-potassium ATPase to maintain the gradients.