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Altogether, VNIRS can be considered a useful method for monitoring grasslands soil properties for management purposes.
Plots with heathland soil were covered with heather and gorse, whereas plots with grasslands soil were overflowing with a variety of grasses.
At precipitation levels typical of grasslands, soil water will be lower on coarse-textured than fine-textured soils, increasing water limitation of community productivity, and thus the importance of soil water increases in regulating productivity.
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Most abundant in the grasslands soils were subgroups 16, 6, 4, 3, and 7, which represented 6.8, 4.4, 2.8, 1.8, and 1.4%, respectively, of all sequences that were classified in grassland.
The soils under trees, for instance, are much more acidic and contain much less humus than those under grass, and nitrogen content is considerably greater in the grassland soil.
The SOC content was higher in forest than grassland soil in the particle-size fraction samples.
A grassland soil (Haplic Cambisol) was chosen since its aggregates were not disturbed by tillage.
Fire-affected grassland soil appeared to have lower TOC than forest soils in all soil particle-size fractions in our study.
The second greatest C functional group in the soil was alkyl-C, with higher content in forest than grassland soil (P = 0.002).
Even so, the majority of P in typical grassland soil is present as organic P which represents a large pool of potentially available nutrient (Bourke et al. 2008).
The potential increase in aromatic-C content via combustion in the studied grassland soil might offset the high aromatic-C content originally in the forest soils and litters, since little difference in aromaticity was observed between the forest and grassland soils.
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