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Adding zeolite to the soil caused an increase in the bulk density at the beginning of the experiment.
While most of the soil characteristics between the field sites were similar, bulk density at the forest site (0.7 g cm− 3) was significantly lower than bulk density at the other field sites (1.0 g cm− 3).
Here, we use mean wet bulk density at the sampling site for calculation because granitic saprolite contains water, in contrast to fresh rock.
Three variables were recorded for this: the mean bulk density at the end of the filling phase, the discharge rate and the flow pattern.
We show that spectroscopic and gamma attenuation sensors can produce accurate measures of soil organic C and bulk density at the sampling locations, in this case every 5 cm to a depth of 1 m.
Table 5 Bulk density at the beginning and at the end of the experimental period A0 A5 A10 Bulk5 B10 Bulk density (g · cm3) Beginning 1.88a* 1.94a 1.91a 1.50a 1.60a 1.64a Ending 1.68b 1.55b 1.65b 1.25b 1.20b 1.10b *Values in any column followed by the same letter do not differ at the 0.05 significance level.
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Separate soil core were also collected with corer (15 cm height) for the measurement of bulk density at these sites.
Table 5 shows the comparison between the bulk densities at the beginning and end of the experimental period.
The spatial distributions of the first PCs resembled bulk density at short scale and the paleo-channels and texture at long scale.
Conventional till site showed the lowest microporosity values and the highest macroporosity, followed by lower soil bulk density at 0 10 cm layer.
50 vol.% of this interslab space was filled with organic compounds and the other 50 vol.% with water, both at densities in accordance to their respective bulk densities at standard conditions.
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