Biogas
slurry (BS) is now increasingly used for organic rice production
in China. However, the isotopic response and fractionation of different
BS application rates to characterize organic rice cultivation have
not yet been investigated. In this study, different fertilizer treatments
were applied to rice paddy soil including urea, BS with five different
application rates and a control with no fertilizer added. Multiproxy
analyses (% C, % N, δ13C, δ15N,
δ2H, and δ18O) of rice, rice straw,
and soil were undertaken using elemental analyzer–isotope ratio
mass spectrometry. Rice, straw, and soil showed only minor isotopic
and elemental variations across all fertilizer treatments except for
δ15N. δ15N values of rice and straw
became more positive (+6.1 to +11.2‰ and +6.1 to +12.2‰,
respectively) with increasing BS application rates and became more
negative with urea fertilization (+2.8 and +3.0‰, respectively).
The soil had more positive δ15N values after BS application
but showed no significant change with different application rates.
No obvious δ15N isotopic differences were found between
the control soil and soils fertilized with urea. 15N fractionation
was observed between rice, straw, and soil (Δrice‑soil −2.0 to +4.3‰, Δstraw‑soil −1.9 to +5.3‰) and their isotopic values were strongly
correlated to each other (r > 0.94, p < 0.01). Results showed that % C, % N, δ13C,
δ2H, and δ18O in rice displayed
only minor variations for different fertilizers. However, δ15N values increased in response to BS application, confirming
that BS leaves an enriched 15N isotopic marker in soil,
straw, and rice, indicating its organically cultivated status. Results
from this study will enhance the stable isotope δ15N databank for assessing organic practices using different fertilizer
sources.