Plant production and community structure in a mesic semi-natural grassland: Moderate soil textural variation has a much stronger influence than experimentally increased atmospheric nitrogen deposition

Abstract

Aims

Atmospheric nitrogen (N) deposition derived from agricultural intensification and fossil fuel burning can significantly impact plant growth, species diversity, and nutrient cycling. Semi-natural grasslands are of particular concern because their generally low intensity agricultural management suggests they may be very sensitive to enhanced atmospheric N deposition inputs, although previous experimental research indicates highly variable, site-specific responses. Mediating factors such as soil texture that influence actual availability of soil water and nutrients to plants have generally not been investigated.

Methods

We report the impacts of 16 years of experimental N addition (simulating 2050 atmospheric N input rates) and a separate, single growing season, high-level N and phosphorus (P) factorial experiment to a hayfield of varying loam soil texture (clay-loam – sandy-loam) on plant community structure and above-and belowground biomass.

Results

The chronic low-level N addition treatment had no significant effects on either species or community aboveground growth, species richness, or diversity. These properties were best explained by variation in soil water-filled pore space, and were substantially larger on plots with relatively clay-rich soils.

Conclusions

The general lack of responses to the low-level N additions and the lack of a growth response to the short factorial high-level N and P addition experiment, indicate that future atmospheric N deposition increases are unlikely to have major impacts on hay production or species composition in mesic semi-natural grasslands. By contrast, the strong interconnected influences of soil clay content and plant water availability in our results suggest that textural variation – even within loamy soils—will be a primary determinant of the impacts of anticipated future summer warming and reduced rainfall on hayfield vegetation.