Methodological uncertainty in estimating carbon turnover times of soil fractions. (September 2016)

• Record Type: Journal Article
• Authors: Feng, Wenting; Shi, Zheng; Jiang, Jiang; Xia, Jianyang; Liang, Junyi; Zhou, Jizhong; Luo, Yiqi
• Is Part Of: Soil biology and biochemistry. Volume 100(2016)
• Page Start: 118
• Page End: 124
• Publication Date: 2016-09
• Subjects: Soil organic carbon -- Turnover -- 13C -- 14C -- Incubation -- Fraction; Soil biochemistry -- Periodicals; Soil biology -- Periodicals; Sols -- Biochimie -- Périodiques; Sols -- Biologie -- Périodiques; Sols -- Microbiologie -- Périodiques; Bodembiologie; Biochemie; 631.46
• DOI: 10.1016/j.soilbio.2016.06.003
• Languages: English
• ISSNs: 0038-0717

Abstract

Abstract: Improving predictions of soil organic carbon (SOC) dynamics by multi-compartment models requires validation of turnover times of different SOC pools. Techniques such as laboratory incubation and isotope analysis have been adopted to estimate C turnover times, yet no studies have systematically compared these techniques and assessed the uncertainties associated with them. Here, we tested whether C turnover times of soil fractions were biased by methodology, and how this changed across soil particle sizes and ecosystems. We identified 52 studies that quantified C turnover times in different soil particles fractionated either according to aggregate size ( e.g., macro- versus micro-aggregates) or according to soil texture ( e.g., sand versus silt versus clay). C turnover times of these soil fractions were estimated by one of three methods: laboratory incubation (16 studies), δ 13 C shift due to C3 –C4 vegetation change (25 studies), and 14 C dating (19 studies). All methods showed that C turnover times of soil fractions generally increase with decreasing soil particle size. However, estimates of C turnover times within soil fractions differed significantly among methods, with incubation estimating the shortest turnover times and 14 C the longest. The short C turnover times estimated by incubation are likely due to optimal environmental conditions for microbial decomposition existing in these studies, which is often a poor representation of field conditions. The 13 C method can only be used when documenting a successive C3 versus C4 vegetation shift. C turnover times estimated by 14 C were systematically higher than those estimated by 13 C, especially for fine soil fractions ( i.e., silt and clay). Overall, our findings highlight methodological uncertainties in estimating C turnover times of soil fractions, and correction factors should be explored to account for methodological bias when C turnover times estimated from different methods are used to parameterize soil C models. Graphical abstract: Highlights: C turnover times of soil fractions differ significantly among estimate methods. C turnover times of soil fractions generally follow the order: incubation < 13 C < 14 C. C turnover times of soil fractions: 14 C conventional model > 14 C bomb model. All methods show C turnover times of soil fractions rise with decreasing particle size.