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United States Department of Agriculture

Agricultural Research Service

Methyl Bromide
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1 - Background
2 - Chemical and Physical Properties
3 - Reactions with Stratospheric Ozone
4 - Solubility
5 - Henry's Law Constant
6 - Vapor Pressure
7 - Adsorption
8 - Diffusion Coefficient
9 - Air Sampling
10 - Field Experiments
11 - Transformation of MeBr in Water
12 - Transformation of MeBr in Soil
13 - Transport Model
14 - Simulating MeBr Volatilization
15 - Fumigation
16 - Post-Fumigation
17 - Further Reading
Diffusion Coefficient
 
The value of the diffusion coefficient of a chemical in the vapor phase is generally 104 times larger than that in the liquid phase (Jury et al., 1983). The diffusion coefficient can be estimated using a variety of methods (Reid et al., 1987), including the Fuller correlation
Diffusion Coefficient equation
 
where Dab is the binary diffusion coefficient (cm2/s), T is the absolute temperature (K), Mab = 2/(Ma-1 + Mb-1), Ma and Mb are the molecular weights of air and MeBr, respectively, P is the pressure (bars) and EL is obtained using the atomic diffusion volumes (Reid et al., 1987). Using this Equation yields an estimated diffusion coefficient for MeBr of 0.114 cm2 s-1 at 20°C and 1 atmosphere ambient pressure. The temperature dependence of the diffusion coefficient is shown in Figure 3 and appears to be nearly a straight line over the temperature range 0-60°C. The temperature dependence of the binary diffusion coefficient can be described using the Equation above or using activation energy and the Arrhenius Equation as shown in Figure 3.
 
Using a screening model, Jury et al., (1991) found that the movement of a chemical is dominated by vapor-phase diffusion if the air-to-water partition coefficient, or the Henry’s Law coefficient (KH) is »10-4. Since the KH for MeBr is approximately 0.25, transport in the vapor phase is important in describing the fate and transport in soil.
 
Diffusion Coefficient graph
 
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Last Modified: 10/20/2005
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