Deposition

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Deposition is a process where compounds in air come down and stay in the soil or water. This page is a method about estimating deposition of different compounds.

Question

How to estimate deposition for different compounds?

Answer

Default key: UcK5o1jtjD3DMLT5 [1]

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Rationale

If there is no need to consider atmospheric chemistry, it can be assumed that everything that goes into the air eventually comes down. The question is: what is the geographical distribution of the deposition around the source?

For screening purposes, we can assume that the wind rose is a circle (especially if averaged over long periods of time), although in many places this is not true. However, meteorological information is not easily available and usable, and then the alternative is to not estimate anything. Therefore, a robust assumption is better than no estimate.

Many compounds of interest are naturally occurring compounds in small concentrations (such as metals), and many living organisms have developed some tolerance against exposure to these compounds. Therefore, if the exposure is very low (e.g. much smaller than natural background), we can assume that a very small deposition does not cause such increases in environmental concentrations that it would have any human or ecological impact. Thus, the critical question is this: what is the area where the deposition causes biologically significant increases in concentrations and thus exposures?

It is important to notice that if the deposition is very quick, the compound deposits near the source in high amounts, causing high exposures to very small area and small number of individuals. On the other hand, if the deposition is very low, the compound deposits in a very large area and a large number of individuals are exposed to biologically insignificant amounts. Therefore, there seems to be somewhere in between a deposition rate that causes the maximal health impact. What that deposition rate is, depends on the total emission, the threshold of biologically significant exposure, and the population distribution.

We can assume constant deposition rate as a function of distance from source, which results in exponential reduction of the compound in air:

Failed to parse (Missing <code>texvc</code> executable. Please see math/README to configure.): M_r = M_0 * e^{-k r}

where M is the mass of compound (in kg) in air when it has traveled distance r, and k is a deposition rate constant. This will result in deposition rate S (in kg/m2):

Failed to parse (Missing <code>texvc</code> executable. Please see math/README to configure.): S_r = \frac{-D(M_0 * e^{-k r})}{2 \pi r} = \frac{k M_0 e^{-k r}}{2 \pi r},

which is the negative derivative of the mass in the air at distance r, divided by the circumference of a circle centered around the source at that distance. Time is not involved in the equation, because we are observing the situation integrated over a proper time period.

This results in a robust equation with only two parameters, deposition rate k and emission M0 (and the emission is assumed to be known).

See also

References


Related files

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