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Membrane Potential Calculator

Calculate resting membrane potential and action potential parameters using the Goldman-Hodgkin-Katz equation

Category: Biology

Membrane Potential Calculator Inputs

Enter values to calculate

Extracellular potassium concentration

Intracellular potassium concentration

Extracellular sodium concentration

Intracellular sodium concentration

Extracellular chloride concentration

Intracellular chloride concentration

Relative permeability to potassium

Relative permeability to sodium

Relative permeability to chloride

Temperature in Celsius

Enable JavaScript for interactive calculation and step-by-step results.

Membrane Potential Calculator Formula

Equation

V_m = (RT/F) × ln((P_K[K^+]_o + P_Na[Na^+]_o + P_Cl[Cl^-]_i)/(P_K[K^+]_i + P_Na[Na^+]_i + P_Cl[Cl^-]_o)) Nernst Equation: E_ion = (RT/zF) × ln([ion]_o/[ion]_i)

Excel Formula

=V_m=(RT/F)×ln(P_K[K^+]_o+P_Na[Na^+]_o+P_Cl[Cl^-]_i)/(P_K[K^+]_i+P_Na[Na^+]_i+P_Cl[Cl^-]_o)NernstEquation:E_ion=(RT/zF)×ln([ion]_o/[ion]_i)

Variables

  • Extracellular Potassium Concentration (mM) — Extracellular potassium concentration
  • Intracellular Potassium Concentration (mM) — Intracellular potassium concentration
  • Extracellular Sodium Concentration (mM) — Extracellular sodium concentration
  • Intracellular Sodium Concentration (mM) — Intracellular sodium concentration
  • Extracellular Chloride Concentration (mM) — Extracellular chloride concentration
  • Intracellular Chloride Concentration (mM) — Intracellular chloride concentration
  • Potassium Permeability (relative) — Relative permeability to potassium
  • Sodium Permeability (relative) — Relative permeability to sodium
  • Chloride Permeability (relative) — Relative permeability to chloride
  • Temperature (°C) — Temperature in Celsius

How the Membrane Potential Calculator Works

Calculate resting membrane potential and action potential parameters using the Goldman-Hodgkin-Katz equation The Membrane Potential Calculator is designed for Biology applications where you need repeatable, transparent calculations rather than one-off mental math. The relationship is expressed as V_m = (RT/F) × ln((P_K[K^+]_o + P_Na[Na^+]_o + P_Cl[Cl^-]_i)/(P_K[K^+]_i + P_Na[Na^+]_i + P_Cl[Cl^-]_o)) Nernst Equation: E_ion = (RT/zF) × ln([ion]_o/[ion]_i). Use it to verify hand work, compare design alternatives, explore sensitivity to each input, and document assumptions for reports or study notes. Consistent units and realistic input ranges are essential: small data-entry errors often move results more than formula uncertainty. This overview frames what the tool computes, when it applies, and how to read outputs alongside the detailed sections below.

The core relationship is V_m = (RT/F) × ln((P_K[K^+]_o + P_Na[Na^+]_o + P_Cl[Cl^-]_i)/(P_K[K^+]_i + P_Na[Na^+]_i + P_Cl[Cl^-]_o)) Nernst Equation: E_ion = (RT/zF) × ln([ion]_o/[ion]_i). Typical inputs include Extracellular Potassium Concentration, Intracellular Potassium Concentration, Extracellular Sodium Concentration, Intracellular Sodium Concentration.

Enter your values in the membrane potential calculator above, review the step-by-step solution, and compare against the worked examples below so you can see how each input changes the result. This free online biology tool is built for homework, design checks, and professional verification.

Membrane Potential Calculator Theory & Explanation

Goldman-Hodgkin-Katz Equation

The Goldman-Hodgkin-Katz equation calculates the resting membrane potential by considering the concentration gradients and relative permeabilities of the major ions (K+, Na+, Cl-). This equation provides a more accurate prediction than the Nernst equation for a single ion.

V_m = (RT)/(F) \ln(\fracP_K[K^+]_o + P_Na[Na^+]_o + P_Cl[Cl^-]_iP_K[K^+]_i + P_Na[Na^+]_i + P_Cl[Cl^-]_o)

Nernst Equation

The Nernst equation calculates the equilibrium potential for a single ion species. It represents the membrane potential at which there is no net movement of that ion across the membrane.

E_ion = (RT)/(zF) \ln(([ion]_o)/([ion]_i))

Ion Contributions

At rest, the membrane is most permeable to K+, making the resting potential close to the K+ equilibrium potential. Na+ and Cl- also contribute, with Na+ tending to depolarize and Cl- tending to hyperpolarize the membrane.

E_K ≈ -90\,mV, E_Na ≈ +60\,mV, E_Cl ≈ -70\,mV

Action Potential

An action potential occurs when the membrane potential reaches threshold (typically around -55 mV). This triggers rapid depolarization due to Na+ influx, followed by repolarization due to K+ efflux.

Threshold ≈ -55\,mV, Peak ≈ +30\,mV, Rest ≈ -70\,mV

Problem Context and Scope

Calculate resting membrane potential and action potential parameters using the Goldman-Hodgkin-Katz equation In professional Biology work, the same calculation appears in specifications, lab notebooks, spreadsheets, and compliance checks. The Membrane Potential Calculator automates that relationship so you can focus on interpreting outcomes instead of re-deriving algebra. Scope includes typical textbook and field assumptions; exotic boundary conditions, non-standard materials, or regulatory overrides may require specialist review. Before trusting a number for safety-critical, medical, legal, or financial decisions, cross-check units, sign conventions, and whether your scenario matches the model intent described here.

Formula Derivation and Meaning

The calculator implements V_m = (RT/F) × ln((P_K[K^+]_o + P_Na[Na^+]_o + P_Cl[Cl^-]_i)/(P_K[K^+]_i + P_Na[Na^+]_i + P_Cl[Cl^-]_o)) Nernst Equation: E_ion = (RT/zF) × ln([ion]_o/[ion]_i). Each symbol corresponds to a physical, economic, or statistical quantity with implied units. Rearranging the expression highlights which inputs dominate: proportional terms scale linearly, ratios amplify sensitivity when denominators are small, and powers or roots change how uncertainty propagates. When multiple forms of the same law exist, use the version consistent with your reference tables and unit system. Document which variant you applied when sharing results with colleagues or reviewers so comparisons remain fair and reproducible across tools and spreadsheets.

V_m = (RT/F) × ln((P_K[K^+]_o + P_Na[Na^+]_o + P_Cl[Cl^-]_i)/(P_K[K^+]_i + P_Na[Na^+]_i + P_Cl[Cl^-]_o)) Nernst Equation: E_ion = (RT/zF) × ln([ion]_o/[ion]_i)

Input Parameters Explained

Key inputs include Extracellular Potassium Concentration, Intracellular Potassium Concentration, Extracellular Sodium Concentration, Intracellular Sodium Concentration, Extracellular Chloride Concentration, Intracellular Chloride Concentration, Potassium Permeability, Sodium Permeability. Enter values in the units shown beside each field; mixing systems without conversion is the most common source of large errors. Defaults and sliders reflect typical ranges but are not universal limits—extrapolating far beyond calibrated data may still return numbers while losing physical meaning. For select lists, choose the option that best matches your scenario even if labels are approximate. If an input is optional, leaving it blank may trigger built-in assumptions; read tooltips or descriptions when available. Sensitivity analysis—changing one input at a time—reveals which parameters deserve higher measurement precision.

Step-by-Step Calculation Procedure

First, gather measured or assumed values and convert them to the required units. Second, enter data in the Membrane Potential Calculator form and confirm selections or toggles that alter the model branch. Third, submit the calculation and record the primary output together with any secondary metrics or charts. Fourth, sanity-check magnitude and sign: compare against order-of-magnitude estimates, limiting cases, or known benchmarks. Fifth, if results feed another equation, propagate uncertainty explicitly rather than treating intermediate values as exact. This workflow mirrors good laboratory and engineering practice and reduces the risk of publishing a correct formula with incorrect inputs.

Practical Applications

Typical uses include homework verification, quick feasibility checks, client estimates, and teaching demonstrations. Teams often run best, nominal, and conservative cases to bracket outcomes. In design iterations, automate repeated evaluations while varying one parameter across a sweep. In education, pair calculator output with hand-derived steps to build intuition. In operations, snapshot inputs and outputs for audit trails when regulations require traceability. Pair numerical results with charts when available to communicate trends to non-specialist stakeholders who may not read equations comfortably.

Common Mistakes and Troubleshooting

Watch for unit slips (meters versus feet, percent versus decimal), sign errors (compression versus tension, income versus expense), off-by-one period choices (monthly versus annual rates), and using stale constants. If results look surprising, re-check input order, whether angles are in degrees or radians, and whether the tool expects absolute or gauge values. Compare with a second method or tabulated example when possible. Large discontinuities often indicate crossing a domain threshold coded in the implementation—review piecewise rules. When exporting to spreadsheets, lock cell references so later edits do not silently break linked formulas.

Accuracy, Limitations, and Validation

Displayed precision may exceed real-world accuracy. Report only the significant figures justified by your input quality. The model may assume ideal conditions—uniform properties, steady state, linear response, perfect markets, or representative samples—that real systems violate. Validate against measured data when stakes are high. Document temperature, pressure, humidity, sample size, or market regime if they influence constants. For regulated industries, cite the code edition or standard you followed. Treat online tools as aids, not replacements for professional judgment where codes mandate licensed review.

Related Concepts and Extensions

Adjacent topics often include dimensional analysis, uncertainty propagation, inverse problems (solving for an input given a target output), and optimization under constraints. Exploring related calculators on the same topic helps build a coherent workflow—for example, converting units before using this tool, or feeding its output into a downstream capacity check. Advanced users may implement custom scripts that batch-evaluate the same relationship across parameter grids. Students benefit from plotting dependent variables versus one input while holding others fixed, reinforcing calculus and physical intuition beyond a single numeric answer.

Membrane Potential Calculator Worked Examples

Worked Example

Inputs

  • k_out: 4
  • k_in: 140
  • na_out: 145
  • na_in: 12
  • cl_out: 110
  • cl_in: 4
  • p_k: 1
  • p_na: 0.04
  • p_cl: 0.45
  • temperature: 37

Explanation

The calculated resting membrane potential of -70.2 mV is typical for neurons. The K+ equilibrium potential (-91.8 mV) is close to the resting potential, indicating that K+ permeability dominates at rest. The Na+ equilibrium potential (+61.5 mV) shows the driving force for depolarization during action potentials.

Second Scenario

Inputs

  • k_out: 4.6
  • k_in: 140
  • na_out: 145
  • na_in: 12
  • cl_out: 110
  • cl_in: 4
  • p_k: 1
  • p_na: 0.04
  • p_cl: 0.45
  • temperature: 37

Explanation

This scenario uses different inputs (k_out = 4.6, k_in = 140, na_out = 145, na_in = 12, cl_out = 110, cl_in = 4, p_k = 1, p_na = 0.04, p_cl = 0.45, temperature = 37) to show how changing one variable affects the membrane potential result. Run the calculator above with these values to get the exact updated output with step-by-step work.

Common Membrane Potential Calculator Use Cases

  • Membrane Potential homework and study
  • Membrane Potential design and analysis
  • Quick membrane potential estimates
  • Verifying spreadsheet or hand calculations

Membrane Potential Calculator FAQs

Why is the resting potential negative?

The resting potential is negative because there are more negative charges (anions) inside the cell than outside. This is primarily due to the high intracellular K+ concentration and the fact that the membrane is more permeable to K+ at rest, allowing K+ to diffuse out and leave behind negative charges.

What happens during an action potential?

During an action potential, the membrane potential rapidly depolarizes from -70 mV to about +30 mV due to Na+ influx through voltage-gated Na+ channels. This is followed by repolarization due to K+ efflux through voltage-gated K+ channels, returning the membrane to resting potential.

How does the sodium-potassium pump affect membrane potential?

The Na+/K+ pump directly contributes only a few millivolts to the membrane potential. However, it maintains the concentration gradients that drive the resting potential by pumping 3 Na+ out and 2 K+ in for each ATP hydrolyzed, creating the ionic gradients that the Goldman equation uses.

What is the difference between equilibrium potential and resting potential?

Equilibrium potential (Nernst potential) is the membrane potential at which there is no net movement of a specific ion. Resting potential (Goldman potential) is the actual membrane potential at rest, determined by the relative permeabilities and concentrations of all permeable ions.

What does the Membrane Potential Calculator calculate?

It applies the formula on this page to your inputs and returns the primary result plus any supporting values shown in the output panel.