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 />
pelletized 15N labelled ammonium sulfate fertiliser to the<br />
West Bear Brook catchment, from June 1991 until December 1992<br />
(1991: 21 kg N/ha, 1992: 42 kg/ha). This was part of an<br />
experiment involving otherwise unlabelled ammonium sulfate<br />
fertiliser application at the same level, which has run from<br />
1989 to 1996. The nearby East Bear Brook catchment, with no<br />
fertiliser application, was used as a control.<br />
Remark:<br />
Further information on soil characterisation may be<br />
available in Norton et al (1999), in Environmental<br />
Monitoring and Assessment 55 (page not given).<br />
Result:<br />
Analysis of stream water established that the 1.5 year<br />
(1991-1993) cumulative exports of fertiliser-derived<br />
ammonium represented less than 1% of the labelled fertiliser<br />
added to the catchment. Nitrate plus ammonium exports<br />
contained ca. 2 kg N/ha of the 42 N kg/ha<br />
deposited.<br />
Test substance: Commercial pelletised ammonium sulfate fertiliser, enriched<br />
in 15N at the Tenessee Valley Authority laboratory by<br />
dissolution of the pellets in water, addition of (15NH4)2SO4<br />
into the fertiliser solution, and repelletizing the<br />
precipitated, labelled fertiliser.<br />
Reliability: (1) valid without restriction<br />
study well documented and assignable<br />
28-MAY-<strong>20</strong>04 (41)<br />
Type of measurement: other<br />
Media:<br />
soil<br />
Result: In two soils treated with ammonium sulfate at rates of 0,<br />
25, 50, 100 and 150 mg N/kg ammonium was rapidly converted<br />
to nitrate. In Tifton soil (fine loamy, siliceous, thermic<br />
Plinthic Paleudults) practically all ammonium had<br />
disappeared by day 22, whilst nitrification in Dothan soil,<br />
a fine loamy, siliceous, thermic Typic Hapludults, was much<br />
slower, and almost stopped by day 30. This difference<br />
between soils was probably due to differences in soil pH and<br />
buffer capacity. Tifton soil had an initial pH of 6.8,<br />
wihich is considered to be close to the optimum for<br />
nitrification. In contrast, Dothan soil had an initial pH of<br />
5.5, providing a much less favorable environment for<br />
nitrification. Nitrification in Dothan soil stopped when thepH<br />
approximated a value of 4.5.<br />
Test condition: temperature: 30 °C<br />
test duration: 40 d in quadruplicate<br />
air change: each 2. day<br />
Reliability: (1) valid without restriction<br />
study well documented and assignable<br />
28-MAY-<strong>20</strong>04 (42)<br />
Type of measurement: other: laboratory study<br />
Media:<br />
soil-air<br />
Remark:<br />
1) This is a static test, so less ammonia will be removed<br />
than in a flow through test.<br />
2) This reference also cites other papers which give ammonia<br />
losses from fertilisers and liquid sludges applied to soils<br />
of up to 60%. The ammonia volatilisation is dependent upon<br />
the pH of the soil and mode of application, with subsurface<br />
application having greatly reduced ammonia loss from soil.<br />
UNEP PUBLICATIONS 71