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  • 1
    ISSN: 1432-2285
    Keywords: Amino acids ; Arginine ; Eucalyptus ; Foliage ; Nitrogen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Rates of growth of seedlings of E. globulus, E. regnans and E. nitens were related to phosphorus supply in two soils but concentrations of total nitrogen and total phosphorus in most plant tissues did not vary significantly among soil or phosphorus treatments. Differences in concentrations of nitrogen and phosphorus and in the composition of the pool of free amino-acids among leaves at different stages of development were far greater than differences between treatments. The most significant of these differences were several-fold greater concentrations of arginine in the oldest leaves and these are most likely due to protein degradation and/or in situ synthesis since arginine is not generally phloem mobile. The concentration of reduced nitrogen in xylem sap was inversely related to growth and glutamine was by far the dominant nitrogenous solute. We suggest that specific nitrogenous solutes may be useful indices of the nitrogen status of eucalypt tissues for insect herbivores.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 142 (1992), S. 167-176 
    ISSN: 1573-5036
    Keywords: Eucalyptus regnans ; mineralization ; nitrification ; nitrogen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Laboratory and in situ rates of N mineralization in soils from Mountain Ash (Eucalyptus regnans) forests were measured fortnightly for two years in stands aged 9, 40, 80 and about 250 years (overmature), and for one year in stands aged 5 and 46 years. Rates of anaerobic mineralization (the laboratory test) showed little seasonal or annual variation. In contrast, rates of in situ mineralization varied markedly with season, being highest in spring and summer. Anaerobic mineralization was highly correlated with stand age to 80 years, but decreased between ages 80 and 250 years. In situ mineralization also decreased between these two ages, but otherwise was not related to stand age. Hence, the correlation between anaerobic and in situ mineralization along the age sequence was weak, suggesting that the anaerobic test is of maximum utility when this pool is in balance with inputs from decomposing litter (‘steady-state’ ecosystems). Nitrification was strong in stands aged 9, 46, 80 and 250 years and weak in stands aged 5 and 40 years. Within stands, the rate of nitrification during each period of in situ containment was highly dependent on the supply of NH4 ions. Between stands, annual rates of nitrification appear to be related to the balance between the N capital of the site, its rate of turnover, and the demand for N by heterotrophs and vegetation so that if NH4 supply is depleted, little is left for autotrophic nitrifiers.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 142 (1992), S. 177-185 
    ISSN: 1573-5036
    Keywords: Eucalyptus regnans ; microbial phosphorus ; organic phosphorus ; soil P tests ; P availability ; phosphatase activity
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Concentrations of labile inorganic P (Pi, dilute double acid-extractable), labile organic P (Po, bicarbonate-extractable), microbial P, and phosphatase activities were measured in Mountain Ash (Eucalyptus regnans) stands aged 0, 5, 9, 16, 40, 46, 80 and 250 years. Labile Pi, initially 34 μg g-1 at age 0 years, decreased to 2.3 μg g-1 at age 16 years, and was constant thereafter. All other indices of available P increased with stand age. Microbial P varied the most along the age sequence, from 1.8 μg g-1 at 0 years to 99 μg g-1 at age 80 years. Oxidation of organic P during the regeneration burn creates a large and readily available source of Pi for the young, developing stand. After canopy closure, the stand becomes increasingly dependent on P released by mineralization. Phosphatase activities were as high as have been recorded, and the organic pools are therefore significant stores of potentially available P. At age 80 years (for example) the amount of labile Po and microbial P in the surface 5 cm of soil was 26 kg ha-1. However, the adsorption maxima for Pi fixation were also as high as has been recorded, and so it is apparent that roots must possess specialized mechanisms of uptake to compete for mineralized P.
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