The genesis and transformation of organo-mineral colloids in a drained peatland area (original) (raw)
Physics and Chemistry of the Earth, 1998
Abstract
The spatial evolution of colloids from a drained peat bog to a river was studied in a karstic watershed (Jura Mountains, Switzerland) by bulk chemistry and electron microscopy. Raw waters (peat bog pore water, water from artificial drains and river water) were analyzed using ICP (Fe, Ca), Colorimetry (Fe2+), TOC and UV (organic matter) and analytical electron microscopies (TEM-EDS, STEM-EDS,
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