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Lab #8 - 11/22/04 |
| I. Objectives: | |||
| a.) To follow
changes in nitrogen over time after
addition of ammonium (NH4+) on the three soils. Extract iron (Fe) and manganese (Mn) from soils and soil fractions using the acidified oxalate method. |
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| II. Nitrification Procedure | |||
| 1.) Weigh out
2.0 g (in duplicate) aliquots of your air-dried soil into two 30 mL
Nalgene plastic bottles. Add a clean stir bar. |
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| 2.) Add 20 mL
of deionized water. Stir for 10 minutes. Pull a 2 mL blank
suspension sample while stirring and record initial pH. |
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| 3.) From a
0.1 M NH4Cl stock solution, add the calculated amount of
stock solution
needed to achieve an initial NH4+ of 1 mM without changing the solid:solution ratio. The “time zero” will coincide with the emptying of the pipette carrying the NH4+ stock solution. |
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| 4.) Bottles
will be shaken on the Big Bill shaker and 2 mL suspension samples
removed at 1h, 2h, 24h, 48h, 96h, and 168h (one week). |
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| 5.) Measure
equilibrium pH using a calibrated pH meter during sampling. |
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| 6.) The
reaction between NH4+
and soil will be stopped by filtration with 0.2µm
pore size membrane filters using 25 mm filter holders and 10 mL syringes into labeled test tubes. |
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| 7.) Store
filtrates in labeled test tubes in the refrigerator. The
concentrations of NH4+, NO3-,
and NO2- will be measured in the filtrates using colorimetic methods. |
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| III. Fe and Mn Extractions (McKeague and Day, 1966). | |||
| 1.)
Weigh out 0.50 g (in duplicate) aliquots of your air-dried soil and
0.10 g aliquots of each fraction (feel free to readjust this weight depending on the amount of fraction remaining) in 40 mL centrifuge tubes (this should be a total of 8 tubes per group). |
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| 2.)
Add 10 mL of 0.2 M (NH4)2C2O4
buffered to pH 4.0. |
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| 3.)
Wrap in aluminum foil and shake for 24 h. |
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| 4.)
Separate the solid from solution by centrifugation and/or filtration. |
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| 5.)
Total Fe and Mn will be measured using FAAS. |
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| IX.)
References:
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McKeague, J.A. and J.H. Day.
1966. Dithionite and oxalate-extractable Fe and Al as aids in
differentiating various classes of soils. Can. J. Soil Sci.
46:13-22. |
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