OUR / CER / RQ Off-Gas Analyzer
Single Point
Time Series
Organism Preset
Inlet Gas Composition
Inlet O2 (%) ?
Inlet CO2 (%) ?
Outlet Gas Composition
Outlet O2 (%)
Outlet CO2 (%)
Gas Flow Rate (L/min) ?
Culture Volume (L)
Biomass (g/L DCW) ?
Temperature (°C)
Pressure (mbar) ?
Humidity Correction
Paste Time-Series Data ?
Gas Flow (L/min)
Volume (L)

Inlet gas: uses single-point inlet values above. Biomass, temperature, and pressure also shared.

0.00
mmol O2/L/h
Oxygen Uptake Rate (OUR)
CER (mmol CO2/L/h)
RQ
qO2 (mmol/g/h)
qCO2 (mmol/g/h)
ParameterValueUnit

Typical RQ Values by Organism & Substrate

OrganismSubstrateRQMetabolic State
E. coliGlucose (aerobic)1.00Oxidative
E. coliGlucose (overflow)1.1–1.5Acetate production
S. cerevisiaeGlucose (aerobic)1.00Oxidative
S. cerevisiaeGlucose (Crabtree)2.0–10+Ethanol fermentation
P. pastorisMethanol0.66Methanol oxidation
P. pastorisGlycerol0.86Glycerol oxidation
CHO cellsGlucose + glutamine0.9–1.1Mixed metabolism
Lipid oxidationFatty acids0.70Beta-oxidation

Related Articles

How to Calculate OUR in Fermentation
Complete guide to OUR calculation methods
How to Calculate kLa for Any Bioreactor
OTR capacity estimation and oxygen transfer
Acetate Overflow in E. coli
RQ shift as an indicator of overflow metabolism
Yield Coefficients Reference Table
Yx/s, Yo/s, Yp/s values for common organisms

Frequently Asked Questions

How do you calculate OUR from off-gas data?

OUR is calculated using the inert gas (N₂) balance method. Since nitrogen is neither consumed nor produced in aerobic fermentation, it serves as an internal standard for determining the outlet gas flow rate. First, calculate the N₂ fractions: yN2,in = 1 − yO2,in − yCO2,in and yN2,out = 1 − yO2,out − yCO2,out. The outlet flow is Fout = Fin × (yN2,in / yN2,out). Then OUR = (Fin × yO2,in − Fout × yO2,out) / VL, converted to mmol/L/h using the ideal gas molar volume at STP (22.414 L/mol).

What does the respiratory quotient (RQ) tell you about metabolism?

RQ = CER / OUR indicates which metabolic pathways are active. RQ ≈ 1.0 means balanced oxidative glucose metabolism. RQ < 0.7 indicates fat or methanol oxidation (Pichia on methanol gives RQ ≈ 0.66). RQ > 1.0 suggests overflow metabolism — acetate production in E. coli or ethanol production in yeast (Crabtree effect). RQ is used as a real-time control signal: in RQ-stat feeding strategies, the feed rate is adjusted to maintain RQ near the target value, preventing overflow metabolism while maximising growth rate.

What is the difference between OUR and OTR?

OUR (Oxygen Uptake Rate) is the actual oxygen consumed by the culture, measured from off-gas analysis. OTR (Oxygen Transfer Rate) is the rate at which oxygen transfers from gas bubbles to the liquid, defined as kLa × (C* − CL). At steady state, OUR = OTR and dissolved oxygen remains constant. OTRmax = kLa × C* represents the maximum oxygen supply capacity of your bioreactor. When OUR approaches OTRmax, dissolved oxygen drops toward zero and the culture becomes oxygen-limited.

Why is the N₂ balance method needed for off-gas analysis?

The total gas flow rate changes across the bioreactor whenever RQ ≠ 1. If more O₂ is consumed than CO₂ produced (RQ < 1), the total outlet flow is lower than the inlet. If you assume equal flow rates, OUR and CER calculations can have 5–15% errors. The N₂ balance corrects for this: since N₂ is inert, Fout = Fin × yN2,in / yN2,out. This is the standard method in bioprocess engineering textbooks and is implemented in most commercial off-gas analysis software (BlueSens, Infors eve, Eppendorf BioCommand).

What is a normal RQ for E. coli growing on glucose?

E. coli growing fully aerobically on glucose has RQ ≈ 1.0, reflecting the stoichiometry of complete oxidation: C₆H₁₂O₆ + 6O₂ → 6CO₂ + 6H₂O. When growth rate exceeds the capacity for full oxidation (the critical growth rate µcrit ≈ 0.3–0.4 h⁻¹), acetate overflow begins and RQ rises above 1.0. An RQ of 1.1–1.2 is an early warning; above 1.3 indicates significant overflow. In fed-batch fermentation, monitoring RQ and reducing feed rate when RQ > 1.05–1.10 is a proven strategy for minimising acetate accumulation.

How do I correct off-gas data for water vapor?

Outlet gas from a bioreactor is saturated with water vapor at the culture temperature. The water vapor pressure is calculated using the Antoine equation: log₁₀(PH₂O) = 8.07131 − 1730.63 / (233.426 + T), where T is in °C and P in mmHg. At 37°C, PH₂O ≈ 47 mmHg, so about 6.2% of outlet gas is water vapor. If your analyzer reads wet-basis compositions, the dry-basis correction is: ydry = ywet / (1 − yH₂O). Most modern off-gas analyzers (BlueSens, Servomex) include a condenser and measure on a dry basis, but you should check your instrument documentation.