Quantifying signal dispersion in a hybrid ice core melting system.
We describe a microcontroller-based ice core melting and data logging system allowing simultaneous depth coregistration of a continuous flow analysis (CFA) system (for microparticle and conductivity measurement) and a discrete sample analysis system (for geochemistry and microparticles), both supplied from the same melted ice core section. This hybrid melting system employs an ice parcel tracking algorithm which calculates real-time sample transport through all portions of the meltwater handling system, enabling accurate (1 mm) depth coregistration of all measurements. Signal dispersion is analyzed using residence time theory, experimental results of tracer injection tests and antiparallel melting of replicate cores to rigorously quantify the signal dispersion in our system. Our dispersion-limited resolution is 1.0 cm in ice and ~2 cm in firn. We experimentally observe the peak lead phenomenon, where signal dispersion causes the measured CFA peak associated with a given event to be depth assigned ~1 cm shallower than the true event depth. Dispersion effects on resolution and signal depth assignment are discussed in detail. Our results have implications for comparisons of chemistry and physical properties data recorded using multiple instruments and for deconvolution methods of enhancing CFA depth resolution.
Department of Physics and Astronomy, Bennett Hall, University of Maine, Orono, Maine 04469, USA. daniel.j.breton@dartmouth.edu
Daniel J
DJ
Breton
Bess G
BG
Koffman
Andrei V
AV
Kurbatov
Karl J
KJ
Kreutz
Gordon S
GS
Hamilton
D000465:Algorithms; D004784:Environmental Monitoring / Q000295:instrumentation* / Q000379:methods; D005615:Freezing; D007053:Ice; D008962:Models, Theoretical
D007053:Ice