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User Guide to Thresholds and Classification - Environmental ...

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361<strong>User</strong> <strong>Guide</strong> for <strong>Thresholds</strong> <strong>and</strong> <strong>Classification</strong>schemicals with unknown hydrolysis rates <strong>and</strong> a more detailed test that is performed for chemicals that areknown <strong>to</strong> be hydrolytically unstable <strong>and</strong> for chemicals for which the preliminary test shows fast hydrolysis. Inthe preliminary test the concentration of the chemical in buffered solutions at pHs in the range normallyfound in the environment (pHs of 4, 7 <strong>and</strong> 9) at 50°C is measured after 5 days. If the concentration of thechemical has decreased less than 10% it is considered hydrolytically stable, otherwise the detailed test maybe performed. In the detailed test, the overall hydrolysis rate is determined at three pHs (4, 7 <strong>and</strong> 9) bymeasuring the concentration of the chemical as a function of time. The hydrolysis rate is determined atdifferent temperatures so that interpolations or extrapolations <strong>to</strong> environmentally relevant temperatures canbe made. The OPPTS 835.2130 test is almost identical in design <strong>to</strong> the OECD Test <strong>Guide</strong>line 111, thedifference mainly being in the treatment of data.It should be noted that apart from hydrolysis the hydrolysis rate constants determined by the tests include allother abiotic transformations that may occur without light under the given test conditions. Good agreementhas been found between hydrolysis rates in natural <strong>and</strong> in pure waters (OPPTS 835.2110).Pho<strong>to</strong>lysisAt present, there is a draft OECD guideline on aqueous pho<strong>to</strong>degradation, <strong>and</strong> a guidance document,concerning aquatic direct pho<strong>to</strong>lysis, is available (OECD, 1997). The guidance document is supposed <strong>to</strong>form the basis for the scheduled guideline. According <strong>to</strong> the definitions set out in this guidance document,pho<strong>to</strong>transformation of compounds in water can be in the form of primary or secondary pho<strong>to</strong>transformation,where the primary pho<strong>to</strong>transformation (pho<strong>to</strong>lysis) can be divided further in<strong>to</strong> direct <strong>and</strong> indirect pho<strong>to</strong>lysis.Direct pho<strong>to</strong>transformation (pho<strong>to</strong>lysis) is the case where the chemical absorbs light <strong>and</strong> as a direct resulthereof undergoes transformation. Indirect pho<strong>to</strong>transformation is the case where other excited speciestransfer energy, electrons or H-a<strong>to</strong>ms <strong>to</strong> the chemical <strong>and</strong> thereby induces a transformation (sensitisedpho<strong>to</strong>lysis). Secondary pho<strong>to</strong>transformation is the case where chemical reactions occur between thechemical <strong>and</strong> reactive short lived species like hydroxy radicals, peroxy radicals or singlet oxygen that areformed in the presence of light by reactions of excited species like excited humic or fulvic acids or nitrate.The only currently available guidelines on pho<strong>to</strong>transformation of chemicals in water are therefore OPPTS835.2210 Direct pho<strong>to</strong>lysis rate in water by sunlight <strong>and</strong> OPPTS 835.5270 Indirect pho<strong>to</strong>lysis screening test.The OPPTS 835.2210 test uses a tiered approach. In Tier 1 the maximum direct pho<strong>to</strong>lysis rate constant(minimum half-life) is calculated from a measured molar absorptivity. In Tier 2 there are two phases. InPhase 1 the chemical is pho<strong>to</strong>lysed with sunlight <strong>and</strong> an approximate rate constant is obtained. In Phase 2,a more accurate rate constant is determined by using an actinometer that quantifies the intensity of the lightthat the chemical has actually been exposed <strong>to</strong>. From the parameters measured, the actual directpho<strong>to</strong>degradation rate at different temperatures <strong>and</strong> for different latitudes can be calculated. Thisdegradation rate will only apply <strong>to</strong> the uppermost layer of a water body, for example, the first 50 cm or less<strong>and</strong> only when the water is pure <strong>and</strong> air saturated which may clearly not be the case in environment.However, the results can be extended over other environmental conditions by the use of a computerprogram incorporating attenuation in natural waters <strong>and</strong> other relevant fac<strong>to</strong>rs.January 2012 EPA0109

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