When comparing simultaneously across all BNEA land-use types and
BNEN ecosystem types, it was found that BNE from riparian, vegetable
and intentional fallow areas were significantly higher than from boreal forests
(P< 0.05). As mentioned above, riparian areas can receive abundant N
input from surrounding crop fields and sustain anaerobic conditions, vegetable
fields can have a history of previous N fertilizer additions, and intentional
fallow fields register net N mineralization from soil organic matter in absence
of N and water uptakes by crop plants, while boreal forests typically exhibit N
limited status and they are also subjected to relatively cold temperatures.Other than boreal forests, riparian, vegetable, and
intentional fallow sites, none of the other land-use or ecosystem types assessed
in our meta-analysis showed significant effects on BNE. Likewise, when
comparing overall BNEA vs. overall BNEN, no significant
difference was found. This can suggest that although BNEN values tended
lower than BNEA on median basis, we cannot generalize at this stage that BNE is
different between agricultural and natural lands. Many factors can contribute
to mask and confound these tendencies including interactions between land-use
or ecosystem type with soil properties and climatic factors as well as previous
land management history. For instance, natural lands typically exhibit higher
soil organic C and N contents than agricultural lands (soil organic C medians =
45.7 vs. 23.7 g kg-1, respectively). However, soil C:N ratios are
slightly wider for natural than for agricultural lands (medians = 12.2 vs.11.2,
respectively), and also natural lands exhibited much lower pH than agricultural
lands (medians = 4.5 vs. 6.4, respectively). These observed variations in soil
properties between natural and agricultural lands are not clearly explained.
They might be caused by a differential influence of land-use or ecosystem types
on these soil properties and/or conversely the result of a human-driven
selection of the more fertile available lands (i.e., soils with high organic
matter and neutral pH) for agricultural use.
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