Abstract

Our understanding of the cycling of fire-derived, i.e. pyrogenic organic matter (pyOM), as well as the goals of the community of researchers who study it, may be inhibited by the many terms and methods currently used in its quantification and characterization. Terms currently used for pyOM have evolved by convention, but are often poorly defined. Further, each of the different methods now used to quantify solid and dissolved pyrogenic carbon (pyC) comes with its own biases and artifacts. That is, each detects only a fraction of the total pyrogenic products produced by fire, while, at the same time, include some fraction of non-pyrogenic OM. This may be evident in the commonly observed correlations between pyC and total organic C reported for both soils and dissolved OM in many different systems. We suggest that our research area can be placed on a stronger footing by: 1) agreement upon a common set of terms tied to the method used for detection (e.g. of the form pyCmethod), 2) implementation of another ‘ring trial’ study with a wider set of natural soil and water samples that cross-compare more recently developed methods, and 3) further investigation of the processes which preserve/degrade/transport pyOM in the environment.

Highlights

  • The understanding that fire and pyrogenic organic matter have contributed to shaping Earth’s biosphere is one that has evolved within a number of disparate fields including geology, ecology, atmosphere science, agriculture/soil science, and anthropology

  • Detection and quantification of charcoal in marine and lake sediments led to the first use of pyrogenic organic matter (pyOM) as a proxy for past fire-frequency and climate in the 1970’s (Smith et al, 1973; Herring, 1976; Swain, 1978), though there was some debate at this time as to its pyrogenic origin (Schopf, 1975)

  • A call to compare methods used to quantify pyrogenic carbon in soils and sediments, which requires the use of techniques different from those used in atmospheric sciences due to the presence of interfering matrices, came at much the same time

Read more

Summary

Introduction

The understanding that fire and pyrogenic organic matter (pyOM) have contributed to shaping Earth’s biosphere is one that has evolved within a number of disparate fields including geology, ecology, atmosphere science, agriculture/soil science, and anthropology. A call to compare methods used to quantify pyrogenic carbon (pyC) in soils and sediments, which requires the use of techniques different from those used in atmospheric sciences due to the presence of interfering matrices, came at much the same time.

Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call