Keyphrases
Organo-mineral Associations
100%
Clay Fraction
100%
Glacier Retreat
100%
Soil Chronosequence
100%
Organic Matter
85%
Mineral Surface
57%
Specific Surface Area
42%
Hydrogen Peroxide
42%
Carbohydrates
42%
Cation Exchange Capacity
42%
Alkyl
28%
Aging
28%
Aromatics
28%
Clay
28%
Carboxyl
28%
Acid Soil
28%
Organic Carbon
28%
Mineral Phase
28%
Organic Carbon Content
28%
Solid-state 13C NMR Spectroscopy
28%
Organic Carbon Loading
28%
X Ray Diffraction
14%
Switzerland
14%
Amino Acids
14%
Glacier
14%
Sorption
14%
Chemical Composition
14%
Residence Time
14%
Strong Correlation
14%
Ferrihydrite
14%
Organic Compounds
14%
Organic Components
14%
Oxalate
14%
Acid Hydrolysis
14%
Increasing Age
14%
Structural Organization
14%
Neutral Sugars
14%
N2 Adsorption
14%
Surface Exchange
14%
Fe Oxides
14%
Relative Proportion
14%
Structural Mechanism
14%
Compound Surface
14%
CN Ratio
14%
Soil Formation
14%
Organo-mineral Interactions
14%
Mineral Constituents
14%
Initial Soil Formation
14%
Foreland
14%
Soluble Fe
14%
Mineral Weathering
14%
Clay-sized Particles
14%
Soil Aging
14%
Poorly Crystalline Fe
14%
Proglacial Area
14%
Mineral Surface Area
14%
Organic Carbon Accumulation
14%
Preferential Association
14%
Old Soils
14%
Expandable Clays
14%
Oxalate Extraction
14%
Loading Point
14%
Treated Clay
14%
Glacial Till
14%
Chronosequence Approach
14%
Earth and Planetary Sciences
Glacier Retreat
100%
Organic Carbon
100%
Chronosequence
100%
Organic Matter
85%
Mineral Surface
71%
Surface Area
57%
Ion Exchange
42%
Acid Soil
28%
Oxalic Acid
28%
Pedogenesis
28%
Switzerland
14%
X Ray Diffraction
14%
Ferrihydrite
14%
Monomer
14%
Amino Acid
14%
Agricultural and Biological Sciences
Chronosequence
100%
Clay Fraction
100%
Surface Area
57%
Cation Exchange Capacity
42%
Acid Soil
28%
Soil Formation
28%
NMR Spectroscopy
28%
X-Ray Diffraction
14%
Glacial Till
14%
Ferrihydrite
14%
Enzymatic Hydrolysis
14%