Les Maths Effrayantes (Multiplication & Division à Un, Deux ou Trois Chiffres) (A)

Furthermore, for simulating GPR reflection data acquired above a transition from unsaturated to saturated soil, geophysicists often approximate the soil water retention curve by

Title Page Abstract Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc. Printer-friendly Version Interactive Discussion on the FB and in the

data from the good weather period were used, and the model results were compared with both in-situ (UV absorption) and remote sensing measurements (LP-DOAS)..

Figure 3 illustrates calculated and measured monthly averaged daily maximum ozone for (a) all 54 sites, (b) the northern European sites (Norway, Sweden and Fin- land), (c) the

The Polysaccharide Utilization Loci (PUL) database was launched in 2015 to present PUL predictions in ∼70 Bacteroidetes species isolated from the hu- man gastrointestinal tract, as

side pockets.[11] Semagina and co-workers furthermore evidenced that despite of loss of crystallinity microporosity increases, due to selective removal of Al form

different treatments (T, UVT, and UV) had no significant effects on the community dark respiration rates even if a slight increase was observed at the beginning of the experiment

During the late summer season, rates of primary production showed an homogeneous profile, with surface values close to winter carbon uptake rates (0.77 ± 0.2 mmoles L
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