Hydrogen tips the scale
Natural hydrogen is mostly ¹H; swapping to deuterium (²H) adds ~1 g/mol per atom—a tiny change that can make drugs degrade more slowly.
Tip: Press Ctrl/Cmd + K to focus the input. Press Ctrl/Cmd + Enter to re-run the last calculation.
When you input a formula like H2O or C12H22O11, the calculator parses each element, multiplies by its atomic weight (IUPAC averages), and sums the total. It supports simple parentheses such as Fe(OH)3.
The tool detects sequence type from one-letter codes and ambiguity codes (IUPAC):
Residue weights are average literature values and account for polymerization (loss of H2O per bond). One terminal H2O is added back to represent intact ends.
AGYWCF → calculated from average amino-acid residue weights + terminal waterATGCGT → calculated as a polymer from base-specific residue weights + terminal waterYes. The calculator detects sequence type automatically and applies average residue weights for proteins, DNA, and RNA.
All calculations happen in your browser. Nothing is uploaded or stored—ideal for proprietary or unpublished research.
Yes. It handles basic parentheses such as (OH)2, though nested parentheses are not supported in this version.
Natural hydrogen is mostly ¹H; swapping to deuterium (²H) adds ~1 g/mol per atom—a tiny change that can make drugs degrade more slowly.
Proteins/DNA/RNA lose one H₂O per bond during polymerization, but calculators add a terminal water back so the chain ends aren’t undercounted.
Textbook masses use natural-abundance averages; mass spec peaks are monoisotopic—often ~0.5–1 Da lighter on small peptides.
Neutral masses ignore adducts: add ~22.99 for Na⁺ or ~38.96 for K⁺ if you’re matching an ESI spectrum with sodium/potassium adduction.
IUPAC letters like R or N mean multiple possibilities; use exact bases for a single mass, or treat them as a range when designing constructs.