Document 1yy03ggXeB3OnZdNjOKRQ8ond
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`AAtrttahcuhreMdeanrdeelc,omPrmoejnetcst 9o9n7t0h6e1326M43TeFcahtneiocaflFlRueoproorcthe"Amniaclayltsi,caRleMpeotrhtoNdoo.lo8,gyJana.nd17S,up1p9o7r9t". made by Professor Stephen A. Boyd, Michigan State University, dated May 19, 1993.
006506
Review of Technical Report Summary Analytical Methodology and Support
Discussion and Results
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There water
is a strong for organic
Solutes given by the equation (Chiou et al., 1982, Eaviron. Sci. Technol. 16:4-10).
log Kou = 0.862 log S, + 0.710
This relationship the K, value of
6w.o6uxld10pr.ediFcotratshuepKerncoaonldedS,l,iqvuailduessoltuobibleitcyoomfpactai.b4l7eprpebquFirMe
3422 based on that either FM
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by the same group (Chiou 2 looksa litle different
et al.) and I think than the equation
this is above.
a
useful exercise. The The main cautionary
line plotted in note is that
Fig. these
relationships predict (>100 to 150C) the
the supercooled liquid solubility of solids. actual water solubility may be substantially
If the (~ 10x)
solid has a high m.p. lower. When working
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experimental value should fall. It also emphasizes the importance and utility of obtaining
accurate S,, and Ky values.
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relationship. lipid content,
A unified analogous
relationship can be obtained by to normalizing the soil sorption
normalizing the BCF of coefficient, K, tothesoil
a species by its organic carbon
cdoifnfteernetnttospgeicvieesK.o.f. aqTuhaetincoorrmgaalniizsemdsf(ac.tgo.r,, zBoCoFp,l,anikstolnin,eagrupwpiitehs,S,raainndboKwytroounta, clatofgisshc)a.leTfhoer
equation is:
.
log BCF, = 0.899 log K,, + 0.623
(from Chiou, 1985, Environ. Sci. predicting BCF values for different
Technol. 19:57-62). This equation has the advantage species, as long as you know their lipid content.
of
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006507
Experimental
The water solubility here is reported as ppm or 100 times the 0.05 ppm value discussed above.
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should know concentration
if it forms micelles. This (CMC). There are a variety
is of
easily done methods for
by this
measuring the determination.
critical micelle Sorption of this
compound by soil may be quite different above and below the CMC.
`Water solubility determinations. The differenceof 43 times in the water solubilitiesofFM 3925 are FM 3422 seems rather large considering the high degree of structural similarity.
Recommendation
1. Obtain an accurate water solubility for FM 3422 and 3925. 2. Obtain an accurate octanol-water partition coefficient for FM 3422 and 3925.
3. Dcoentceernmtiranteioinfs.FM 3422 and 3925 form micelles, i.e., measure the critical micelle
*A key reference describing methodology for determining water solubility and octanol-water
partition coefficient is:
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Chemists. Washington, D.C.
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