Osmolarity tells you how many osmotically active particles a solution carries per litre, which determines the osmotic pressure it exerts and how it will move water across a membrane. It is the number that decides whether a solution is isotonic, and getting it right is essential when preparing infusions, culture media, or buffers.
How it works
Every solute contributes particles in proportion to both its concentration and how far it dissociates. The osmolar contribution of a solute is its molar concentration multiplied by its van’t Hoff factor i:
osmolarity = sum over solutes of ( C_i x i_i )
The factor i is the number of independent particles one formula unit produces. A non-electrolyte like glucose or urea has i = 1. A salt that splits into two ions, such as NaCl or KCl, has i = 2. One that splits into three, such as CaCl2 or Na2SO4, has i = 3. Summing the weighted concentrations and expressing the result in milliosmoles gives the total in mOsm/L.
Tonicity and notes
Human plasma osmolarity is about 285 to 295 mOsm/L. A solution below that band is hypotonic and tends to drive water into cells, while one above it is hypertonic and tends to draw water out. The tool compares your total against this reference.
Two caveats matter for accuracy. First, osmolarity is per litre of solution, whereas osmolality is per kilogram of water; the two agree closely only in dilute solutions. Second, the van’t Hoff factors used here assume complete dissociation, so for concentrated electrolytes the real osmolarity is a little lower because of ion pairing, an effect described by the osmotic coefficient.