Dissolved Fe, 2012

In 2012, iron (Fe) dissolved in soil pore water was measured at various locations within the drained thaw lake basin previously used for the Biocomplexity Experiment (BE), near Barrow, AK. Collars were arranged in three clusters within the central region of the BE, referred to as A, B and C. Soil wa...

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Bibliographic Details
Main Authors: K. Miller, E. Friedman, L. Angenent, D. A. Lipson
Format: Dataset
Language:unknown
Published: Arctic Data Center 2013
Subjects:
EARTH SCIENCE > BIOSPHERE > AQUATIC ECOSYSTEMS > WETLANDS > PEATLANDS
IN SITU/LABORATORY INSTRUMENTS > SPECTROMETERS/RADIOMETERS > COLORIMETERS
FIELD SURVEY
environment
Barrow
Alaska
Online Access:https://doi.org/10.18739/A2P34X
Description
Summary:In 2012, iron (Fe) dissolved in soil pore water was measured at various locations within the drained thaw lake basin previously used for the Biocomplexity Experiment (BE), near Barrow, AK. Collars were arranged in three clusters within the central region of the BE, referred to as A, B and C. Soil water was sampled with Rhizon water samplers, preserved with hydrochloric acid (HCl) and analyzed colorimetrically with 1,10-phenanthroline.

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