Water accessibility to plant roots in different soil structures occurring in the same soil type

The capacity of a soil to supply roots with water and nutrients for crop growth is important when defining sustainable land management which implies maintenance of production and reduction of production risks. Not only the amount of available water is important but also its accessibility, which differs among different soil structures. Different structures within one soil series were associated with three types of management: (i) conventional, temporary grassland (Conv), (ii) biodynamic, temporary grassland (Bio) and (iii) conventional permanent grassland (Perm). Transpiration of barley plants, under identical circumstances, and the associated rooting patterns, were measured in five large undisturbed cores from each of the three soil structures. Management had significantly changed bulk density, organic matter content and porosity. Measured transpiration showed significant differences with highest amounts for Perm followed by Conv and lowest amounts for Bio. Rooting pattern characteristics, defined as the relation between a series of hypothetical extraction zones around each root and the volumes of excluded soil were determined for the three structures. These rooting pattern characteristics were most favourable for Perm, followed by Bio and Conv, respectively. The water supply characteristics, defined as the number of days the soil can satisfy a transpiration demand of 5 mm d^-1 as a function of a hypothetical extraction zone, reflects the capacity of the soil to supply roots with water. These water supply characteristics combined with the rooting pattern characteristics were used to quantify the accessibility of soil water. Accessibility was highest for Perm and Conv with 95% and 94% respectively, followed by Bio with 68%. When used in a simulation model and compared with simulations implicitly assuming total accessibility, measured transpirations were better simulated by introducing the expression for water accessibility.