Step 1: Henry's Law and Concentration in Air
Henry's Law relates the concentration of a gas in the air to its concentration in water: Cair=H×CwaterCair=H×Cwater
Where:
- CairCair is the concentration of the gas in the air (atm)
- HH is Henry's law constant (atm·m³/mol)
- CwaterCwater is the concentration of the gas in water (mol/m³)
Given:
- Cwater=0.25 ppb=0.25×10−9 g/LCwater=0.25ppb=0.25×10−9g/L
First, convert CwaterCwater from g/L to mol/m³: Molecular weight of C2Cl4=165.83 g/molMolecular weight of C2Cl4=165.83g/mol
Cwater=0.25×10−9 g/L165.83 g/molCwater=165.83g/mol0.25×10−9g/L Cwater=1.507×10−12 mol/L=1.507×10−9 mol/m3Cwater=1.507×10−12mol/L=1.507×10−9mol/m3
Using Henry's Law: Cair=H×CwaterCair=H×Cwater H=0.081 atm\cdotpm3/molH=0.081atm\cdotpm3/mol
Cair=0.081×1.507×10−9Cair=0.081×1.507×10−9 Cair=1.221×10−10 atmCair=1.221×10−10atm
Step 2: Calculate the Flux Density
The volatilization flux (J) can be calculated using the gas exchange coefficient and the concentration difference between water and air: J=kL×(Cwater−Cair/H)J=kL×(Cwater−Cair/H)
Given:
- kL=2.6×10−3 cm/s=2.6×10−5 m/skL=2.6×10−3cm/s=2.6×10−5m/s
Assuming CairCair is negligible: J=kL×CwaterJ=kL×Cwater J=2.6×10−5 m/s×1.507×10−9 mol/m3J=2.6×10−5m/s×1.507×10−9mol/m3 J=3.92×10−14 mol/(m2s)J=3.92×10−14mol/(m2s)
Step 3: Convert the Flux Density to a More Convenient Unit
To convert to g/(m²·s): J=3.92×10−14 mol/(m2s)×165.83 g/molJ=3.92×10−14mol/(m2s)×165.83g/molJ=6.5×10−12 g/(m2s)J=6.5×10−12g/(m2s)
Important Environmental Factors
Two significant environmental factors that can affect the volatilization flux of tetrachloroethylene are:
- Water Temperature: Higher water temperatures increase the kinetic energy of the molecules, which can enhance the volatilization rate. Additionally, Henry's law constant is temperature-dependent, typically increasing with temperature, leading to higher gas concentrations in the air above the water.
- Wind Speed and Turbulence: Increased wind speed and surface water turbulence enhance the gas exchange rate by reducing the boundary layer resistance at the water-air interface. This increases the volatilization flux of tetrachloroethylene from the water to the atmosphere.