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The implications of tephra burial and composition on pedogenetic processes have been studied by comparing soil profiles in two different locations influenced by the pumice fall-deposit from the Vesuvian Avellino eruption (about 3360 years BP): Mt. Somma volcano and Mt. Arciano.
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We then cross-check the correlation by comparing LR04 stack profile with NGR profile.
In this study we analyzed and compared soil hydraulic properties obtained by traditional laboratory experiments and inverse optimization tension infiltrometer data along the vertical direction within two typical Podzol profiles with sand texture in a potato field.
The effect of treatment of BP film mounted on unsterilized soil with culture filtrate of B47-9 on the transition in the diversity of fungal community was analyzed by comparing the 18S rDNA profiles of soil DNAs created with PCR-DGGE.
This is an increase of organic carbon by a factor of 3.8 and 4.7 for the upper 20 cm and upper 30 cm of the riparian profiles, respectively, when compared to the upland soil profiles.
BSC sites had thicker soil profiles compared to non-BSC sites, which could be a result of past geological processes and also partially accounted for by the establishment of BSCs that can help limit erosion and promote significant soil accumulation.
Averages of pit profile data showed the higher temperatures of 5 8 °C at 30 cm depth in the HBS soil profiles, compared to consistently freezing temperatures measured at bottom of the 30-cm deep unburned site profiles.
Although the δC values of the CO2 efflux from the dolomite soil cores were within a narrow range (A-horizon −26.2 ± 0.1 ‰; whole soil profile wet −25.8 ± 0.1 ‰; whole soil profile dry −25.5 ± 0.1 ‰) the CO2 efflux from the separated A-horizons was significantly depleted in C when compared to the whole soil profiles (p = 0.015).
Verification of the above approach for estimating actual evapotranspiration was achieved by comparing ET-values obtained by the soil moisture profile changes and the ET-values obtained by the above equation.
In a third treatment, we tested adaptation between Europe and Asia, by comparing growth of plants in 'home soil' and 'away soil' from the other region.
The airborne estimates are subject to attenuation by the soil profile.
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