(1) Ion-exchange and 'reversed phase' Liquid Chromatography (Dionex)
(2) Spectralphotometry - UV/Vis Spectrometer Lambda 2 (Perkin Elmer)
(3) Flow-Injection-Analysis, FIAS 200 (Perkin Elmer)
(4) Elektrothermische AAS, Zeeman ET-AAS 4100 ZL (Perkin Elmer)
(5) ICP-OES, iCAP 6000 series Spectrometer (Thermo Electron Cooperation)
(6) Quadrupol ICP-MS, Mass Spectrometer ELAN DRC-e (Perkin Elmer)
(7) IR-Spectrometry, TOC-5000A (Shimadzu)
(8) Coulometry, Coulomat 702 (Ströhlein)(currently out of operation)
(1) Gamma Spectrometry
(2) Alpha Spectrometry
(3) Liquid-Scintillation Spectrometry
Portable instrument for lab and field measurements with lead-shielding of the measuring chamber and α—liquid scintillation counting on the basis of α/β decay discrimination using the different extinguish time of induced photo-peaks.
Procedures, devices and applications
What is tephra?
Tephra, the Greek word for ash, is used to describe any material that is ejected by a volcano into the atmosphere (pyroclasts). Tephra includes dense blocks and bombs (>64mm), and lighter materials such as scoria, pumice and ash (<2mm). As one moves away from a volcano, the tephra deposits become finer grained (smaller particles) and thinner. This is because small airborne particles hover longer and stay within the atmosphere for a greater distance from the volcano. These particles of ash can be carried in the atmosphere for thousands of kilometers. The smallest particles are so-called crypto-tephra and are invisible to the naked eye.
In the laboratory for tephra analytics, samples taken from lake sediment cores are prepared for the identification and geochemical analysis of individual cryptotephras (glass shards). Identified cryptotephras are a prerequisite for the creation of a tephrochronology that allows the independent dating of our palaeoclimate and environmental archives.
Procedures, devices and applications: