Advanced NMR Shift Predictor Calculator

Predict educational NMR shifts from structure and environment. Adjust shielding, anisotropy, and bonding influences easily. Review estimates, export results, and visualize trends with confidence.

Predicted Result

This section appears above the form after calculation.

Predicted Shift

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δ in ppm

Estimated Range

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Practical comparison window

Confidence

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Heuristic educational score

Region

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Predicted Shift = Base Site Shift + Sum of Applied Corrections
Contribution Correction (ppm)
No result yet.

Interpretation

Complete the form and press Calculate.

Advisory:
Use results as guided estimates, not final assignments.

Chosen Site: --

Base Reference: --

NMR Shift Predictor Inputs

The page uses a single stacked layout, while the input grid expands to three columns on large screens, two on medium screens, and one on mobile.

Choose the nucleus you want to estimate.
Select a site to view its base reference.
Use this for an added nearby heteroatom effect.
Count added O, N, F, Cl, Br, or similar influences.
Apply only one main halogen correction.
Use when the site sits near an aromatic system.
Represents nearby unsaturated anisotropic effects.
Carbonyl groups strongly deshield nearby sites.
Choose a larger value for extended delocalization.
Especially important for O-H and N-H signals.
Polar media can shift exchangeable and polar sites.
Charge changes local shielding and deshielding.
Use for constrained cyclic environments.

Plotly Graph

The graph shows the base shift, each correction, and the final predicted position.

Formula Used

This calculator uses an additive correction model. It starts from a base chemical shift for a chosen proton or carbon environment. It then adds or subtracts structural corrections that represent deshielding or shielding influences.

δpredicted = δbase + Δhetero + Δelectronegative + Δhalogen + Δanisotropy + Δcarbonyl + Δconjugation + ΔH-bond + Δsolvent + Δcharge + Δstrain

Base shift

The base shift represents a typical literature-centered region for a chosen site class, such as alkyl proton, aromatic proton, ether carbon, or carbonyl carbon.

Corrections

Each correction modifies the base value. Deshielding factors raise the ppm value. Shielding factors lower it. The calculator uses simple fixed increments so the result stays transparent and explainable.

Uncertainty window

The estimated range widens when more modifiers are used. That helps reflect the broader spread often seen in real spectra, especially for exchangeable protons and highly substituted carbon sites.

How to Use This Calculator

  1. Select whether you want a 1H or 13C estimate.
  2. Choose the base site class that best matches the atom you are studying.
  3. Add only the extra corrections that are not already captured by the base site.
  4. Press Calculate NMR Shift to show the result above the form.
  5. Review the predicted ppm, range, confidence, and interpretation.
  6. Use the Plotly graph to see how each correction moved the final value.
  7. Export the result with the CSV or PDF buttons.
  8. Compare the estimate with your real spectrum and confirm using splitting, integration, and reference data.

Example Data Table

These sample rows show how the additive model can move a signal from its base site reference into a more realistic range.

Nucleus Example Site Base Shift Total Correction Predicted Shift Estimated Range
1H Benzylic proton with extra oxygen influence 2.35 ppm +1.05 ppm 3.40 ppm 3.20 - 3.60 ppm
1H Vinylic proton near a carbonyl group 5.35 ppm +0.70 ppm 6.05 ppm 5.78 - 6.32 ppm
1H Carboxylic acid proton with strong hydrogen bonding 11.20 ppm +1.25 ppm 12.45 ppm 11.86 - 13.04 ppm
13C Ether carbon attached to oxygen 65.00 ppm +6.00 ppm 71.00 ppm 68.95 - 73.05 ppm
13C Conjugated ketone carbonyl carbon 200.00 ppm +5.00 ppm 205.00 ppm 202.20 - 207.80 ppm

FAQs

What does this calculator estimate?

It estimates educational 1H and 13C chemical shifts using an additive correction model. It combines a base environment shift with structural and environmental adjustments.

Can this replace full spectral analysis?

No. Real NMR interpretation also depends on coupling, integration, symmetry, concentration, temperature, impurities, and instrument settings. Use this as a guided predictor.

Why do O-H and N-H peaks vary so much?

Exchangeable protons respond strongly to solvent, concentration, hydrogen bonding, and temperature. Their peaks may broaden, move, or even disappear after exchange experiments.

Does solvent polarity really matter?

Yes. Polar solvents can alter local shielding, stabilize hydrogen bonding, and shift exchangeable signals. The effect is often modest for fixed carbon sites but important for labile protons.

Why are 13C ranges wider than 1H ranges?

Carbon nuclei span a much larger chemical shift window because carbon environments differ more strongly in electron density and bonding patterns than most proton environments.

Does multiplicity change the chemical shift?

Multiplicity mainly affects splitting, not the core chemical shift. However, neighboring groups that cause splitting can also influence shielding through inductive and anisotropic effects.

Should I add every correction at once?

Only add meaningful corrections beyond the chosen base site. Overfilling options can double count effects and push predictions away from realistic values.

How should I compare this with a real spectrum?

Match the predicted region, not just one exact number. Then confirm with integration, multiplicity, carbon count, reference data, and the molecule’s expected functional groups.

Related Calculators

Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.