Find [H⁺] from pH 7
pH = 7.00
pH = 7.00, pOH = 7.00, [H⁺] = 1.00 × 10^-7 mol/L, [OH⁻] = 1.00 × 10^-7 mol/L
A oddiy pH calculator to aylantirish H⁺, pH, and pOH for education and tezkor field izohlar. It helps you check pH hisoblash, pOH hisoblash, and hydrogen ion konsentratsiya in one place.
See pH / pOH / [H⁺] / [OH⁻] together, with optional formulalar and short amaliy izohlar.
pH = 7.00
pH = 7.00, pOH = 7.00, [H⁺] = 1.00 × 10^-7 mol/L, [OH⁻] = 1.00 × 10^-7 mol/L
[H⁺] = 1e-3 mol/L
pH = 3.00, pOH = 11.00
pOH = 5.00
pH = 9.00, [OH⁻] = 1.00 × 10^-5 mol/L
A logarithmic expression of hydrogen ion konsentratsiya.
A logarithmic expression of hydroxide ion konsentratsiya.
The logarithmic form of the ion product of suv. Around 25°C, 14 is often used as the asosli value.
An effective konsentratsiya term used to describe non-ideal behavior, especially in konsentrlangan or high-ionic-strength systems.
A system that resists pH change when kislota or asosiy is added, so it cannot be handled by oddiy pH-to-konsentratsiya aylantirish alone.
pH = -log10([H+])pOH = -log10([OH-])pH + pOH = 14.00[H+] = 10^(-pH)[OH-] = 10^(-pOH)Strictly speaking, yes. This vosita uses the asosli assumption pKw = 14.00 and treats harorat as a izoh only.
Not directly. Bufer systems need a different model, so a oddiy pH-to-konsentratsiya aylantirish is not enough.
Treat it as an estimate. For research or sifat nazorat, foydalanish actual measurements, calibration standards, and aktivlik-aware methods when needed.
This vosita assumes mol/L (M).
Fourteen is a keng tarqalgan asosli value near 25°C, but pKw changes with harorat. This vosita fixes it at 14.00 for asosli calculations.