Extractable iron (Fe) at various drained thaw lake basins near Barrow, Alaska, 2009-2011

Soils from various drained thaw lake basins near Barrow, Alaska (AK) were extracted with various solvents reflecting different iron (Fe) pools. Values are presented in micromoles per gram (g) and micromoles per cubic centimeter (cm^3) (the latter being more appropriate for comparing light organic an...

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Bibliographic Details
Main Author: 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
EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > SPECTROMETERS/RADIOMETERS > SPECTROMETERS > SPECTROMETERS
FIELD SURVEY
environment
Barrow
Alaska
Online Access:https://doi.org/10.18739/A2FX73Z99
Description
Summary:Soils from various drained thaw lake basins near Barrow, Alaska (AK) were extracted with various solvents reflecting different iron (Fe) pools. Values are presented in micromoles per gram (g) and micromoles per cubic centimeter (cm^3) (the latter being more appropriate for comparing light organic and dense mineral layers). See Lipson et al. (2013) Global Biogeochemical Cycles 27:1-11, doi:10.1002/gbc.20038, and Lipson et al. (2010) J Geophys Res-Biogeosci (G) 115, G00I06, doi:10.1029/2009JG001147. The mineral types generally associated with each solvent are indicated.

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