Application of structural equation modeling for assessing relationships between organic carbon and soil properties in semiarid Mediterranean region
Restoration of atmospheric carbon in soils has principal many good effects. Arid lands cover more than 40 % of the global earth area, but only stock 16 % from the global carbon stock. It seems to be a suitable solution for this environmental issue, but still all variables controlling organic carbon...
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Veröffentlicht in: | International journal of environmental science and technology (Tehran) 2011-03, Vol.8 (2), p.305-320 |
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Sprache: | eng |
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Zusammenfassung: | Restoration of atmospheric carbon in soils has principal many good
effects. Arid lands cover more than 40 % of the global earth area, but
only stock 16 % from the global carbon stock. It seems to be a suitable
solution for this environmental issue, but still all variables
controlling organic carbon in such kinds of soil, was ignored. This
study aims to develop two models of organic carbon under clayey and
sandy soils in semi-arid Mediterranean zones basing on physical and
chemical soil properties. For establishing both models, structural
equation modeling was used. For modeling organic carbon, two Tunisian
soil databases composed from clayey and sandy soils made respectively,
of 450 and 602 soil horizons were used. Using the two databases for all
properties, the principal component analysis shows two components for
clayey soil; (i) chemical properties and bulk density and (ii) physical
properties. For the sandy soil it reveals two components; (i) chemical
properties and (ii) physical properties. According to the derived
components for each soil category, two models have been built.
Structural equation modeling results show that clayey model has proved
that organic carbon was controlled by chemical properties and bulk
density more than physical properties and sandy model has proved that
organic carbon was controlled by chemical properties more than physical
properties. The root mean square errors of approximation were 0.079 and
0.050 for the clayey and sandy models, respectively. Then these two
models were validated with two other databases from Tunisian dry land
soils. |
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ISSN: | 1735-1472 1735-2630 |
DOI: | 10.1007/bf03326218 |