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Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...

Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...

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MATERIALS AND METHODS<br />

Bulk density: Bulk density is determined by drying a known volume (100 cc)<br />

<strong>of</strong> undisturbed soil at 105°C, after which <strong>the</strong> oven-dry weight <strong>of</strong> <strong>the</strong><br />

soil is divided by <strong>the</strong> volume <strong>of</strong> <strong>the</strong> soil.<br />

Calcium carbonate: (according to Van Wesemael; only in samples with<br />

pH(H20) > 6.5). Gravimetric determination <strong>of</strong> <strong>the</strong> loss <strong>of</strong> weight, after<br />

treatment with 4N HC104.<br />

CEC(-NH40Ac): For <strong>the</strong> cation exchange capacity, <strong>the</strong> sample is leached<br />

subsequently with 1 M ammonium acetate at pH 7.0. 80% ethanol to<br />

wash out <strong>the</strong> excess <strong>of</strong> ammonium and 10% KG at pH 2.5 to replace<br />

<strong>the</strong> absorbed ammonium. In <strong>the</strong> leachate, ammonium is determined<br />

by distillation and titration.<br />

EC (1:2.5): The electrical conductivity is measured in a 1:2.5 soil-water<br />

extract.<br />

Exchangeable acidity/aluminium: (only in samples with pH < 5.5). The soil is<br />

leached with 1 M KC1. Exchangeable acidity (Al + H) and aluminium are<br />

determined titrimetrically.<br />

Exchangeable bases: Exchangeable Na and K are determined flamephotometrically<br />

in <strong>the</strong> leachate <strong>of</strong> <strong>the</strong> CEC-determination.<br />

Exchangeable Ca and Mg are determined in <strong>the</strong> same leachate using an<br />

atomic absorption spectro-photometer.<br />

Organic carbon: (according to Walkley and Black). Organic matter is oxidized<br />

with an excess <strong>of</strong> potassium dichromate in an acid medium. The excess<br />

is back-titrated with ferrous ammonium sulphate.<br />

Particle size analysis: (pipette method). The sample is pre-treated with H2O2<br />

and sodium acetate, in order to remove organic matter and CaC03.<br />

After dispersing with Na-hexametaphosphate, <strong>the</strong> clay and silt<br />

fractions are calculated for samples, taken from <strong>the</strong> suspension with a<br />

pipette. The total sand fraction is determined by wet sieving; <strong>the</strong><br />

different sand fractions are determined after dry sieving.<br />

pH (H2O): Potentiometric determination in a 1:2.5 soil-water suspension.<br />

pH (KG): Potentiometric determination in a 1:2.5 soil-1 M KG suspension.<br />

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