Plant uptake of soil water and nitrogen determines plant growth, community composition and ecosystem functioning. Despite its importance, resource uptake is typically inferred from root biomass distributions rather than measured directly. Here we use a depth-controlled, dual tracer experiment in a sagebrush ecosystem, ID, USA to measure vertical patterns of water and nitrogen uptake. We compare these patterns of resource uptake to patterns of resource availability and root biomass.
Results/Conclusions
Vertical patterns of root biomass, water uptake and nitrogen uptake were strikingly different from one another. Half of root biomass (0-188 cm) occurred in the top 24 cm of the soil. Half of water uptake occurred in the top 14 cm. Half of nitrogen uptake occurred in the top 86 cm. Shallow water uptake and deep nitrogen uptake were better correlated with water and nitrogen availability than with root biomass. This suggested that root systems foraged independently for different resources. Root biomass has long been used as a proxy measure of plant access to soil resources, but our results suggest that resource availability may be a better predictor of uptake.