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Environmental fate & pathways

Adsorption / desorption

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Administrative data

Endpoint:
adsorption / desorption: screening
Type of information:
experimental study
Adequacy of study:
key study
Study period:
2002/08/23 to 2003/03/25
Reliability:
1 (reliable without restriction)
Rationale for reliability incl. deficiencies:
guideline study

Data source

Reference
Reference Type:
study report
Title:
Unnamed
Year:
2003
Report date:
2003

Materials and methods

Test guideline
Qualifier:
according to guideline
Guideline:
OECD Guideline 106 (Adsorption - Desorption Using a Batch Equilibrium Method)
Version / remarks:
2000
Deviations:
yes
Remarks:
Deviations to SETAC are minor.
GLP compliance:
yes
Type of method:
batch equilibrium method
Media:
soil

Test material

Constituent 1
Chemical structure
Reference substance name:
N-cyclopropyl-1,3,5-triazine-2,4,6-triamine
EC Number:
266-257-8
EC Name:
N-cyclopropyl-1,3,5-triazine-2,4,6-triamine
Cas Number:
66215-27-8
Molecular formula:
C6H10N6
IUPAC Name:
N2-cyclopropyl-1,3,5-triazine-2,4,6-triamine
Test material form:
solid: particulate/powder
Radiolabelling:
no

Study design

Test temperature:
20 °C

Batch equilibrium or other method

Analytical monitoring:
yes
Matrix propertiesopen allclose all
Matrix no.:
#3
Matrix type:
loamy sand
% Clay:
7.7
% Silt:
10.8
% Sand:
81.5
% Org. carbon:
1.8
pH:
6.8
CEC:
134 other: meq/kg
Matrix no.:
#2
Matrix type:
loam
% Clay:
22.7
% Silt:
43.1
% Sand:
34.2
% Org. carbon:
1.5
pH:
7.5
CEC:
200 other: meq/kg
Matrix no.:
#1
Matrix type:
loamy sand
% Clay:
4.1
% Silt:
16.9
% Sand:
79
% Org. carbon:
1.3
pH:
5.9
CEC:
106 other: meq/kg
Details on matrix:
Loamy Sand (#1) - Horst Soil
Loam (#2) - Westmaas soil
Loamy Sand (#3) - Naaldwijk soil
Details on test conditions:
Adsorption and desorption experiments were carried out at five concentration levels of the test compounds at 20°C in the dark. Initial concentrations of the test compounds in aqueous 0.01 M CaCl2- solution ranged from 0.07 to 6.0 µg/mL. 50 g of each soil type were pre-equilibrated with 0.01 M CaCl2-solution for 24 hours and the application solutions were added, resulting in a soil-to-solution ratio of 1:1. After equilibration, the phases were separated by centrifugation. The equilibrated water layer was removed. The concentration of test compound in the original solution and in the aqueous layer after equilibration was measured by HPLC, after which the adsorption was calculated from the difference. Following the adsorption experiment, desorption of the test compound was measured by replacing the removed aqueous phase by the same volume of 0.01 M CaCl2-solution. After this, the tubes were equilibrated again and the phases separated by centrifugation. The respective aqueous solutions were analysed by HPLC to quantify the amount of test item and to determine the distribution of the substances between solid and aqueous phase. The equilibration times for the adsorption and the desorption stages were 24 hours for cyromazine and 72 hours for melamine. After the desorption step, the soil layer was also subjected to chemical analysis in order to obtain a mass balance.
Duration of adsorption equilibration
Duration:
24 h
Remarks:
All soils
Duration of desorption equilibration
Duration:
24 h
Remarks:
All soils

Results and discussion

Adsorption coefficientopen allclose all
Key result
Sample No.:
#1
Type:
Koc
Remarks:
adsorption Kfoc
Value:
521 other: mL/g
pH:
5.9
Remarks on result:
other: 1/n 0.92
Key result
Sample No.:
#2
Type:
Koc
Remarks:
adsorption Kfoc
Value:
96 other: mL/g
pH:
7.5
Remarks on result:
other: 1/n 0.73
Key result
Sample No.:
#3
Type:
Koc
Remarks:
adsorption Kfoc
Value:
200 other: mL/g
pH:
6.8
Remarks on result:
other: 1/n 0.87
Partition coefficients
Remarks on result:
not determinable

Results: Batch equilibrium or other method

Adsorption and desorption constants:
For cyromazine, the mean adsorption coefficient KF was 3.94 mL/g, the mean adsorption KOC-value 272 ml/g. The compound is hence found to be of medium mobility (McCall). The slope N for the adsorption isotherms was on average 0.84, indicating a non-linear concentration dependence of KF (increasing KF with decreasing concentration). The adsorption coefficient strongly correlates with the pH value of the soils, whereas only a weak to medium correlation with the clay content and the cation exchange capacity was found. No significant correlation of KF with the organic carbon content of the soil was observed, indicating that the carbon content does not represent a measure for sorption. Nevertheless, the KOC-value correlates relatively strongly with the soil pH due to the dominant pH- dependence of KD and the low variation of the organic carbon content of the three soils. Adsorption of cyromazine was to some extent reversible in the tested soils, i.e. desorption coefficient was in the same range as the adsorption coefficient. For desorption a mean coefficient of 4.35 mL/g and a mean KOC-value of 296 mL/g were calculated.
Recovery of test material:
The mass balance during the sorption experiment for the soils Horst, Westmaas and Naaldwijk ranged for cyromazine from 83 to 86%. The lower recovery of cyromazine is partly the result of transformation of cyromazine into melamine.

Any other information on results incl. tables

Table 2: Freundlich adsorption and desorption constants of cyromazine



























































Cyromazine



Soil texture



Adsorption



Desorption



 



KF (mL/g)



KOC(mL/g)



N



KF (mL/g)



KOC (mL/g)



N



Horst


Loamy sand



 


6.77



 


521



 


0.92



 


6.56



 


505



 


0.84



Westmaas


Loam



 


1.44



 


96



 


0.73



 


2.01



 


134



 


0.84



Naaldwijk


Loamy sand



 


3.60



 


200



 


0.87



 


4.48



 


249



 


0.85



Mean



3.94



272



0.84



4.35



296



0.84


Applicant's summary and conclusion

Validity criteria fulfilled:
not specified
Conclusions:
The mean adsorption coefficient KF was 3.94 mL/g, the mean adsorption KOC-value 272 mL/g. The compound is hence found to be of medium mobility. For desorption a mean coefficient of 4.35 mL/g and a mean KOC-value of 296 mL/g were calculated.
Executive summary:

The adsorption and desorption of the test compounds cyromazine and melamine were investigated in three soils, using the batch equilibrium method following OECD Guideline 106. Adsorption and desorption experiments were carried out at five concentration levels of the test compounds at 20°C in the dark. Initial concentrations of the test compounds in aqueous 0.01 M CaCl2- solution ranged from 0.07 to 2.0 µg/mL. 50 g of each soil type were pre-equilibrated with 0.01 M CaCl2-solution for 24 hours and the application solutions were added, resulting in a soil-to-solution ratio of 1:1.


The mass balance during the sorption experiment for the soils Horst, Westmaas and Naaldwijk ranged for cyromazine from 83 to 86%. The lower recovery of cyromazine is partly the result of transformation of cyromazine into melamine. For cyromazine, the mean adsorption coefficient KF was 3.94 mL/g, the mean adsorption KOC-value 272 mL/g. The compound is hence found to be of medium mobility. For desorption a mean coefficient of 4.35 mL/g and a mean KOC-value of 296 mL/g were calculated.