The bulk soil δ15N signature in grassland soils is fingerprinting
nitrogen inputs, and losses, both shaped by land management, climate,
and biodiversity. δ15N has been explored as an indicator of these
factors in multiple studies with mixed results regarding its primary
drivers. This study quantified changes in soil δ15N natural abundance
for 72 German grassland sites after 12 years (2011 vs. 2023) and linked
these changes to detailed records of land-use intensity, biodiversity,
and climate. Land-use intensity was calculated from management
activities including mowing, grazing and fertilisation. In the top 10 cm
of the soil, δ15N changes between 2011 and 2023 ranged from -0.86 to
+2.49‰ (equating to an average increase of +0.35‰ per decade). Over
two-thirds of our study sites showed a long-term increase in δ15N. These
sites with rising δ15N were associated with high land-use intensity,
particularly high rates of fertilisation and grazing. Our findings
indicate that management with organic fertiliser application and grazing
are the dominant drivers of increases in δ15N. A biodiversity-induced
decrease in δ15N due to a tightening of the N cycle and reduction of N
losses was not observed. The slow decadal-scale shifts show that single
sampling of soil δ15N without known starting values is only informative
for long-term processes spanning > 50 years, and does not allow for
insights regarding the impacts of more recent management practices.
Thus, our findings emphasize the long-term character of bulk soil δ15N
as an indicator of management in temperate grasslands, particularly when
repeated sampling is not possible.