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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 />

acid brown soil, silty clay loam, stand = Picea abies,<br />

aluminium buffer range, C/N 17.0, past N input 37.1 kg/ha/a,<br />

pHH2O 3.3.and Wekerom (NL) - Podsol soil, sand, stand = Pinus<br />

sylvestris, aluminium buffer range, C 22.0, past N input 52.1<br />

kg/ha/a, pHH2O 3.9.Cation exchange capacity and base<br />

saturation information can be found in the paper.<br />

Lysimeters were prepared from soil cores (14 cm inner<br />

diameter and 24 cm deep) taken at each site in Plexiglas<br />

cylinders. The bases of the cores were trimmed, and a 5 cm<br />

deep layer of acid washed sand was placed at the bottom of<br />

each core, which was then capped and sealed.<br />

A ceramic cup conected to a suction apparatus was inserted<br />

diagonally into the sand layer, and the join with the cykinder<br />

was sealed.<br />

The throughfall solution was removed through the ceramic cup<br />

during the experiment. 28 lysimeters were installed at each<br />

site, using a randomised block design. The lysimeters were<br />

roofed to enable control of throughfall inputs. One half of<br />

the lysimeters contained carefully inserted living tree roots.<br />

Throughfall applications consisting of the throughfall<br />

volumes of each individual site, collected and measured for<br />

the period, with the addition of 75 kg ha-1-a-1 (NH4)2SO4<br />

for the N treatments, were made to each lysimeter at 2 week<br />

intervals. The leachates were collected every 2 weeks, for 1<br />

year from September 1992, and analysed for volume, pH, and<br />

major cations and anions.<br />

Result:<br />

Soil texture and pH were important in controlling NH4+<br />

leaching. The two less acidic, clay/clay loam soils showed<br />

almost total retention of NH4+. Nearly 75% of added N was<br />

leached as NH4+ in the acid sandy soils. The presence of<br />

living roots significantly reduced soil solution nitrate and<br />

associated cation concentrations at two of the six sites.<br />

The very different responses of the six soils to increased<br />

(NH4)2SO4 deposition emphasises that the establishment of N<br />

critical loads for forest soils needs to allow for<br />

differences in the N storage capacity and nitrification<br />

potential of the soils<br />

Test substance: ammonium sulfate (NH4)2SO4, not specified further<br />

Reliability: (2) valid with restrictions<br />

study well documented and assignable<br />

Flag:<br />

Critical study for SIDS endpoint<br />

04-JUN-<strong>20</strong>04 (46) (47)<br />

3.3.1 Transport between Environmental Compartments<br />

Type:<br />

Media:<br />

adsorption<br />

water - sediment<br />

Result: log Koc = 1.38 (Koc = 24)<br />

Reliability: (2) valid with restrictions<br />

accepted calculation method<br />

Flag:<br />

Critical study for SIDS endpoint<br />

27-JAN-<strong>20</strong>04 (16)<br />

Media:<br />

Method:<br />

Remark:<br />

74<br />

soil - air<br />

other: measured<br />

1) This is a static test, so less ammonia will be removed<br />

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