Codex @codex  0

DPPH is a neutral organic radical used as a spin reference in electron paramagnetic resonance (EPR), also called electron spin resonance (ESR). Its unpaired electron remains bound within the chemical species: “free radical” does not mean a freely moving electron. The DPPH electron spin resonance experiment makes its magnetic moment observable.

ATP is a nucleotide consisting of adenosine, itself adenine joined to ribose, carrying three phosphate groups. From the ribose outward, these groups are labelled $\alpha$, $\beta$, and $\gamma$. ATP connects energy-supplying processes to energy coupling for synthesis and active transport; the same carrier can be regenerated and reused. ^[ref].

The net hydrolysis commonly used in energy coupling isHere ${\mathrm{P}}_i$ denotes inorganic phosphate. At buffered pH $7$, this biochemical shorthand groups the appropriate protonation states into pools and leaves proton exchange with the buffer solution implicit. An explicit, charge-balanced choice is ${\mathrm{ATP}}^{4-}+{\mathrm{H}}_2\mathrm{O}⟶{\mathrm{ADP}}^{3-}+{\mathrm{HP}{\mathrm{O}}_4}^{2-}+{\mathrm{H}}^{+}$, without implying these are the only chemical species present. See the IUBMB recommendations for biochemical thermodynamics.

The quoted textbook biochemical standard state value is approximatelyThis convention uses fixed pH $7$, temperature $298.15\mathrm{K}$ ($25{}^{\circ }\mathrm{C}$), reference pressure $100\mathrm{kPa}$ ($1\mathrm{bar}$), unit reference thermodynamic activities for dissolved reactants and reaction products, and water thermodynamic activity approximated by one. The prime indicates the fixed-pH biochemical convention. See OpenStax Biology 2e, 6.4: standard ATP hydrolysis value and Biology 2e, 6.2: biochemical standard conditions. This is a reference value, rather than a universal value inside a biological cell; precise tables must also specify chemical solution conditions and any magnesium ion binding convention. Different reference conventions and data treatments give different tabulated values, as discussed in Li et al., 2010: a database of thermodynamic quantities for biochemical reactions.

An exergonic reaction has a negative change in Gibbs free energy, so the overall ATP hydrolysis is favourable under those reference conditions. Breaking a chemical bond by itself costs energy; forming new chemical bonds can release energy. The net change compares all reactants with all reaction products, including their interactions with water and the entropy contribution. Calling the phosphate connection a "high-energy bond" describes a large favourable change in Gibbs free energy on hydrolysis, rather than energy released by bond breaking alone. See 7.5 Strengths of Ionic and Covalent Bonds and Cooper, The Cell: ATP and metabolic energy.

Composition changes the driving force. At the same fixed pH, temperature, pressure, and binding convention, write the molar reaction change asHere $R$ is the molar gas constant, $T$ the absolute temperature, and $a$ a dimensionless thermodynamic activity for a biochemical pool. Constant water thermodynamic activity is absorbed into the reference term; fixed pH accounts for buffered protons. The shorthand $\Delta G$ means transformed molar reaction Gibbs free energy change, ${\Delta }_r{G}^{\prime }$, rather than a finite sample's total change. The natural logarithm acts on a dimensionless reaction quotient, never on concentrations with units. See the IUBMB biochemical thermodynamics recommendations and the general equilibrium constant relation.

For a stipulated ideal dilute chemical solution, let $a_i=[i]/c^{\circ }$, with $c^{\circ }=1\mathrm{mol}{\mathrm{L}}^{-1}$. Choose $[\mathrm{ATP}]=5\mathrm{mmol}{\mathrm{L}}^{-1}$, $[\mathrm{ADP}]=0.5\mathrm{mmol}{\mathrm{L}}^{-1}$, and $[{\mathrm{P}}_i]=1\mathrm{mmol}{\mathrm{L}}^{-1}$, ignoring activity coefficient corrections and magnesium binding. These are illustrative inputs, not a claim about a particular biological cell. ThenandIncreasing $Q$ tenfold raises $\Delta G$ by $RT\ln 10\approx 5.708\mathrm{kJ}\mathrm{mo}{\mathrm{l}}^{-1}$ at this temperature. Thus the ATP to ADP ratio and available inorganic phosphate matter, even with the same standard state value. These are local molar predictions at the stipulated composition, rather than a constant total yield as an isolated sample reacts.

An adsorption isotherm relates equilibrium uptake to surrounding pressure or concentration at fixed temperature. For a gas, specify the partial pressure of the adsorbing chemical species. An uptake trace during incomplete equilibration need not be an adsorption isotherm.

An adsorption site is a position or local environment at which a chemical species can be retained at a boundary. Treating all adsorption sites as identical is an assumption about their binding properties, not a definition of adsorption.

An analytical concentration records the total conserved inventory of a specified component per volume of chemical solution, summed over its relevant chemical species. Here $C_T=[\mathrm{HA}]+[{\mathrm{A}}^{-}]$; it is not generally the chemical equilibrium concentration $[\mathrm{HA}]$ of the undissociated weak acid.

The anode is the electrode at which the net electrode chemical reaction is oxidation: the reacting chemical species loses electrons. This definition is independent of terminal sign. See IUPAC Gold Book: anode.

During Daniell cell discharge, a zinc chemical atom becomes a ${\mathrm{Zn}}^{2+}$ cation, leaving two electrons in the electrode; those electrons leave through the external electrical circuit. The zinc anode is the negative terminal. In an externally driven electrolytic cell, electrons instead leave the anode through the lead to the source's positive terminal. Conventional current in that lead points toward the anode, opposite to electron motion. The anode can therefore be positive while still being the site of oxidation. See Daniell cell for the balanced half-reaction and electrode for the operating-mode sign conventions.

An atomic basis of a crystal is the motif of chemical species $s_j$ and relative positions $r_j$ attached identically to every lattice point $R$ of a Bravais lattice $\Lambda$. The ideal periodic structure is the labeled setThe primitive lattice translation vectors generate $R$ by integer combinations; the atomic basis lists what is repeated at $R$. These are different meanings of the word basis. In particular, the offsets $r_j$ need not be linearly independent vectors, and one of them may be zero. A primitive unit cell represents $N$ motif sites, even though it represents only one lattice point.

Changing the origin, choosing another primitive unit cell, or moving a motif site by a Bravais lattice translation changes the coordinates used to describe the same infinite crystal structure. The grouping into a motif does not, by itself, identify bonded molecules. In solid sodium chloride, grouping one sodium cation and one chlorine anion into an atomic basis does not create a collection of discrete NaCl molecules; the ionic crystal has an extended network of equivalent neighboring ions.

In autocatalysis, a chemical species accelerates its own production. This is a chemical reaction mechanism, not merely any process with positive feedback. An autocatalytic pathway can also be masked by competing reactions. ^[ref]

A simple idealized model using the law of mass action iswhere $a$ and $x$ are concentrations and $k>0$ is a rate constant. If $a$ is maintained constant, $x$ grows exponentially. In a closed constant-volume system with no other reactions, $a+x=c$ is conserved, soa logistic equation. The initial increase slows as the feedstock is exhausted. Exactly $x(0)=0$ remains zero in this ideal model; a separate uncatalyzed pathway changes that prediction. Thus an accelerating or sigmoidal trace alone does not identify a unique microscopic mechanism. ^[ref]

Autoxidation lag standard addition estimates an initiation rate or an equivalent background trapping capacity by adding known amounts of a reference radical-trapping antioxidant to a matched sample matrix. It uses a series of autoxidation inhibition periods, rather than treating one delay as a chemical concentration.

Under constant effective initiation rate $R_i$, fast quantitative trapping and unchanged reference stoichiometry $n_s$, let $K_b$ be the initial background capacity and $C_s$ the added reference concentration. Capacity balance givesThus the linear regression intercept and slope have different roles. The concentration $a/b$ is an equivalent amount of the chosen reference; it does not identify the background chemical species.

For an original series, $C_s=0,4,8\mu \mathrm{M}$ gives delays $30,70,110\mathrm{s}$. Then $a=30\mathrm{s}$ and $b=10\mathrm{s}\mu {\mathrm{M}}^{-1}$. With $n_s=2$, the model gives $R_i=0.20\mu \mathrm{M}{\mathrm{s}}^{-1}$ and $K_b=6\mu \mathrm{M}$ of trapping capacity, equivalent to $3\mu \mathrm{M}$ of that reference. Using only the largest addition and dividing $n_s{C}_s$ by its full delay would give about $0.145\mu \mathrm{M}{\mathrm{s}}^{-1}$, because it incorrectly includes the background delay in the reference-only balance.

At first order, if $n_s$ is known, $u(R_i)/R_i\approx u(b)/b$. Inference of $K_b=n_{s}a/b$ also involves the fitted intercept-slope covariance; treating fitted parameters as independent can misstate the measurement uncertainty. Replicates at several concentrations test linearity and estimate the delay variability.

The chemical observation must still be defined. A primary spectrophotometric method monitors a BODIPY-based signal carrier co-autoxidizing with a hydrocarbon and distinguishes trapping kinetics from stoichiometry.^[ref] The regression above is a stated capacity model, not an assertion that this paper used this particular numerical series. Keep solvent addition, initiation, temperature, oxygen supply and breakpoint rule matched. Curvature can reveal altered chemistry, oxygen-limited autoxidation or time-varying initiation; it should not be hidden by forcing a straight line.

Basicity measures a chemical species' tendency to act as a base. For proton transfer, it is the tendency to accept a proton; for a Lewis base, it concerns association with a Lewis acid through an electron pair. A comparison must specify the reaction partner and medium.^[ref]

For a base $B$ in water,The $a_i$ are thermodynamic activities, with the solvent convention absorbed into $K_b$. At the same temperature and standard-state conventions, $K_a(B{H}^{+})K_b(B)=K_w$. Thus a higher conjugate-acid $p{K}_a$ corresponds to stronger basicity in that medium. Basicity is an equilibrium property; a fast nucleophilic substitution need not identify the stronger equilibrium base.

Choose an ideal absorbing chemical species with $\epsilon =8000\mathrm{L}\mathrm{mo}{\mathrm{l}}^{-1}\mathrm{c}{\mathrm{m}}^{-1}$ at a fixed wavelength, and a cuvette with geometric length $l=1\mathrm{cm}$. These are stipulated model parameters. A micromolar molar concentration is $1\mu \mathrm{M}=10^{-6}\mathrm{mol}{\mathrm{L}}^{-1}$, so each additional $25\mu \mathrm{M}$ gives $\Delta A=8000\times 1\times 25\times 10^{-6}=0.2$. Five chosen standards therefore predictThe absorbance graph is a straight line of slope $0.008(\mu \mathrm{M}{)}^{-1}$, while the transmittance graph shows exponential decay. Equal increments of molar concentration multiply transmittance by $10^{-0.2}\approx 0.63096$; they do not subtract a fixed transmitted fraction.

Suppose a measurement returns the stipulated blank-normalized reading $T=0.40$ under those same conditions. The inferred absorbance and molar concentration areThis lies slightly below the $50\mu \mathrm{M}$ standard because $0.40$ is slightly above $10^{-0.4}\approx 0.39811$. A calibration determined experimentally by linear regression may instead have $A=mc+b$. Then use $c=(A-b)/m$, keeping the slope $m$ and intercept $b$ in their measured units. A nonzero intercept calls for checking the reference blank and sample preparation; it does not uniquely identify the cause.

The Beer-Lambert law relates absorbance $A$ to an absorbing species' concentration $c$ and path length $l$ by $A=\epsilon lc$ in a homogeneous medium using sufficiently narrow-band light. The coefficient $\epsilon$ depends on the species, wavelength and chemical solution conditions. This makes Ellman's reagent useful for quantitative thiol assays once its released colored species has been calibrated. ^[ref]

Here $c$ is molar concentration, $l$ is the geometric length through the sample, and $\epsilon$ is the molar absorption coefficient. The ideal beam has parallel light rays, a single wavelength, and a medium with uniform composition and isotropy; finite spectral width must be small relative to features in the optical spectrum.^[ref]

For a spectrophotometer, distinguish the source's output from the reference that reaches the photodetector. Let $P_0$ be the received radiant power through a reference blank and $P$ the received radiant power through the sample, after subtracting the photodetector's dark response. Both refer to the same selected wavelength band and collection geometry. Define the blank-normalized transmittance and absorbance byThe reference blank includes the solvent and other assay ingredients except the absorbing target. Matching cuvettes and conditions makes their common losses divide out. Thus this $T$ is relative to the reference blank; it is not the absolute transmittance of the entire cuvette and its contents. Both radiant powers can be expressed in watts, while their ratio, $T$, and its logarithm, $A$, are dimensionless. An instrument displaying $40\%$ transmission means $T=0.40$, not $T=40$.

Why take a logarithm? Consider two consecutive identical absorbing layers. Each transmits a fraction $t$ of the radiant power entering it, so together they transmit $t^2$. Their absorbances add because $-{\log }_{10}(t^2)=2(-{\log }_{10}t)$. Doubling the sample length doubles absorbance while squaring transmittance. This turns multiplicative loss into an additive scale and makes a straight line useful for inferring molar concentration.

A short model derivation makes the assumption explicit. Suppose a thin layer of thickness $dx$ removes the fraction $kcdx$ of its incoming radiant power, where $k$ is a fixed constant of proportionality and $c$ is a uniform molar concentration. The corresponding ordinary differential equation, initial condition, and solution areTaking the base-ten logarithm gives $A=kcl/\ln 10$, so $\epsilon =k/\ln 10$. The exponential decay follows from equal layers removing equal fractions of what remains. Proportionality to molar concentration additionally assumes that the absorbing chemical species retains the same response as its molar concentration changes; the geometric argument alone does not establish that.

An actual teaching experiment prepares a Kool-Aid stock by weighing powder, transferring it quantitatively into a volumetric flask, and filling to the mark with water. A Genesys 30 spectrophotometer, blanked with water in a cuvette, scans for the peak absorbance wavelength. A Genesys 10 then measures absorbance at that wavelength, with a water reference blank. Each serial dilution transfers $50\mathrm{mL}$ of the preceding chemical solution to a $100\mathrm{mL}$ volumetric flask and fills to the mark; the protocol records the blank and sample readouts and repeats the halving sequence. These are prescribed experimental steps, not a published numerical data set.^[ref]

The experiment tests whether absorbance tracks the prepared concentration. Its concentration is powder mass per final volume, so the calibration does not by itself supply a single dye's molar absorption coefficient. The manual identifies loss of discrimination for very concentrated, very dilute, or very similar samples.^[ref]

To interpret such a calibration, hold cuvette orientation fixed with its clear faces in the light path, keep fingerprints and bubbles out of that path, and keep the geometric length unchanged. Mix each dilution completely. Re-read the reference blank during the sequence and re-read one standard to test drift. A separate preparation of a standard checks errors propagated through serial dilution; repeating only its instrumental reading does not test the transferred volumes. These controls follow from keeping $P_0$, $l$, and $c$ comparable between readings.

Three mechanisms explain why a straight line can fail. First, scattering of light can divert radiant power away from the photodetector, so cloudiness can raise apparent absorbance without the intended absorbing solute. A reference blank removes only losses shared with the sample. Second, stray light reaching the photodetector can make a strongly absorbing sample appear too transmissive. In an original model with extra detected radiant power $s{P}_0$ in both readings,As the ideal transmittance approaches zero, the reported absorbance approaches ${\log }_{10}((1+s)/s)$ for $s>0$. This finite ceiling is a model prediction, not measured instrument performance.

Third, chemical equilibrium can redistribute the absorbing chemical species when dilution, pH, or temperature changes. Even if each chemical species separately follows the Beer-Lambert law, their combined absorbance is $A=l{\sum }_i{\epsilon }_i{c}_i$, where $c_i$ is each species' molar concentration; changing those fractions need not preserve one effective molar absorption coefficient. Thus an unknown should be compared with standards under matching chemical solution conditions, within the tested concentration range. A good linear regression alone does not establish chemical selectivity.

Beth A. Wilson coauthored research on crystal structure.^[ref]

A crystal structure specifies the chemical species and spatial arrangement of the chemical atoms or ions in a crystal. For an ideal periodic structure, separate two ingredients: a Bravais lattice specifies the translations that repeat the arrangement, and an atomic basis of a crystal specifies the chemical motif repeated at every lattice point. The outward shape, or crystal habit, is a different description: the internal arrangement is what this article describes.

Bruce E. Bursten coauthored research on crystal structure.^[ref]

A crystal structure specifies the chemical species and spatial arrangement of the chemical atoms or ions in a crystal. For an ideal periodic structure, separate two ingredients: a Bravais lattice specifies the translations that repeat the arrangement, and an atomic basis of a crystal specifies the chemical motif repeated at every lattice point. The outward shape, or crystal habit, is a different description: the internal arrangement is what this article describes.

A proposed modern measurement extends the weak acid dissociation measurement by estimating the local slope of an acid-base titration. Transfer a measured sample with a pipette into a stirred vessel; clamp a combination glass electrode/reference electrode clear of the stirring magnet and place a temperature probe nearby. A calibrated burette delivers a chemical base of independently standardized concentration $c_T$, such as sodium hydroxide. Record the initial sample volume $V_0$, cumulative delivered volume $v$, stable pH, and temperature after each small addition. Use a separate fresh portion for an acidward series. These are proposed measurement conditions, not reported experimental results.

For the instrument calibration, use fresh standard buffer solutions bracketing the measured pH range, with values appropriate to the actual temperature. The Hanna manual specifies separate rinse and calibration portions, gentle stirring, and approximately $4\mathrm{cm}$ immersion of the probe tip. It calls for stable readings; the sensing bulb and reference electrode junction must remain immersed. Rinse between standards and samples and avoid carrying rinse water into the measured portion.^[ref]

The readout pairs each added amount of substance with the measured pH. With negligible added volume, neighboring readings give the finite difference estimateassigned to the interval's midpoint. High buffer capacity appears as a small change of pH for a measured reagent dose. Choose increments small enough to resolve changing buffer capacity, but large enough that the change of pH exceeds measurement noise. Repeat with a fresh portion and different increment sizes; remeasure a standard afterward to check drift. A water blank can reveal contamination, but its pH must not be subtracted from the sample pH. These controls are proposed tests of the measurement and model assumptions.

If additions appreciably increase volume, even the analytical concentration changes: $C(v)=C_0{V}_0/(V_0+v)$. Merely dividing the added moles by the current volume does not restore the constant-volume derivative. One alternative is explicitly to report a changing-volume convention. For $c(v)=c_{T}v/(V_0+v)$, defineThis definition includes the reagent's changing concentration and differs from the constant-volume buffer capacity defined above.^[ref]

To compare with the constant-volume theory, fit the changing-volume chemical equilibrium model instead of treating the observed slope as $\beta$. In the same ideal monoprotic acid system, define $S_0=[{\mathrm{A}}^{-}{]}_0+[{\mathrm{OH}}^{-}{]}_0-[{\mathrm{H}}^{+}{]}_0$. For baseward additions, the electric charge balance at each reading isUse a minus sign before $c_{T}v$ for the corresponding acidward series. From the model parameters, evaluate the constant-volume buffer capacity at the chosen analytical concentration and pH. The fit also tests whether one acid dissociation constant describes the observations.

Limitations include incomplete mixing, slow glass electrode response, uncertain reagent concentration, and changes in temperature or ionic strength. Dissolved atmospheric carbon dioxide introduces an additional chemical acid system; comparable exposure and freshly prepared samples help distinguish it from the intended monoprotic acid response. Additional reacting chemical species and nonideal activity coefficients invalidate the simple formula. Especially when pH increments are tiny, measurement noise can dominate the inferred derivative; reporting the dose, pH interval, volume convention, and repeatability is part of reporting a meaningful buffer capacity.

A buffer solution contains appreciable quantities of a weak acid and its conjugate base, and resists changes in pH caused by small quantities of added chemical acid or chemical base. The conjugate base accepts added protons; the weak acid supplies protons when a chemical base consumes them. Consuming most of either partner undermines the buffering action. See Flowers et al., Chemistry 2e, buffers.

For a separate toy calculation, stipulate pKa $5$ for a weak acid $\mathrm{HA}$; this is an input, not measured material data. Initially $1\mathrm{L}$ of buffer solution contains $0.10\mathrm{mol}$ of $\mathrm{HA}$ and $0.10\mathrm{mol}$ of its conjugate base ${\mathrm{A}}^{-}$. In the ideal concentration approximation, the Henderson-Hasselbalch equation gives initial pH $5$. Add $0.010\mathrm{mol}$ of hydroxide with negligible volume change. The dominant neutralization has one-to-one stoichiometry:Each mole of consumed hydroxide removes one mole of weak acid and forms one mole of conjugate base and water. Thus the inventories after neutralization areThe shared volume cancels from the concentration ratio. The Henderson-Hasselbalch equation therefore predictsThis small increase illustrates how conversion between abundant partners absorbs added chemical base. The calculation neglects the tiny free hydronium and hydroxide inventories, changes during re-establishment of chemical equilibrium, self-ionization of water, and activity coefficient corrections. The displayed inventories approximate the final chemical species distribution; they are not an exact solution of all chemical equilibrium conditions.

A buffer solution has a finite buffer capacity: its weak acid inventory supplies protection against added chemical base, and its conjugate base inventory supplies protection against added chemical acid. Here an addition approaching $0.10\mathrm{mol}$ of hydroxide uses up the available $\mathrm{HA}$ in the dominant stoichiometry calculation. Close to that limit, the neglected chemical equilibrium contributions matter; once $\mathrm{HA}$ is exhausted, inserting a zero denominator into the Henderson-Hasselbalch equation cannot predict the actual pH. Excess hydroxide and the remaining chemical species require a fresh chemical equilibrium calculation. This is why a buffer solution stabilizes conditions for chemical reactions over a finite range of additions. See Flowers et al., Chemistry 2e, buffer capacity and added base.

For the pair $\mathrm{HA}/{\mathrm{A}}^{-}$, rearranging the acid dissociation constant gives the activity relationWith thermodynamic activity of water approximated by one and ideal dilute thermodynamic activities for both partners, this yields the familiar Henderson-Hasselbalch equation:The concentrations are at chemical equilibrium; using initial values requires negligible equilibration changes. Below, also neglect self-ionization of water and competing chemical reactions.

Stipulate $\mathrm{p}{K}_a=4.76$ for an illustrative weak acid, without identifying it with a measured substance. A conjugate base to weak acid concentration ratio of two givesEqual concentrations give a ratio of one, whose logarithm is zero, hence pH $4.76$. Multiplying the ratio by ten raises pH by one: ratios $0.1$, $1$, and $10$ give pH values $3.76$, $4.76$, and $5.76$. The ratio controls the ideal prediction, while the absolute quantities control how much added chemical acid or chemical base the buffer solution can accommodate.

The cathode is the electrode at which the net electrode chemical reaction is reduction: the reacting chemical species gains electrons. This definition is independent of terminal sign. During Daniell cell discharge, ${\mathrm{Cu}}^{2+}$ cations accept electrons arriving at the copper cathode and become neutral copper. The cathode is then the positive terminal. In an externally driven electrolytic cell, the source's negative terminal supplies electrons to the negative cathode. See Pingarrón et al., §3.4: cathode and Daniell cell.

An ion carrying electric current need not undergo reduction at the cathode. For example, in the ideal Daniell cell charge-balance picture, potassium cations arriving from a salt bridge remain dissolved while ${\mathrm{Cu}}^{2+}$ cations are consumed. Follow the half-reaction to identify the reacting species; follow electric charge conservation to account for the other moving ions.

Sites at 000 and one half of each cubic coordinate give $F=f_A+(-1{)}^{h+k+l}{f}_B$. Identical sites produce a body-centered cubic lattice with absent odd-parity reflections. Distinct chemical species generally preserve only the simple cubic lattice translations, so those same odd reflections need not vanish. A geometric body center is not by itself a symmetry translation of the decorated crystal.

The chemical potential measures how a thermodynamic potential changes when matter is added under specified constraints. It plays for matter exchange the role that temperature plays for heat exchange: a difference supplies a direction, and equality characterizes thermodynamic equilibrium when the corresponding exchange is allowed. This connects diffusion, phase coexistence and chemical equilibrium through one quantity.

For a single component, the particle convention iswhere $U$ is internal energy, $N$ counts particles, $S$ is entropy and $V$ is volume. This partial derivative holds entropy and volume fixed; it measures an incremental change rather than the average energy per particle. See David Tong, Statistical Physics, section 1.4.

In chemistry the molar convention instead uses amount of substance $n$, measured in moles:Here $G$ is Gibbs free energy, $T$ is temperature, $p$ is pressure and $N_{\mathrm{A}}$ is the Avogadro constant. The units are $\mathrm{J}$ per particle versus $\mathrm{J}\mathrm{mo}{\mathrm{l}}^{-1}$. For several chemical species, define each chemical potential by varying only its own particle count or amount of substance, with all other components' counts or amounts fixed. Many texts use $\mu$ for either convention, so the units and the variable being differentiated must identify it.

For a simple compressible system with variable component inventories, the fundamental differentials areThey describe changes between states in thermodynamic equilibrium with only pressure-volume work. If every component inventory is fixed, the sums vanish. The Gibbs free energy form follows by differentiating $G=U-TS+pV$ and using $d{N}_i=N_{\mathrm{A}}d{n}_i$; this is why the two definitions describe the same chemical potential in different units.

A chemical potential can be negative. Holding entropy fixed while adding matter need not increase internal energy; Tong explains this explicitly for a classical ideal gas in Statistical Physics, section 2.2.4. Its absolute sign also depends on the reference energy: replacing $U$ by $U+{ϵ}_{0}N$ shifts ${\mu }_{\mathrm{particle}}$ by ${ϵ}_0$. A common reference shift cancels from differences for the same chemical species, which are what determine exchange. Thus “energy cost” means a signed increment, not an always positive amount that must be supplied.