Unusually high SOC levels have been reported for sandy cropland soils in North-Western Europe. A potential link with their general heathland land-use history was investigated by comparing two soil pairs of relict heathland and cultivated former heathland in the Belgian sandy region. A sequential chemical fractionation yielded similar sizes in corresponding SOM fractions between the heathland and cropland soils (i.e. NaOCl resistant: 12.3-15.0 g C kg(-1) and NaOCl + HF resistant: 2.6-5.3 g C kg(-1)). Higher amounts of clay sized N in the cropland plots can be attributed to N additions from mineral fertilizers and animal manure. Temperature resolved Pyrolysis Field Ionization Mass Spectroscopy analysis showed that the composition of both reli...
The ubiquitous abundance of pyrolysed, highly aromatic organic matter, called “Black Carbon” (BC), i...
Soil characteristics in palaeosols are an important source of information on past climate and vegeta...
Molecular assessment of the origin and transformation processes of soil organic matter (SOM) was car...
Unusually high SOC levels have been reported for sandy cropland soils in North-Western Europe. A pot...
Unusually high SOC levels have been reported for sandy cropland soils in North-Western Europe. A pot...
Land-use history is often overlooked when assessing soil fertility of intensive cropland production ...
A renewed interest in chemical fractionation of soil organic matter (SOM) originates from the premis...
Sandy cropland soils in NW Europe were found to contain unusually high organic-carbon (OC) levels, a...
Land-use history is oft en overlooked when assessing soil fertility of intensive cropland production...
Sandy cropland soils in NW Europe were found to contain unusually high organic-carbon (OC) levels, a...
In archaeology and nature conservation studies, knowledge about (pre)historical land-use is importan...
A renewed interest in chemical fractionation of soil organic matter (SOM) originates from the premis...
Preservation of soil organic matter (SOM) is strongly affected by occlusion within aggregates and by...
Soil organic matter (SOM) stabilisation on tropical sloping land can be influenced by slash burning ...
Soil Organic Matter (SOM) is essential for soil stability, fertility and crop productivity. Recent f...
The ubiquitous abundance of pyrolysed, highly aromatic organic matter, called “Black Carbon” (BC), i...
Soil characteristics in palaeosols are an important source of information on past climate and vegeta...
Molecular assessment of the origin and transformation processes of soil organic matter (SOM) was car...
Unusually high SOC levels have been reported for sandy cropland soils in North-Western Europe. A pot...
Unusually high SOC levels have been reported for sandy cropland soils in North-Western Europe. A pot...
Land-use history is often overlooked when assessing soil fertility of intensive cropland production ...
A renewed interest in chemical fractionation of soil organic matter (SOM) originates from the premis...
Sandy cropland soils in NW Europe were found to contain unusually high organic-carbon (OC) levels, a...
Land-use history is oft en overlooked when assessing soil fertility of intensive cropland production...
Sandy cropland soils in NW Europe were found to contain unusually high organic-carbon (OC) levels, a...
In archaeology and nature conservation studies, knowledge about (pre)historical land-use is importan...
A renewed interest in chemical fractionation of soil organic matter (SOM) originates from the premis...
Preservation of soil organic matter (SOM) is strongly affected by occlusion within aggregates and by...
Soil organic matter (SOM) stabilisation on tropical sloping land can be influenced by slash burning ...
Soil Organic Matter (SOM) is essential for soil stability, fertility and crop productivity. Recent f...
The ubiquitous abundance of pyrolysed, highly aromatic organic matter, called “Black Carbon” (BC), i...
Soil characteristics in palaeosols are an important source of information on past climate and vegeta...
Molecular assessment of the origin and transformation processes of soil organic matter (SOM) was car...