Determination of Soil Respiration rates and d13C in situ using a spectroscopic Picarro G1101-i instrument

Variation in the d13C-signature of soil respiration can be used as a tracer in ecological research. Up until now, isotopic determinations have mainly been performed by gas sampling and expensive and complex laboratory IRMS analyses. Recently, user friendly, portable and less expensive spectroscopic instruments have become available on the market. However, if these instruments give reliable data in dynamic systems under highly variable temperatures and air humidity conditions is unknown. In this talk we will present results from the first summer of tests of the use of a Picarro G1101-i cavity ringdown spectroscopy instrument (size 43 x 25 x 59 cm; 26.3 kg) to determine the d13C of soil respiration in various systems.

Björk, Robert G.,1974Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences(Swepub:gu)xbjoro (author)
Hagedorn, Frank (author)
Kätterer, Tomas (author)
Menichetti, Lorenzo (author)
Wipf, Sonja (author)
Göteborgs universitetInstitutionen för växt- och miljövetenskaper (creator_code:org_t)

By the author/editor: Ekblad, Alf; Björk, Robert G. ...; Hagedorn, Frank; Kätterer, Tomas; Menichetti, Lore ...; Wipf, Sonja

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