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Whether the observed increase in mi- crobial biomass and soil respiration in the FACE rings is driven by altered or increased litter input is not com- pletely clear as other

Much of the differences in soil compression data are not in good agreement with earlier ®ndings, dis- cussed by Canarache (1980) and in part brie¯y presented here, which had shown

Water stress signi®cantly reduced growth rate (Table 1) while causing greater range of diurnal expansion and contraction of fruit diameter (Fig.. A peculiar `growth jump' was

the Neoproterozoic sedimentary rocks seem to contain rare zircons of pre-Mesoproterozoic age relative to zircons of Grenvillian and Early Cado- mian age (Table 1, Fig. This may

(1998) reported that high genetic merit factors can result in errors in ration formulation and cows were still in negative energy balance at 20 the prediction of animal

With a high degree of profile stability (soil types numbers 1, 2 and 4), the water table depth is linked to drain depth, and the unstable layer occurs below 0.60 m.. At the

Distribution of (a) NaHCO3-Pi and (b) NaOH-Pi with depth in Le Bras silt loam soil amended with liquid pig manure over 14 years. 2) were significantly (p < 0.01) affected by the

Measured and estimated soil hydraulic properties: water retention curve and drainage volume±water table relationship.. Observed (H3) and estimated water retention curves (H1 and H2)