Acid pre-analysis treatment: methods and effects
Researchers interested in the organic carbon fraction of bulk samples typically must remove carbonate prior to analysis. This post focuses on important considerations and limitations associated with carbonate removal.Elemental analysis (EA) of bulk material will convert almost any carbon into carbon dioxide (CO2) whether it is from an organic or inorganic (e.g. carbonate) source. The presence of carbonate will inflate the total amount of carbon as well as severely bias the stable carbon isotope value (13C). Terrestrial carbonates typically have more 13C present relative to 12C, making the carbon isotope ratio, expressed as δ13C, more positive or "heavier". Organic carbon typically has a reduced amount of 13C relative to 12C, i.e. a more negative δ13C. In any case, the organic carbon and carbonate carbon will most likely have different isotopic compositions and they must be separated or analyzed in such a way so that the presence of one does not affect the measurement of the other.
Researchers typically use an acid to remove the carbonate. The species and strength of acid should be considered. While the dominant reaction is the conversion of carbonate to CO2 and H2O, organic carbon species can be impacted to a measurable extent by, for example, washing away soluble organic compounds. Also, typical EA of carbon has historically included the analysis of nitrogen. All nitrogen present in a bulk sample will be converted to N2 during EA for total and/or isotope abundance. The soluble nitrogen species present in a bulk sample can also be washed away during acid pretreatment and / or can react with the the acid leading to measurable effects. Many researchers have described how acid pretreatment, also referred to as acidification, affects their samples.
The purpose of this post is to survey studies that directly compared methods of carbonate removal in an attempt to document the effect of the method itself. Many many publications exist on different approaches for removal of, or separation of, carbonate carbon from organic carbon. These studies are typically geared towards the immediate sample type of interest. Your samples will very likely have a different composition and this is an important consideration when choosing a method. This is not meant to be an exhaustive review, but rather a taste of how complicated this issue is.
Broad Methodology
Selective roasting - This approach aims to heat samples to a lower temperature (e.g. 500 °C) to drive off organics and then at a higher temperature (e.g. 1000 °C) to quantify carbonate. The difference between the higher temperature treatment and the lower temperature treatment provides an estimate of total organic carbon (TOC). The overlapping loss of some carbonate as well as incomplete removal of organic carbon at the lower temperature make this method problematic (Froelich 1980; Weliky et al. 1983). This method is not recommended and is included here for completeness.
Acid Washing - This method involves a large amount of sample in a reaction vessel or test tube typically with dilute acid, sonication, soaking or otherwise incubating while effervescence continues, followed by rinsing with purified water. Take care to ensure you know the particular carbonate species that is present in your samples (e.g., siderite Vinduskova et al. 2019). This method does well at retaining the insoluble, non-volatile portion of the sample while removing the carbonate portion. However it also guarantees the removal of any soluble organic carbon and nitrogen (CN) or volatilized CN compounds. Researchers have reported using hydrochloric acid (HCl), phosphoric acid (H3PO4), and sulfurous acid (H2SO3) (reviewed and tested in Brodie et al. 2011a). Both Froelich (1980) and Weliky et al. (1983) demonstrate the presence of dissolved organic carbon in solution after sample reaction with H3PO4. Loss of organic carbon in the soluble fraction ranged from 5 to 45% (Froelich 1980). Despite potential losses in the liquid phase, Midwood and Boulton (1998) tested four HCl concentrations and incubation durations on two distinct soils and show that δ13C was largely unaffected; TOC and total N, however were still affected to varying degrees. Mazumder et al. (2010) also show disparate effects of acid washing on CN, δ13C and δ15N depending on the sample type.
In-capsule aqueous acidification - In an effort to harness the decarbonating potential of acid solution but trying to limit losses due to repeated washing and rinsing, an in-capsule aqueous acidification reaction is allowed to proceed in a silver sample capsule (tin capsules degrade in the presence of acid; so do silver capsules if the experiment runs too long). The sample material inside the capsules is never rinsed and the liquid phase evaporates away after effervescence is finished. Nieuwenhuize et al. (1997) show in-capsule acidification using 25 % HCl exhibits no detectable loss of organic carbon when compared with an alternative method. However, Lohse et al. (2000) demonstrate loss of nitrogen using in-capsule aqueous acidification when compared with no acid treatment. More recently, Kazanidis et al. (2019) demonstrate biases in conclusions when acid pretreated samples vs untreated samples are considered.
In-capsule acid fumigation - Another attempt at driving away carbonate using acidification is via the vapor phase of HCl. Here samples are loaded into silver capsules and placed in a sealed container with a reservoir of 12N HCl. Gaseous HCl reacts with carbonate to form CO2 and H2O but does not have an aqueous phase to dissolve any organic C or N. Hedges and Stern (1984) compare this method to a method similar to the acid washing approach without the decanting. That is, they add 1 N HCl and sample material to a reaction vessel but then allow all of the liquid to evaporate at 50 °C. This method, too, avoids loss of material in the liquid phase. In this way, their acid washing method is more like a large-scale in-capsule aqueous acidification. Komada et al. (2008) recommend in-capsule acid fumigation after observing better accuracy and precision as well as reduced labor compared with in-capsule aqueous acidification. They also caution against long fumigations and recommend 6 hours. However, if your samples contain siderite (iron carbonate) or an otherwise difficult to digest carbonate species, you may have to use in-capsule aqueous acidification with stronger concentrations and correct for any losses or effects of said treatment (Larson et al. 2008). Lorrain et al. (2003) successfully used fumigation to decarbonate particle filters while leaving the TOC, total N, δ13C and δ15N unaltered.
Nitrogen
It is important to recognize that while you are interested in removing carbonate to hedge towards better organic carbon data, acid pre-treatment also affects your nitrogen data (Lohse et al, 2000; Harris et al. 2001; Walthert et al. 2010, Brodie et al, 2011b and c). Mateo et al. (2008) is an impressive compilation of published analyses showing that broad effects of acid washing affect δ15N of marine invertebrates. Acid washing could be removing nitrogen in the same way as organic carbon but it could also be leaving behind nitrogen present in the acid (Wolman and Miller, 1971). Assuming you can achieve complete combustion during your analyses, the best approach is to obtain your nitrogen data with untreated sample material (Kazanidis et al. 2019).
Recommendations
With hundreds to thousands of papers reporting acid-pretreatment of samples and a fraction of those attempting to document the effect of their treatment on the measurement of interest, you may still end up justified in thinking you have a unique sample composition and thus no real direction on how to proceed. Brodie et al. have a collection of three papers from 2011 that provide a thorough review of the above three acidification methods and the affect on CN amounts and δ13C and δ15N. If you are going to read only a paper or two, start with the Brodie series. In the end, the only recommendation is to accept a compromise. Know your samples and know that treating them with acid will affect your results in more ways that removing the carbonate. The reason your percent carbonate results differ when you compare acid washing to methods using CO2 yield (e.g., Kiel carbonate device), for example, become apparent when you consider forty years of decarbonating.References
- Brodie CR, Leng MJ, Casford JSL, Kendrick CP, Lloyd JM, Yongqiang Z, Bird MI. (2011a). Evidence for bias in C and N concentrations and [delta] 13C composition of terrestrial and aquatic organic materials due to pre-analysis acid preparation methods. Chemical Geology. 282. doi: 10.1016/j.chemgeo.2011.01.007.
- Brodie CR, Casford JSL, Lloyd JM, Leng MJ, Heaton THE, Kendrick CP, Yongqiang Z. (2011b). Evidence for bias in C/N, δ13C and δ15N values of bulk organic matter, and on environmental interpretation, from a lake sedimentary sequence by pre-analysis acid treatment methods. Quaternary Science Reviews 30. doi: 10.1016/j.quascirev.2011.07.003.
- Brodie CR, Heaton THE, Leng MJ, Kendrick CP, Casford JSL, Lloyd JM. (2011c). Evidence for bias in measured δ15N values of terrestrial and aquatic organic materials due to pre-analysis acid treatment methods. Rapid Communications in Mass Spectrometry 25. 1089–1099. doi: 10.1002/rcm.4970
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