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Administrative data

Hazard for aquatic organisms

Freshwater

Hazard assessment conclusion:
PNEC aqua (freshwater)
PNEC value:
0.126 mg/L
Assessment factor:
50
Extrapolation method:
assessment factor
PNEC freshwater (intermittent releases):
0.46 mg/L

Marine water

Hazard assessment conclusion:
PNEC aqua (marine water)
PNEC value:
0.013 mg/L
Assessment factor:
500
Extrapolation method:
assessment factor

STP

Hazard assessment conclusion:
PNEC STP
PNEC value:
47.47 mg/L
Assessment factor:
100
Extrapolation method:
assessment factor

Sediment (freshwater)

Hazard assessment conclusion:
PNEC sediment (freshwater)
PNEC value:
0.484 mg/kg sediment dw
Extrapolation method:
equilibrium partitioning method

Sediment (marine water)

Hazard assessment conclusion:
PNEC sediment (marine water)
PNEC value:
0.048 mg/kg sediment dw
Extrapolation method:
equilibrium partitioning method

Hazard for air

Air

Hazard assessment conclusion:
no hazard identified

Hazard for terrestrial organisms

Soil

Hazard assessment conclusion:
PNEC soil
PNEC value:
0.023 mg/kg soil dw
Extrapolation method:
equilibrium partitioning method

Hazard for predators

Secondary poisoning

Hazard assessment conclusion:
no potential for bioaccumulation

Additional information

Read-across approach In the assessment of the environmental fate and ecotoxicity of potassium adipate, a read-across approach from data for adipic acid (CAS 124 -04 -9; EC 204 -673 -3) is followed. This read-across strategy is based upon the assumptions that i) upon release to the environment, potassium adipate will completely dissociate and only be available in its dissociated form, i.e. as potassium cation and the adipic anion and ii) toxicity is only caused by the adipic anion.

Upon dissolution in water, it is indeed predicted that metal carboxylates dissociate completely into the metal cation and the organic anion at environmentally relevant conditions. No information is available on the stability constants of potassium adipate, but predictions of stability of another potassium carboxylate (K isovalerate) in a standard ISO 6341 medium (2 mMCaCl2, 0.5 mM MgSO4, 0.77 mM NaHCO3 and 0.077 mM KCl, pH 6 and 8) clearly show that carboxylic acids have no potential for complexing potassium ions in solution (Visual minteq. Version 3.0, update of 18 October 2012. http://www2.lwr.kth.se/English/OurSoftware/vminteq/index.html).

Potassium is abundantly present in natural environments (Table x), and emissions of potassium adipate are not expected to significantly increase the exposure concentration for potassium in water, sediment and soil. Moreover, potassium is a major essential element for living organisms and therefore it is not considered as critical for the environmental effects assessment of potassium adipate.

Table x. Typical baseline background concentrations for potassium in water, sediment and soil (data for freshwater, sediment and soil from FOREGS*, data for marine water from Culkin and Cox, 1966)

 Compartment Unit   Typical (50th percentile baseline level) 90th percentile of baseline concentrations 
 Aquatic (freshwater) mg K/L 1.60  6.83 
 Aquatic (marine water) mg K/L  399   
Sediment (freshwater)  mg K/kg dw  11050  17650 
Topsoil mg K/kg dw  10560  17870 

* The FOREGS geochemical baselines mapping program represents the end twentieth century state of the surficial environment in Europe. The main aim of the FOREGS (Forum of European Geological Surveys) Geochemical Baseline Mapping Program was to provide high quality, multi-purpose environmental geochemical background data for stream water, stream sediment, floodplain sediment, soil, and humus across Europe. A baseline background concentration was defined as the concentration of an element in the present or past corresponding to very low anthropogenic pressure (i.e., close to the natural background). The FOREGS-data set was published in September 2007 (http://www.gsf.fi/publ/foregsatlas/ForegsData.php) and is considered to be of high quality. A detailed description of sampling methodology, sampling preparation and analysis is given by Salminen et al. (2005).

References:

Culkin, F. and R.A. Cox. 1966. Sodium, potassium, magnesium, calcium and strontium in sea water. Deep-Sea Res., 13: 789-804. Salminen, R. (Chief-editor), Batista, M.J., Bidovec, M. Demetriades, A., De Vivo. B., De Vos, W., Duris, M., Gilucis, A., Gregorauskiene, V., Halamic, J., Heitzmann, P., Lima, A., Jordan, G., Klaver, G., Klein, P., Lis, J., Locutura, J., Marsina, K., Mazreku, A., O'Connor, P.J., Olsson, S.Å., Ottesen, R.-T., Petersell, V., Plant, J.A., Reeder, S., Salpeteur, I., Sandström, H., Siewers, U., Steenfelt, A., Tarvainen, T., 2005. Geochemical Atlas of Europe. Part 1 – Background Information, Methodology and Maps. Geological Survey of Finland, Espoo, Finland, 526 pp. ISBN 951-690-921-3 [also available at: http://www.gtk.fi/publ/foregsatlas/].

Conclusion on classification

Potassium adipate will dissociate into potassium and adipate ions after dissolution in water and hence can be regarded as a mixture of both constituent ions. The classification as hazardous to the aquatic environment of potassium adipate is therefore based on the classification of its moieties (K and adipic acid). Both potassium and adipic acid are not classified as hazardous to the aquatic environment, and according to the summation method, it is concluded that potassium adipate is not hazardous to the aquatic environment.

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