AMMONIUM SULFATE CAS N°: 7783-20-2
AMMONIUM SULFATE CAS N°: 7783-20-2
AMMONIUM SULFATE CAS N°: 7783-20-2
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OECD SIDS<br />
<strong>AMMONIUM</strong> <strong>SULFATE</strong><br />
3. ENVIRONMENTAL FATE AND PATHWAYS ID: <strong>7783</strong>-<strong>20</strong>-2<br />
DATE: 18.04.<strong>20</strong>06<br />
<strong>20</strong>03).<br />
Reliability: (2) valid with restrictions<br />
18-APR-<strong>20</strong>06 (33) (34) (11) (12) (35)<br />
Type of measurement: other<br />
Medium:<br />
food<br />
Remark:<br />
Small amounts of ammonium sulfate are used in food/food<br />
stuff additives. Average amounts used were reported as<br />
0.033% in baked goods, and as 0.075% in gelatins, puddings,<br />
and custard.<br />
Reliability: (4) not assignable<br />
secondary citation<br />
21-APR-<strong>20</strong>03 (36)<br />
3.2.2 Field Studies<br />
Type of measurement: other: Leaching from soil- laboratory or greenhouse<br />
experiments<br />
Media:<br />
Leachate from lysimeter<br />
Method:<br />
Remark:<br />
Result:<br />
68<br />
Artificial soil profiles were constructed in PVC cylinders<br />
(155 mm inner diameter), with bottom plates and 15 µm pore<br />
size suction filters connected to an Erlenmeyer flask for<br />
leachate removal. The parent soil was a glacial till with<br />
sand and fine sand dominating, which had received 110 kg N<br />
ha-1 yr--1 ammonium nitrate as fertiliser for <strong>20</strong> years.<br />
The profiles consisted of 50 mm O (O: humus; 43%C, 1.3%N, pH<br />
H2O 4.1) and 100 mm E (2.9% C, 0.10%N, pH H2O 4.4) horizons (A<br />
columns), or 50 mm O (43% C, 1.3%N, pH H2O 4.1), 100 mm E<br />
(2.9% C, 0.10%N, pH H2O 4.4) and 100 mm B (2.5% C, 0.10%N, pH<br />
H2O 4.9) horizons (B columns).<br />
4 replicates were run for each experimental situation, which<br />
comprised bare and vegetated soil (grass, and ammonium sulfate<br />
at 0.0025 (control), 0.25,and 0.5 mM/l and 2 profile depths.<br />
Irrigation was performed manually at irregular intervals,<br />
generally about once a week, as intense rain showers of 5.3<br />
mm. Just before sampling the irrigation rate was increased to<br />
5.3 mm per day, to make leachate collection possible.<br />
These laboratory or greenhouse experiments with repacked<br />
soil all demonstrate that soil texture, clay content, and pH<br />
are important in controlling NH4+ leaching, with more<br />
leaching occurring with sandy soils at a low pH. The ionic<br />
strength of the irrigation water may also be important, as<br />
may be the level of application of ammonium sulfate. More<br />
leaching is observed from bare soil than in the presence of<br />
crops.<br />
In the absence of vegetation up to 80 % of applied NH4+ was<br />
recovered in the leachate in the A columns (O and E horizons<br />
only) for the higher level (0.5mM) ammonium sulfate solution.<br />
In the presence of vegetation, up to 50% of applied NH4+ was<br />
recovered in the leachate. At the lower level (0.25 mmM) of<br />
application very little NH4+ was<br />
recovered in the leachate, in both the presence and the<br />
absence of vegetation. The B columns, which contained soil<br />
from the B horizon as well as from the O and E horizons,<br />
showed reduced NH4+ in the leachate, with only about 30% of<br />
NH4+ being found in leachate for the 0.5 mM application in<br />
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