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An improved method for quantifying sedimentary charcoal via a volume proxy

Chengyu Weng

Department of Biological Sciences, Florida Institute of Technology, Melbourne, Florida 32901, USA; Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Kruislaan 318, 1098 SM Amsterdam, The Netherlands weng{at}science.uva.nl

In charcoal analysis, number and area of charcoal particles are the most commonly measured parameters. However, neither measurement is precise as charcoal fragments can be broken into smaller pieces during preservation and laboratory processing, and then both number and apparent area will increase. Volume is a more reliable parameter than area to represent charcoal amount but is difficult to measure. However, a simple approximation provides a stable and reliable proxy estimate of charcoal volume. By applying the formula CIA3/2 (where C is a constant, Ai is area of a charcoal particle, and I means sum), measures of area are shown to be convertible to volume. The constant may be estimated empirically if enough experimental data are available. Even if C is not precisely quantifiable, the application of XA312 as a stable parameter provides a good first approximation to measurements of convert area to estimates of volume. Empirical experiments demonstrate that volume estimates reduce the error induced by fragmentation or loss of tiny pieces during processing or measuring.

Key Words: Charcoal analysis • charcoal volume • particle size • charcoal area • fire history

The Holocene, Vol. 15, No. 2, 298-301 (2005)
DOI: 10.1191/0959683605hl795rr


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This article has been cited by other articles:


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C. Carcaillet, A.-S. Perroux, A. Genries, and Y. Perrette
Sedimentary charcoal pattern in a karstic underground lake, Vercors massif, French Alps: implications for palaeo-fire history
The Holocene, September 1, 2007; 17(6): 845 - 850.
[Abstract] [PDF]


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The HoloceneHome page
W. Tinner, S. Hofstetter, F. Zeugin, M. Conedera, T. Wohlgemuth, L. Zimmermann, and R. Zweifel
Long-distance transport of macroscopic charcoal by an intensive crown fire in the Swiss Alps - implications for fire history reconstruction
The Holocene, February 1, 2006; 16(2): 287 - 292.
[Abstract] [PDF]