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

被引:982
作者
Harris, D
Horwáth, WR
van Kessel, C [1 ]
机构
[1] Univ Calif Davis, Dept Agron & Range Sci, Davis, CA 95616 USA
[2] Univ Calif Davis, Stable Isotope Lab, Davis, CA 95616 USA
[3] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA
关键词
D O I
10.2136/sssaj2001.1853
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The use of C-13 natural abundance (delta C-13) 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 C-13 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 microliter 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 CO2 by the acid treatment in 6 to 8 It. The soil samples are then dried at 60 degreesC 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 N-15 natural abundance of soil N.
引用
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页码:1853 / 1856
页数:4
相关论文
共 18 条
[1]  
Balesdent J., 1996, Mass spectrometry of soils., P83
[2]   SOIL ORGANIC-MATTER TURNOVER IN LONG-TERM FIELD EXPERIMENTS AS REVEALED BY C-13 NATURAL ABUNDANCE [J].
BALESDENT, J ;
WAGNER, GH ;
MARIOTTI, A .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1988, 52 (01) :118-124
[3]  
BOUTTON T W, 1991, P173
[4]   Soil carbon dynamics in corn-based agroecosystems: Results from carbon-13 natural abundance [J].
Collins, HP ;
Blevins, RL ;
Bundy, LG ;
Christenson, DR ;
Dick, WA ;
Huggins, DR ;
Paul, EA .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1999, 63 (03) :584-591
[5]   Carbon isotopes reveal soil organic matter dynamics following arid land shrub expansion [J].
Connin, SL ;
Virginia, RA ;
Chamberlain, CP .
OECOLOGIA, 1997, 110 (03) :374-386
[6]   CARBON AND NITROGEN DETERMINATIONS OF CARBONATE-CONTAINING SOLIDS [J].
HEDGES, JI ;
STERN, JH .
LIMNOLOGY AND OCEANOGRAPHY, 1984, 29 (03) :657-663
[7]   CARBON-ISOTOPE DYNAMICS OF FREE-AIR CO2-ENRICHED COTTON AND SOILS [J].
LEAVITT, SW ;
PAUL, EA ;
KIMBALL, BA ;
HENDREY, GR ;
MAUNEY, JR ;
RAUSCHKOLB, R ;
ROGERS, H ;
LEWIN, KF ;
NAGY, J ;
PINTER, PJ ;
JOHNSON, HB .
AGRICULTURAL AND FOREST METEOROLOGY, 1994, 70 (1-4) :87-101
[8]   Carbonate removal by acidification causes loss of nitrogenous compounds in continental margin sediments [J].
Lohse, L ;
Kloosterhuis, RT ;
de Stigter, HC ;
Helder, W ;
van Raaphorst, W ;
van Weering, TCE .
MARINE CHEMISTRY, 2000, 69 (3-4) :193-201
[9]   Soil carbonate decomposition by acid has little effect on δ13C of organic matter [J].
Midwood, AJ ;
Boutton, TW .
SOIL BIOLOGY & BIOCHEMISTRY, 1998, 30 (10-11) :1301-1307
[10]  
MUNN JR, 1981, 10007 USDA SCS U CAL