Extractable Fe

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

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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/A22D0X
Description
Summary:Soils from various drained thaw lake basins near Barrow, AK were extracted with various solvents reflecting different Fe (iron) pools. Values are presented in micromoles per g and micromoles per 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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