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Adsorption / desorption

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Reference
Endpoint:
adsorption / desorption: screening
Type of information:
experimental study
Adequacy of study:
key study
Study period:
2017-08-14 to 2017-09-28
Reliability:
1 (reliable without restriction)
Rationale for reliability incl. deficiencies:
guideline study
Qualifier:
according to guideline
Guideline:
OECD Guideline 106 (Adsorption - Desorption Using a Batch Equilibrium Method)
Version / remarks:
The number of soils which were used deviates from the guideline recommendation in the guideline as three soils were used instead of the recommended five soils. The Freundlich isotherms were not determined and the adsorption / desorption behavior was investigated based on one test item concentration. This was the lowest reasonable test concentration which could be used in relation to the detection limit. These deviations from the guideline were on request of the sponsor and are based on earlier adsorption / desorption studies with cationic surfactants

Samples were centrifuged < 3000 g if glass vessels had to be used. Higher centrifugation forces would have destroyed these vials.

Deviations:
yes
Remarks:
see above at "Version / remarks"
Qualifier:
according to guideline
Guideline:
other: Council Regulation (EC) No. 440/2008, Method C.18 (2008)
GLP compliance:
yes (incl. QA statement)
Type of method:
batch equilibrium method
Media:
soil
Radiolabelling:
no
Test temperature:
Nominal: 20 ± 2 °C
Analytical monitoring:
yes
Details on sampling:
Test Procedure

Test vessels
120 mL disposable glass bottles with aluminium tops with butyl/PTFE seals.
50 mL disposable centrifugation tubes during Tier 1 for soil / solution ratio of 1:40.

Concentration for adsorption / desorption experiments
1.5 mg/L test item; The concentration was found to be suitable for measurements above the limit of quantification of the analytical method (20 µg/L test item) which was assigned with regard to the three analytes.

Stock solutions
A stock solution of 1.5 g/L of the test substance in 50 mL acetonitrile was prepared. 0.1 volume-% (0.1 mL) of this stock solution, related to the volume of the aqueous phase in the soil suspensions, were used for spiking.

Preparation of the soil samples (conditioning)
The soils were weighed into the test vessels and anappropriate volume of 0.01 M CaCl2-solution was added. After agitation overnight (12 h minimum), the samples were used for adsorption experiments.

Preparation of the samples for adsorption experiments
The soil samples were conditioned as described above.0.1 volume-% of the stock solutions, related to the volume of the aqueous phase in the soil suspensions was added in order to adjust the test concentrations. Afterwards, the samples were agitated.

Preparation of the samples for desorption experiments
Samples at adsorption equilibrium were used for this purpose. After completion of the adsorption experiments the test vessels were centrifuged, weighed and the supernatant was replaced by fresh 0.01 M CaCl2-solution. Then the test vessels were agitated again to investigate the desorption behavior of the test item.

Samples for analysis
The soil suspensions were centrifuged after agitation at ≥ 3000 rpm (1881 g) to separate the phases, followed by analysing the concentration of the analytes in aqueous phase by LC-MS/MS. For analysis of the soil, the aqueous phase was decanted and the soil was extracted, if feasible. During Tier 2, test vessels were extracted / rinsed with acetonitrile to determine test vessel adsorption. Extracts were also analysed by LC-MS/MS.

Replicates
All samples were prepared in duplicate.

CONTROLS
CaCl2-solution was conditioned as described above, followed by separation of the aqueous phase by centrifugation and filtration. Then the aqueous phase was fortified acc. to the concentrations used for the test item samples to verify the stability of the test item in the aqueous phase under test conditions. The samples were agitated as long as the test item sample with the longest agitation period.

Replicates
Duplicates


BLANK
Blank samples were prepared for all soils as described for the test item samples but without fortification with the test item. The samples were agitated as long as the samples with the longest agitation period.

Replicates
Duplicates (Tier 1), single (Tier 2 and Tier 3)

Sample Preparation

Dilution medium
Acetonitrile : HPLC-water (50:50)

Standards
A stock solution of 1.5 g/L of Tallow Bis(2-hydroxyethyl) amineoxide in 50 mL acetonitrile was prepared. The solution was diluted to 7 calibration standards in the range of 5 to 100 µg/L with dilution medium.

Aqueous phase
All samples were centrifuged ≥ 3000 rpm (1881 g). An aliquot of each aqueous sample was stabilized by dilution with acetonitrile (factor 2). Samples were diluted to calibration range with dilution medium, if necessary.

Test vessel adsorption
After sampling of the aqueous phase during Tier 1 and Tier 2, the test vessels were emptied and rinsed with demineralized water. Acetonitrile was used for extraction of the test item from the test vessel. Therefore ultrasound was used for 10 min and the vessel was shaken 30 min on a shaker. HPLC-water was used to dilute by factor 2. Acetonitrile : HPLC-water (50:50) was used for further dilutions to calibration range, if necessary.


Soil extraction (Tier 1)
After removal of the aqueous phase, 30 mL acetonitrile containing 1 % trifluoro acetic acid was used to rinse the soil from the test vessel into centrifugation tubes. Ultrasound was used for 15 min and the vessel was shaken 30 min on a shaker. The suspensions were centrifuged at 10000 g for 5 min. The extraction was repeated twice with 20 mL acetonitrile containing 1 % trifluoro acetic acid without using ultrasound. The extracts were transferred quantitatively into a 100 mL measuring flask and filled up with acetonitrile containing 1 % trifluoro acetic acid. HPLC-water was used to dilute by factor 2. Acetonitrile : HPLC-water (50:50) was used for further dilutions to calibration range. Prior to using acetonitrile containing 1 % trifluoro acetic acid the extraction was once conducted containing 2 % formic acid.


Soil extraction (“fresh spikes”)
To prove feasibility of extraction, conditioned soil was spiked with the test item and extracted directly after spiking:
The soil was weighed into 50 mL centrifugation tube and was spiked with the test item. Then the samples were extracted with acetonitrile containing 1 % trifluoro acetic acid. For parameters of the extraction method see above. Extracts were transferred quantitatively into a 100 mL measuring flask and filled up with acetonitrile containing 1 % trifluoro acetic acid. HPLC-water was used to dilute by factor 2. Acetonitrile : HPLC-water (50:50) was used for further dilutions to calibration range.

Samples for method validation
Samples were prepared as described above. The aqueous phases were decanted and spiked with test item at 1 x LOQ level. Additional aqueous phase conditioned with LUFA soil 2.4 was spiked with test item at 10 x LOQ level. All samples were diluted with acetonitrile by factor 2. The samples of 10 x LOQ level were additionally diluted with acetonitrile : HPLC-water (50:50) by factor 10 to calibration range for analysis of Tallow bis(2-hydroxyethyl)amineoxide.
Matrix no.:
#1
Matrix type:
loamy sand
% Clay:
8.5
% Silt:
11.3
% Sand:
80.2
% Org. carbon:
1.47
pH:
7.1
CEC:
7.6 other: mval/100 g
Matrix no.:
#2
Matrix type:
other: silty sand
% Clay:
8.6
% Silt:
29.3
% Sand:
62.1
% Org. carbon:
0.412
pH:
7
CEC:
4.9 other: mval/100 g
Matrix no.:
#3
Matrix type:
clay loam
% Clay:
25.2
% Silt:
42.3
% Sand:
32.6
% Org. carbon:
1.74
pH:
7.2
CEC:
22 other: mval/100 g
Details on matrix:
Relevant Characteristics of Test Matrices

Reason for the selection
The content of organic carbon of the selected soils differ significantly. These matrices are suitable for the conduction of the study because all parameters with impact on the adsorption / desorption behavior of a chemical substance were considered.

Origin of soils
Landwirtschaftliche Untersuchungs- und Forschungsanstalt LUFA Speyer, Obere Langgasse 40, 67346 Speyer, Germany

Storage at test facility
Room temperature, in closed containers

Expiry date
LUFA 2.2 (batch: F2.2 4016): 2021-10-24
LUFA 2.3 (batch: F2.3 4116): 2021-10-24
LUFA 2.4 (batch: F2.4 4116): 2021-10-24
Details on test conditions:
CaCl2 solution:
Deionised water was used to prepare the CaCl2 solution (0.01 M).

Soil / Solution ratio
Tier 1: 1:40 and 1:100
Tier 2 and Tier 3: 1:100

Agitation
By overhead shaker for soil / solution ratio of 1:40.
By horizontal shaker for soil / solution ratio of 1:100.
Frequency was adjusted to avoid sedimentation of soil particles during treatment.

Test temperature:
20 +/- 2 °C 
Key result
Sample No.:
#10
Type:
Kd
Value:
2 517 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2: Loamy sand
% Org. carbon:
1.47
Remarks on result:
other: Mean of three main constituents
Key result
Sample No.:
#11
Type:
Kd
Value:
1 157 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA2.3: Silty sand
% Org. carbon:
0.412
Remarks on result:
other: Mean of three main constituents
Key result
Sample No.:
#12
Type:
Kd
Value:
3 139 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4: Clayey loam
% Org. carbon:
1.74
Remarks on result:
other: Mean of three main constituents
Sample No.:
#1
Type:
Kd
Value:
2 160 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#1
Type:
Koc
Value:
146 959 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#1
Type:
other: Kdes
Value:
2 123 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#2
Type:
Kd
Value:
349 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#2
Type:
Koc
Value:
84 739 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#2
Type:
other: Kdes
Value:
552 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#3
Type:
Kd
Value:
1 151 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#3
Type:
Koc
Value:
66 134 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#3
Type:
other: Kdes
Value:
1 135 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C16 saturated compound
Sample No.:
#4
Type:
Kd
Value:
2 598 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#4
Type:
Koc
Value:
176 714 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#4
Type:
other: Kdes
Value:
2 240 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#5
Type:
Kd
Value:
455 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#5
Type:
Koc
Value:
110 408 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#5
Type:
other: Kdes
Value:
697 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#6
Type:
Kd
Value:
1 454 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#6
Type:
Koc
Value:
83 582 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#6
Type:
other: Kdes
Value:
1 516 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 unsaturated compound
Sample No.:
#7
Type:
Kd
Value:
2 772 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Key result
Sample No.:
#7
Type:
Koc
Value:
188 584 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Sample No.:
#7
Type:
other: Kdes
Value:
1 722 L/kg
pH:
7
Temp.:
20 °C
Matrix:
LUFA 2.2 soil/solution ratio 1:100
% Org. carbon:
1.47
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Sample No.:
#8
Type:
Kd
Value:
2 721 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Sample No.:
#8
Type:
Koc
Value:
660 354 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Sample No.:
#8
Type:
other: Kdes
Value:
3 783 L/kg
pH:
7.3
Temp.:
20 °C
Matrix:
LUFA 2.3 soil/solution ratio 1:100
% Org. carbon:
0.412
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Sample No.:
#9
Type:
Kd
Value:
6 939 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Sample No.:
#9
Type:
Koc
Value:
398 782 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Sample No.:
#9
Type:
other: Kdes
Value:
6 759 L/kg
pH:
8
Temp.:
20 °C
Matrix:
LUFA 2.4 soil/solution ratio 1:100
% Org. carbon:
1.74
Remarks on result:
other: Tallow Bis(2-hydroxyethyl) amineoxide C18 saturated compound
Concentration of test substance at end of adsorption equilibration period:
At an initial test substance concentration of 1.5 mg/L using a soil solution ratio of 1:100 after an equilibrium time of 24 hours
The following concentrations were observed at the end of the equilibration time:
LUFA 2.2: C16: 1.08 µg/L; C18=: 1.04 µg/L; C18: 0.88 µg/L
LUFA 2.3: C16: 5.20 µg/L; C18=: 4.85 µg/L; C18: 0.862 µg/L
LUFE 2.4: C16: 1.99 µg/L; C18=: 1.84 µg/L; C18: 0.367 µg/L
Transformation products:
no

Temperature

The temperature was in the range of 20 ± 2 °C during the course of the study

Soil Dry Weights

The soil dry weight of each soil type used was determined.

 

 Soil Dry Weights

Mean values (n = 3)

 

Soil

LUFA 2.2

LUFA 2.3

LUFA 2.4

soil dry weight [%]

92.3

96.1

90.4

pH Values

The pH values of the aqueous media of the test systems were measured before and after equilibration with the corresponding soils and after addition of the test item. Results are shown in the following table.

 

 pH Values of the Aqueous Media

Soil / Solution Ratio 1:100

 

Soil

 

LUFA 2.2

LUFA 2.3

LUFA 2.4

0.01 M CaCl2

7.1

7.0

7.2

after soil contact

6.9

7.1

7.4

after addition of the test item

7.0

7.3

8.0

 


 

Tier 1 - Adsorption

LUFA 2.2 and LUFA 2.4 were used for preliminary investigations on the adsorption behavior of the test item with soil / solution ratios of 1:40 and 1:100 at a concentration of 1.5 mg/L. An adsorption of ≥ 89% was determined for the three analytes in both soils. The equilibrium of the adsorption was reached after 24 h. Test item control samples (samples without soil) showed that test vessel adsorption is possible. For this reason, test vessel adsorption was taken into account for calculations during adsorption experiments. Concentrations and sampling points for Tier 2 have been assigned based on results in the following tables. A soil / solution ratio of 1:100 was used for the further experiments in Tier 2 and Tier 3 to reduce the test item depletion in the aqueous phase as much as possible.

 

Tier 1: LUFA 2.2 – Soil / Solution Ratios 1:40 and 1:100

Soil / Solution Ratio

Applied concentration, test item [mg/L]

Sampling point [h]

Adsorption
C16:0 Compound [%]

Adsorption
C18:1 Compound [%]

Adsorption
C18:0 Compound [%]

1:40

1.5

24

98

99

96

1:100

1.5

24

95

96

96

 

Tier 1: LUFA 2.4 – Soil / Solution Ratios 1:40 and 1:100

Soil / Solution Ratio

Applied concentration, test item [mg/L]

Sampling point [h]

Adsorption
C16:0 Compound [%]

Adsorption
C18:1 Compound [%]

Adsorption
C18:0 Compound [%]

1:40

1.5

24

99

100

96

1:100

1.5

24

89

92

98


 

Tier 1 - Test Vessel Adsorption

The test item adsorption to the test vessels in test item controls was determined in Tier 1 for the samples with the longest agitation period in polypropylene centrifugation tubes and in glass vials. Adsorption in these samples was lower for all analytes when glass was used. For this reason, glass vials were used for the experiments in Tier 2 and Tier 3. No adsorption on test vessels was observed in the soils suspensions (soil / solution ratio 1:100).

Nevertheless, test vessel adsorption was taken into account for the respective calculations in Tier 2.

 

Tier 1: LUFA 2.2 – Test Vessel Adsorption

Soil / Solution Ratio

Applied concentration, test item [mg/L]

Sampling point [h]

Adsorption
C16:0 Compound [%]

Adsorption
C18:1 Compound [%]

Adsorption
C18:0 Compound [%]

1:100 gl

1.5

24

0

0

0

 

Tier 1:LUFA 2.4 – Test Vessel Adsorption

Soil / Solution Ratio

Applied concentration, test item [mg/L]

Sampling point [h]

Adsorption
C16:0 Compound [%]

Adsorption
C18:1 Compound [%]

Adsorption
C18:0 Compound [%]

1:100 gl

1.5

24

0

0

0

 

Tier 1: LUFA 2.2 – Test Vessel Adsorption – Test Item Control Samples

0.01 M CaCl2was conditioned with LUFA 2.2

Soil / Solution Ratio

Applied concentration, test item [mg/L]

Sampling point [h]

Adsorption
C16:0 Compound [%]

Adsorption
C18:1 Compound [%]

Adsorption
C18:0 Compound [%]

1:40 pp

1.5

24

22

25

41

1:40 gl

1.5

24

10

13

28

1:100 gl

1.5

24

8

9

16


 

Tier 1: LUFA 2.4 – Test Vessel Adsorption – Test Item Control Samples

0.01 M CaCl2was conditioned with LUFA 2.4

Soil / Solution Ratio

Applied concentration, test item [mg/L]

Sampling point [h]

Adsorption
C16:0 Compound [%]

Adsorption
C18:1 Compound [%]

Adsorption
C18:0 Compound [%]

1:40 pp

1.5

24

18

25

43

1:40 gl

1.5

24

10

10

37

1:100 gl

1.5

24

2

2

13

pp                    = 50 mL polypropylene centrifugation tube as test vessel

gl                     = 50 mL disposable glass bottle as test vessel


 

Tier 1 - Extraction from Soil / Mass Balance

Different solvents have been tested for soil extraction during method development (non-GLP). During Tier 1, samples were extracted after 24 h. The best results were achieved with acetonitrile containing 1 % trifluoro acetic acid. In addition, freshly spiked samples were extracted by the same method, to prove feasibility of extraction. Recovery rates of 105% to 110% of the nominal concentration for the analytes from LUFA 2.2 and 100% to 108% from LUFA 2.4 were obtained.

 

Tier 1:Mass Balance LUFA 2.2 Soil / Solution Ratio 1:100
applied test item concentration: 1500 µg/L, n=2

 

Sampling point


[h]

Recovery rate from aqueous phase
[%]

Recovery rate from test vessel2)
[%]

Recovery rate from solid phase
[%]

Mass balance1)

[%]

C16:0 Compound

24 III

6

< LCL

93

95

24 IV

5

< LCL

85

C18:1 Compound

24 III

5

< LCL

91

91

24 IV

4

< LCL

82

C18:0 Compound

24 III

5

0

105

107

24 IV

3

< LCL

101

 

Tier 1: Mass Balance LUFA 2.4 Soil / Solution Ratio 1:100
applied test item concentration: 1500 µg/L, n=2

 

Sampling point


[h]

Recovery rate from aqueous phase
[%]

Recovery rate from test vessel2)
[%]

Recovery rate from solid phase
[%]

Mass balance1)

[%]

C16:0 Compound

24 III

11

< LCL

79

92

24 IV

11

< LCL

84

C18:1 Compound

24 III

8

< LCL

81

90

24 IV

8

< LCL

82

C18:0 Compound

24 III

2

< LCL

98

103

24 IV

2

< LCL

104

III, IV                = replicate number

1)                      =Sum of aqueous phase, solid phase and test vessel, mean value

2)                      = obtained from replicates I and II

< LCL               = measured value below lowest calibration level


 

Tier 2 - Adsorption Kinetics

The determination for adsorption kinetics was performed with a nominal test item concentration of 1.5 mg/L. A soil / solution ratio of 1:100 was used and concentrations of the test item were measured in aqueous phase and in extracts of the test vessels at defined sampling points. The equilibrium was reached within 24 hours. The following tables show the percentage of adsorption at equilibrium, the time needed to reach the adsorption equilibrium as well as the obtained distribution coefficients Kd and their corresponding organic carbon normalized distribution coefficients KOC. The test item shows high adsorption within a few hours to all tested soils.

 

Equilibrium Time, Measured Amounts in Aqueous Phase and Soil Extracts, Percent of Adsorption and Distribution Coefficients Kd, KOC for C16:0 Compound

Applied concentration, test item:          1.5 mg/L

Applied amount, test item:                     150 µg

Applied amount, a.i.:22.6 µg

n = 2; soil / solution ratio: 1:100

Vaq= 100 mL

Soil Type

teq

[h]

msoil

 [g]

madsaq(eq)

[µg]

madss(eq)

[µg]

Kd

[mL/g]

%OC

KOC[mL/g]

Adsorption [%]

LUFA 2.2

24

0.923

1.08

21.6

2160

1.47

146959

95

LUFA 2.3

24

0.961

5.20

17.4

349

0.412

84739

77

LUFA 2.4

24

0.904

1.99

20.7

1151

1.74

66134

91

Vaq            =used volume of aqueous phase

teq              =time to reach equilibrium

msoil          =used amount of soil (dry weight)

madsaq        =amount of a.i. in the aqueous phase at equilibrium

madss          =amount of a.i. in the soil at equilibrium

%OC         =percentage of organic carbon content in the soil


 

Equilibrium Time, Measured Amounts in Aqueous Phase and Soil Extracts, Percent of Adsorption and Distribution Coefficients Kd, KOC for C18:1 Compound

Applied concentration, test item:          1.5 mg/L

Applied amount, test item:                     150 µg

Applied amount, a.i.:26.1 µg

n = 2; soil / solution ratio: 1:100

Vaq= 100 mL

Soil Type

teq

[h]

msoil

[g]

madsaq(eq)

[µg]

madss(eq)

[µg]

Kd[mL/g]

%OC

KOC

[mL/g]

Adsorption [%]

LUFA 2.2

24

0.923

1.04

25.0

2598

1.47

176714

96

LUFA 2.3

24

0.961

4.85

21.2

455

0.412

110408

81

LUFA 2.4

24

0.904

1.84

24.2

1454

1.74

83582

93

 

 

Equilibrium Time, Measured Amounts in Aqueous Phase and Soil Extracts, Percent of Adsorption and Distribution Coefficients Kd, KOC for C18:0 Compound

Applied concentration, test item:          1.5 mg/L

Applied amount, test item:                     150 µg

Applied amount, a.i.:23.4 µg

n = 2; soil / solution ratio: 1:100

Vaq= 100 mL

Soil Type

teq[h]

msoil[g]

madsaq(eq) [µg]

madss(eq) [µg]

Kd[mL/g]

%OC

KOC[mL/g]

Adsorption [%]

LUFA 2.2

24

0.923

0.880

22.5

2772

1.47

188584

96

LUFA 2.3

24

0.961

0.862

22.5

2721

0.412

660354

96

LUFA 2.4

24

0.904

0.367

23.0

6939

1.74

398782

98

Vaq            =used volume of aqueous phase

teq              =time to reach equilibrium

msoil          =used amount of soil (dry weight)

madsaq        =amount of a.i. in the aqueous phase at equilibrium

madss          =amount of a.i. in the soil at equilibrium

%OC         =percentage of organic carbon content in the soil

Tier 3 - Desorption Kinetics

The desorption behavior of the test item was determined after 24 h adsorption. The following tables show the desorption coefficient Kdes. The results show that the test item adsorption is not completely reversible since the desorption is only between 2 % und 16 %. Details are showen in the tables below.

 

Percent of Desorption and Desorption Coefficient Kdes for C16:0 Compound

Applied concentration, test item:          1.5 mg/L

Applied amount, test item:                     150 µg

Applied amount, a.i.:22.6 µg

n = 2; soil / solution ratio: 1:100

Vaq= 100 mL

Soil Type

teq[h]

msoil[g]

mdesaq(eq) [µg]

madss(eq) [µg]

Kdes[mL/g]

Desorption [%]

LUFA 2.2

6

0.923

1.05

21.6

2123

5

LUFA 2.3

2

0.961

2.84

17.9

552

16

LUFA 2.4

2

0.904

1.80

20.3

1135

9


 

Percent of Desorption and Desorption Coefficient Kdes for
C18:1 Compound

Applied concentration, test item:          1.5 mg/L

Applied amount, test item:                     150 µg

Applied amount, a.i.:26.1 µg

n = 2; soil / solution ratio: 1:100

Vaq= 100 mL

Soil Type

teq[h]

msoil[g]

mdesaq(eq) [µg]

madss(eq) [µg]

Kdes[mL/g]

Desorption [%]

LUFA 2.2

6

0.923

1.16

25.1

2240

5

LUFA 2.3

2

0.961

2.79

21.5

697

13

LUFA 2.4

2

0.904

1.63

24.0

1516

7

 

 

Percent of Desorption and Desorption Coefficient Kdes for
C18:0 Compound

Applied concentration, test item:          1.5 mg/L

Applied amount, test item:                     150 µg

Applied amount, a.i.:23.4 µg

n = 2; soil / solution ratio: 1:100

Vaq= 100 mL

Soil Type

teq[h]

msoil[g]

mdesaq(eq) [µg]

madss(eq) [µg]

Kdes[mL/g]

Desorption [%]

LUFA 2.2

6

0.923

1.33

22.5

1722

6

LUFA 2.3

24

0.961

0.609

22.7

3783

3

LUFA 2.4

4

0.904

0.369

22.9

6759

2

Vaq            =used volume of aqueous phase

teq              =time to reach equilibrium

msoil          =used amount of soil (dry weight)

mdesaq        =amount a.i. measured in the aqueous phase after desorption step

(entrained water taken into account)

madss          =amount of a.i. adsorbed to soil at equilibrium

Validity criteria fulfilled:
yes
Conclusions:
Valid guideline study with slightly adapted conditions. Adaptations are justified based on specific type of sorption behaviour of the cationic surfactant. Droge et al 2013 (RSS included) showed that sorption of cationic surfactants is mainly driven by ionic interaction. This explains the non-linear sorption observed. In case non-linear sorption is observed extrapolation to lower environmentally realistic concentrations from a Freundlich isotherm is useless and can lead to erroneous predictions. As an alternative the approach as suggested by the Danish EPA (RSS included) is used where the Kd is determined at a concentration as low as reasonably possible and it is assumed that at this low concentration the Kd can linearly be extrapolated to lower concentrations.
Executive summary:

The adsorption / desorption behavior of Tallow Bis(2 -hydroxyethyl) amineoxide was investigated in three different soils according to OECD guideline 106. Distribution coefficients Kd and organic carbon normalized distribution coefficients KOC were determined with a single concentration. In addition, the desorption behavior / reversibility of the adsorption from the soils was investigated. The distribution coefficients Kdes were calculated for this purpose.

 

RelevantCharacteristics of Test Matrices

 

Soils

 

LUFA 2.2

LUFA 2.3

LUFA 2.4

Soil Type1)

Loamy sand

Silty sand

Clayey loam

pH (0.01 M CaCl2)2)

7.1

7.0

7.2

Organic Carbon [%]3)

1.47

0.412

1.74

Clay (<0.002 mm) [%]3)

8.5

8.6

25.2

Silt (0.002-0.063 mm) [%]3)

11.3

29.3

42.3

Sand (0.063-2 mm) [%]3)

80.2

62.1

32.6

Cation Exchange Capacity [mval/100g]3)

7.6

4.9

22

1)according to German DIN

2) data determined during the course of the study

3)determined at Agrolab Agrar und Umwelt GmbH (non-GLP)

 

Based on results of preliminary investigations during Tier 1, a soil / solution ratio of 1:100 was used for adsorption experiments. Experiments for adsorption and desorption kinetics were conducted with a nominal test item concentration of 1.50 mg/L. Three active ingredients C16-Tallow Bis(2-hydroxyethyl) amineoxide(16:0), C18unsaturated-Tallow Bis(2-hydroxyethyl) amineoxide(18:1) and C18saturated-Tallow Bis(2-hydroxyethyl) amineoxide(18:0) were used as lead components of the test item and were analysed by LC-MS/MS.Data are given for each analyte in this report.

The table below shows obtained distribution coefficients Kd and their corresponding organic carbon normalized distribution coefficients KOC. Furthermore, the mobility of the test item in the investigated matrices was classified according to Mc Call et al(1980). Additionally, the desorption coefficient Kdes ispresented in the summarizing table. A mean weighted average value was calculated for all endpoints. A typical distribution of the lead components of 29.8% (C16:0), 34.3% (C18:1) and 30.8% (C18:0) was considered for this purpose.


 

Summarized Endpoints forTallow Bis(2-hydroxyethyl) amineoxideand the Active Ingredients

Mobility according to Mc Call et al. (1980): KOC 0 – 50 very high, KOC 50 – 150 high, KOC 150 – 500 medium, KOC 500 – 2000 low, KOC 2000 – 5000 slight, KOC > 5000 immobile

 

caq(eq)
[µg/L]

Kd
[mL/g]

KOC
[mL/g]

Kdes
[mL/g]

Mobility according to McCall et al.

Soil/Solution Ratio

1:100

C16:0 Compound

LUFA 2.2

1.08

2160

146959

2123

immobile

LUFA 2.3

5.20

349

84739

552

immobile

LUFA 2.4

1.99

1151

66134

1135

immobile

C18:1 Compound

LUFA 2.2

1.04

2598

176714

2240

immobile

LUFA 2.3

4.85

455

110408

697

immobile

LUFA 2.4

1.84

1454

83582

1516

immobile

C18:0 Compound

LUFA 2.2

0.880

2772

188584

1722

immobile

LUFA 2.3

0.862

2721

660354

3783

immobile

LUFA 2.4

0.367

6939

398782

6759

immobile

Tallow Bis(2-hydroxyethyl) amineoxide– Weighted Average Value

LUFA 2.2

-

2517

171223

2035

immobile

LUFA 2.3

-

1157

280834

1653

immobile

LUFA 2.4

-

3139

180402

3098

immobile

caq(eq)            = concentration in the aqueous phase at adsorption equilibrium; value was calculated for
  Tallow Bis(2-hydroxyethyl) amineoxide from measured
  concentrations of the active ingredients and taking the respective contents into account

 

The results show that Tallow Bis(2 -hydroxyethyl) amineoxide adsorbs strongly to all tested soils with Koc values > 5000 and is therefore considered to be immobile in soils according to Mc Call et al. The desorption was not completely reversible. The Freundlich isotherm was not determined and the adsorption / desorption behavior was investigated based on one test item concentration. These deviations from the guideline were on request of the sponsor and are based on earlier adsorption / desorption studies with cationic surfactants and the conclusions from the Danish EPA (see RSS).

Description of key information

A refined sorption/desorption test according to OECD 106 with tallow bis(2hydroxyethyl)amineoxide resulted in equilibrium constants (Kd's) of 2517, 1157 and 3139 L/kg for loamy sand, silty sand and clayey loam soil. As there is no direct relationship with the sorption behaviour of the substance and the organic carbon content of the soil because other soil properties like the Cation Exchange Capacity and the pH are maybe even more important to predict the sorption behaviour, no Koc's are given.

The mean Kd of 2271 L/kg is used for risk assessment.

 

Key value for chemical safety assessment

Other adsorption coefficients

Type:
log Kp (solids-water in soil)
Value in L/kg:
3.356
at the temperature of:
20 °C

Other adsorption coefficients

Type:
log Kp (solids-water in sediment)
Value in L/kg:
3.356
at the temperature of:
20 °C

Other adsorption coefficients

Type:
log Kp (solids-water in suspended matter)
Value in L/kg:
3.657
at the temperature of:
20 °C

Additional information

Due to the cationic surface-active properties will tallow bis(2 -hydroxyethyl) amineoxide adsorb relatively strongly onto the solid phase of soil and sediments. These substances can adsorb both onto the organic fraction and, dependent on the chemical composition, onto the surface of the mineral phase, where sodium and potassium ions can be exchanged against the alkyl ammonium ion. The determination of a Koc from log Kow is not opportune, because the common equations for Koc derivation are not valid for both ionic and surface active substances.

The sorption test is performed according to OECD 106 with some adaptations. These adaptations are considered justified based on specific type of sorption behaviour of the cationic surfactant. Droge et al 2013 showed that sorption of cationic surfactants is mainly driven by ionic interaction. This type of sorption explains the frequently observed non-linear sorption. In case non-linear sorption is observed extrapolation to lower environmentally realistic concentrations using the Freundlich isotherm is useless and can lead to erroneous predictions. As an alternative the approach as suggested by the Danish EPA is considered to be a better alternative where the Kd is determined at a concentration which is as low as reasonably possible and in addition it is assumed that at this low concentration the Kd can linearly be extrapolated to lower concentrations.  

Relevant Characteristics of the soils used in the sorption/desorption test

 

Soils

 

LUFA 2.2

LUFA 2.3

LUFA 2.4

Soil Type1)

Loamy sand

Silty sand

Clayey loam

pH (0.01 M CaCl2)2)

7.1

7.0

7.2

Organic Carbon [%]3)

1.47

0.412

1.74

Clay (<0.002 mm) [%]3)

8.5

8.6

25.2

Silt (0.002-0.063 mm) [%]3)

11.3

29.3

42.3

Sand (0.063-2 mm) [%]3)

80.2

62.1

32.6

Cation Exchange Capacity [mval/100g]3)

7.6

4.9

22

1)according to German DIN

2) data determined during the course of the study

3)determined at Agrolab Agrar und Umwelt GmbH (non-GLP)

 

Based on results of preliminary investigations during Tier 1, a soil / solution ratio of 1:100 was used for adsorption experiments. Experiments for adsorption and desorption kinetics were conducted with a nominal test concentration of 1.50 mg/L. Three active ingredients C16 -Bis(2 -hydroxyethyl) amineoxide(16:0), C18 unsaturated Bis(2 -hydroxyethyl) amineoxide(18:1) and C18 saturated Bis(2-hydroxyethyl) amineoxide(18:0) were used as lead components of the test item and were analysed by LC-MS/MS.

The table below shows obtained distribution coefficients Kd and their corresponding organic carbon normalized distribution coefficients KOC. As indicated these Koc's will not be used for risk assessment! Furthermore, the mobility of the test item in the investigated matrices was classified according to Mc Call et al(1980). Additionally, the desorption coefficient Kdes is presented in the summarizing table. A mean weighted average value was calculated for all endpoints. A typical distribution of the lead components of 29.8% (C16:0), 34.3% (C18:1) and 30.8% (C18:0) was considered for this purpose.


Summarized Endpoints forTallow Bis(2-hydroxyethyl) amineoxide and the Active Ingredients

Mobility according to Mc Call et al. (1980): KOC 0 – 50 very high, KOC 50 – 150 high, KOC 150 – 500 medium, KOC 500 – 2000 low, KOC 2000 – 5000 slight, KOC > 5000 immobile

 

caq(eq)
[µg/L]

Kd
[mL/g]

KOC
[mL/g]

Kdes
[mL/g]

Mobility according to McCall et al.

Soil/Solution Ratio

1:100

C16:0 Compound

LUFA 2.2

1.08

2160

146959

2123

immobile

LUFA 2.3

5.20

349

84739

552

immobile

LUFA 2.4

1.99

1151

66134

1135

immobile

C18:1 Compound

LUFA 2.2

1.04

2598

176714

2240

immobile

LUFA 2.3

4.85

455

110408

697

immobile

LUFA 2.4

1.84

1454

83582

1516

immobile

C18:0 Compound

LUFA 2.2

0.880

2772

188584

1722

immobile

LUFA 2.3

0.862

2721

660354

3783

immobile

LUFA 2.4

0.367

6939

398782

6759

immobile

Tallow Bis(2-hydroxyethyl) amineoxide– Weighted Average Value

LUFA 2.2

-

2517

171223

2035

immobile

LUFA 2.3

-

1157

280834

1653

immobile

LUFA 2.4

-

3139

180402

3098

immobile

caq(eq) = concentration in the aqueous phase at adsorption equilibrium; value was calculated for Tallow Bis(2-hydroxyethyl) amineoxide from measured   concentrations of the active ingredients and taking the respective contents into account

 

The results show that Tallow Bis(2 -hydroxyethyl) amineoxide adsorbs relatively strongly to all tested soils with Koc values > 5000 L/kg and is therefore considered to be immobile in soils according to Mc Call et al. The desorption was not completely reversible. .

For the prediction of the partitioning of Tallow bis(2 -hydroxyethyl)amineoxide in soil, sediment and suspended matter the mean Kd as observed for the three soils of 2271 L/kg will be used.

Because there is relation of the sorption of Tallow bis(2 -hydroxyethyl)amineoxide to the organic carbon fraction allone there will be also no principal difference between the sorption to soil and sediments considering the sorption properties. The Kd value for soil will also be used for sediment and suspended particles.

In the table below the distribution constants used in this assessment is summarized:

Distribution constants to be used for Tallow bis(2 -hydroxyethyl)amineoxide

Kpsoil

2271 L/kg

Ksoil-water

3406.5 m3/m3

Kpsusp

4542 L/kg

Ksusp-water

1135.5 m3/m3

Kpsed

2271 L/kg

Ksed-water

1135.5 m3/m3

 

With a Kpsuspof 4542 L/kg and a concentration of 15 mg/L suspended matter in surface waters, the adsorbed fraction is calculated as 6.4%.