Marco Schmidt
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Papers by Marco Schmidt
visible due to a lack of appropriate data archives. With the West African Data and Metadata Repository, we present a secure long-term archive for a data-poor region allowing detailed documentation by metadata following the EML standard and giving data holders the opportunity to define levels of data access and conditions of use. This article gives an overview of structure, functions and content. The repository is online at the URL http://westafricandata.senckenberg.de.
of West Africa, we compared the magnitude of soil organic C and N differences in bulk soil and aggregate
fractions between contrasting types of land cover (degraded land and native land cover) and soil (Luvisols and
Cambisols). We analyzed the following soil key indicators: CEC, soil respiration, C and N contents, and δ13C and
δ15N signatures of soil organic C.
The average CO2 respired from native land cover was at least 82% higher than its value from degraded land cover
andwas significantly higher in Luvisols than in Cambisols. Likewise, the soil organic C and N contents in bulk soil
were significantly affected by land cover and soil contrasts. The average C loss in bulk soil from degraded land
cover was equivalent to 49% in Cambisols and 54% in Luvisols. In both soil types, all aggregate fractions were sensitive
to land degradation processes and the C loss decreased from macroaggregates to the clay + silt fraction.
Compared to the native land cover, organic C loss from the macroaggregates in degraded land cover was 92%
and 84%, respectively, in Cambisols and Luvisols. The soil type affected significantly the C content only in the
clay + silt fraction. The C/N ratio of finer fractions (microaggregates and clay + silt) was significantly higher
in degraded land cover than in native land cover, indicating greater losses of N than C during land degradation
processes. The differences of δ13C signatures throughout C pools between the two types of land cover suggest a
relative dominance of C3 derived C inmacroaggregates and C4 derived C in the clay+silt fraction in the degraded
lands. The reduction of soil respiration and the rapid N loss in degraded land cover slowed downthe humification
processes of C3 plant derived materials which were effectively dominant in macroaggregates.
visible due to a lack of appropriate data archives. With the West African Data and Metadata Repository, we present a secure long-term archive for a data-poor region allowing detailed documentation by metadata following the EML standard and giving data holders the opportunity to define levels of data access and conditions of use. This article gives an overview of structure, functions and content. The repository is online at the URL http://westafricandata.senckenberg.de.
of West Africa, we compared the magnitude of soil organic C and N differences in bulk soil and aggregate
fractions between contrasting types of land cover (degraded land and native land cover) and soil (Luvisols and
Cambisols). We analyzed the following soil key indicators: CEC, soil respiration, C and N contents, and δ13C and
δ15N signatures of soil organic C.
The average CO2 respired from native land cover was at least 82% higher than its value from degraded land cover
andwas significantly higher in Luvisols than in Cambisols. Likewise, the soil organic C and N contents in bulk soil
were significantly affected by land cover and soil contrasts. The average C loss in bulk soil from degraded land
cover was equivalent to 49% in Cambisols and 54% in Luvisols. In both soil types, all aggregate fractions were sensitive
to land degradation processes and the C loss decreased from macroaggregates to the clay + silt fraction.
Compared to the native land cover, organic C loss from the macroaggregates in degraded land cover was 92%
and 84%, respectively, in Cambisols and Luvisols. The soil type affected significantly the C content only in the
clay + silt fraction. The C/N ratio of finer fractions (microaggregates and clay + silt) was significantly higher
in degraded land cover than in native land cover, indicating greater losses of N than C during land degradation
processes. The differences of δ13C signatures throughout C pools between the two types of land cover suggest a
relative dominance of C3 derived C inmacroaggregates and C4 derived C in the clay+silt fraction in the degraded
lands. The reduction of soil respiration and the rapid N loss in degraded land cover slowed downthe humification
processes of C3 plant derived materials which were effectively dominant in macroaggregates.