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To calculate mass loss, mean dry density from gravimetric density assessment was used if available.
To calculate decomposition constants (k) based on mass loss, mean dry density from gravimetric density assessment was used if available.
Otherwise we used mean dry density based on drill resistance.
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"I mean, dried plums".
These may periodically offset or amplify the mean drying trend.
(Confusingly, sec, which means dry in French, and extra-dry are fairly sweet).
The variability of dry density, mean particle size (D50) and coefficient of uniformity (Cu) is quantified at different size scales.
Table 1 Soil parameters Parameters Value Specific gravity, G s 2.903 Coefficient of uniformity, C u 12.188 Coefficient of curvature, C c 1.154 Mean grain size, D 50 (mm) 0.143 Dry density, ρ d (kg/m3) 1,330 Void ratio, e 1.183.
From Q3 to Q2 and Q1 loess, the mean particle size and the void ratio decrease as well as dry density increases.
The mean dry mass data were collected from 50 randomly sampled individuals in the populations with sowing densities >500/m2 in four replicate plots at each sowing density.
The GU density did not correlate significantly with either the dry mass per plant or the mean dry mass of the GUs.
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