TABLE 3.
Regressions between T-RFLP principal-component ordination and soil chemistry/N-processing ratesa
Parameter | PC1
|
PC2
|
||
---|---|---|---|---|
r2 | P | r2 | P | |
Initial NO3 pool (μg/g) | 0.749 | 0.000 | 0.353 | 0.006 |
Nitrification (μg/g/day) | 0.419 | 0.013 | 0.208 | 0.044 |
DNRA (μg/g/day) | 0.363 | 0.025 | 0.191 | 0.053 |
15N2 flux | 0.228 | 0.049 | 0.026 | 0.493 |
Total N gas flux (denitrification) | 0.225 | 0.050 | 0.025 | 0.508 |
15N2O flux | 0.185 | 0.085 | 0.033 | 0.440 |
Initial NH4 pool (μg/g) | 0.142 | 0.124 | 0.013 | 0.631 |
Microbial biomass N | 0.073 | 0.310 | 0.025 | 0.504 |
15N microbial biomass uptake | 0.032 | 0.444 | 0.001 | 0.970 |
Mineralization (μg/g/day) | 0.029 | 0.417 | 0.104 | 0.166 |
NH4 consumption (μg/g/day) | 0.001 | 0.605 | 0.371 | 0.004 |
PC2 | 0.000 | 0.830 | NAb | NA |
Data are from soil samples collected in the Luquillo Experimental Forest and incubated under four redox regimens. Significant correlations (P < 0.05) are indicated in boldface; those with r2 values of >0.2 are underlined. Separate multiple regression was performed for each principal component. All rates were measured over 0 to 24 h following 15N labeling.