Rl. Bradley et Jw. Fyles, GROWTH OF PAPER BIRCH (BETULA-PAPYRIFERA) SEEDLINGS INCREASES SOIL AVAILABLE C AND MICROBIAL ACQUISITION OF SOIL-NUTRIENTS, Soil biology & biochemistry, 27(12), 1995, pp. 1565-1571
We compared the flux of energy and nutrients in a mineral forest soil
in which paper birch (Betula papyrifera) seedlings had grown with soil
s that had been exposed to one of five other tree species over a 22 we
ek growing period. Soil basal respiration rate, metabolic quotient, so
il available C (AC), and the affinity of soil microorganisms for subst
rate-C left in the soil after harvest all increased significantly, in
soils treated with birch root systems. Concentrations of AC in birch-t
reated soils related to the energy-only limited microbial biomass (MBE
), but not the nutritionally limited microbial biomass (MEN). Amounts
of rhizosphere activity, described as root-supported MBE per unit root
and per unit fine root, were one order of magnitude higher in the bir
ch rhizosphere. Plant uptake of soil-N during the growing period was h
igh while the soil mineral-N pool was low in birch experimental units
relative to those of other species, suggesting that birch competed wel
l against soil microorganisms for available mineral-N. Anaerobic N min
eralization rates were significantly higher while the MB(N)-to-MB(E) r
atio, which describes the degree of nutritional limitation of the micr
obial biomass, was significantly lower in birch-treated soils. Signifi
cant negative correlations were found between the MB(N)-to-MB(E) ratio
and both AC and MB(E). These results suggest that high amounts of roo
t labile C compounds in conjunction with rapid mineral-N uptake by bir
ch roots can stimulate microbial communities to acquire nutrients from
the native soil.