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Acid fumigation of soils to remove carbonates prior to total organic carbon or CARBON‐13 isotopic analysis

Soil Science Society of America Journal · 2001 · Vol. 65(6) · pp. 1853–1856
David J. HarrisWilliam R. HorwáthChris van Kessel

Abstract

The use of 13 C natural abundance (δ 13 C) to follow C input to soil has gained widespread acceptance. However, inorganic C present in the soil as carbonates will interfere with the measurement of soil organic 13 C unless removed or excluded from measurement. We report a simple and convenient HCl‐fumigation method to remove inorganic C from soil. Soil samples are weighed in Ag‐foil capsules, arranged on a microtiter plate, wetted with water to approximately field capacity, and placed in a desiccator containing a beaker with concentrated (12 M ) HCl. The carbonates are released as CO 2 by the acid treatment in 6 to 8 h. The soil samples are then dried at 60°C prior to isotope determination. The advantages of the HCl‐fumigation method to remove inorganic C from the soil are that: (i) no water soluble C will be lost from the soil; (ii) a large number of samples can be processed simultaneously; (iii) the removal of inorganic C is rapid and complete; and (iv) the method could also be used to determine both organic and inorganic C content in the soil. A potential disadvantage, however, is that the HCl fumigation changed the 15 N natural abundance of soil N.

Isotope Analysis in EcologyGroundwater and Isotope GeochemistrySoil Carbon and Nitrogen DynamicsFumigationSoil waterEnvironmental chemistryChemistrySoil testTotal organic carbonDissolved organic carbonEnvironmental scienceSoil scienceAgronomy
Citations
1,280
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4.40
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15
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94%
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References
Carbon and nitrogen determinations of carbonate‐containing solids1
Limnology and Oceanography · 1984 · 1,294 citations
Controls on Natural Nitrogen‐15 and Carbon‐13 Abundances in Forest Soil Organic Matter
Soil Science Society of America Journal · 1988 · 945 citations
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