Table 4 Three techniques used to estimate the annual denitrification rate from the study site.

From: Biotic and abiotic controls on co-occurring nitrogen cycling processes in shallow Arctic shelf sediments

Technique

Correlation variable with D14

Spatial analysis

Modelling approach

Mean annual D14 rate (Gmol N yr−1 study site area−1)

1

None; used mean D14 for all stations

None; used study area as a whole

Propagated error

5.30±3.60

2

BPc for 51 stations

Empirical Bayesian kriging; 7 bins

Propagated error

4.65±0.16

3

BPc for 51 stations

Empirical Bayesian kriging; 7 bins

Randomly generated rates in each bin for 100,000 iterations

4.04±0.001