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assessment of changes in the phosphorus status of forest ...

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example <strong>the</strong> compiled data from BZE-I sites for spruce showed that 3-year old spruce<br />

needles had 30 to 40 % lower values <strong>of</strong> P than <strong>the</strong> fully developed needles from <strong>the</strong><br />

current year (Fig 1). The difference between 1 st - and 3 rd year needles were<br />

surpris<strong>in</strong>gly constant across <strong>the</strong> whole range <strong>of</strong> needle P concentrations <strong>in</strong> spruce<br />

(BMLEF 1997). In ano<strong>the</strong>r data set shown <strong>in</strong> Table 5, foliar P levels <strong>in</strong> ten spruce<br />

stands were measured cont<strong>in</strong>uously for 10 years. Three years old needles had 66 to 82<br />

% <strong>of</strong> P present <strong>in</strong> <strong>the</strong> one year old needles. Five year old needles had fur<strong>the</strong>r reduced<br />

P levels (range 47% to 70%). The amount <strong>of</strong> P re-allocated from 5 year old needles to<br />

<strong>the</strong> youngest cohort <strong>of</strong> needles equated to 30 to 50 % <strong>of</strong> <strong>the</strong> content <strong>in</strong> <strong>the</strong> current year<br />

needles. The withdrawal was not related to any measured site property. Similar results<br />

were also obta<strong>in</strong>ed for one and two years old needles <strong>of</strong> Scots p<strong>in</strong>e.<br />

Soil characteristics<br />

In a study <strong>of</strong> 49 stands <strong>of</strong> European beech (60-or more years-old) <strong>in</strong> <strong>the</strong> Werdenfelser<br />

Land region where <strong>the</strong> canopy conditions were monitored, Ewald (2000) analysed<br />

foliage and soil samples from 8 sites for nutrient composition. Sites could be divided<br />

<strong>in</strong>to 2 groups. Moderate P levels were found <strong>in</strong> trees from well-developed m<strong>in</strong>eral<br />

soils, and extremely low P levels (0.6-1.0 mg/g) <strong>in</strong> immature carbonate soils where<br />

total P levels <strong>in</strong> soils were low and Ca saturation very high. Very high N/P ratios <strong>of</strong><br />

30 or more were associated with low P levels. Phosphorus was a critical element <strong>in</strong><br />

<strong>the</strong> nutrition <strong>of</strong> beech <strong>in</strong> <strong>the</strong> calcareous Alps, which may be partly responsible for<br />

poor vitality <strong>of</strong> this species <strong>in</strong> mixed mounta<strong>in</strong> <strong>forest</strong>s. Foliar P values <strong>in</strong> beech <strong>forest</strong>s<br />

on calcareous bedrocks are commonly low when compared to acid soils. As <strong>the</strong><br />

availability <strong>of</strong> protons is required to release P from rock m<strong>in</strong>erals it is possible that<br />

low foliar P values on calcareous bedrock may result from <strong>the</strong> high buffer<strong>in</strong>g <strong>of</strong> most<br />

<strong>of</strong> <strong>the</strong> protons by carbonates which renders less protons available for silicate<br />

wea<strong>the</strong>r<strong>in</strong>g.<br />

Highest values <strong>of</strong> foliar P are found <strong>in</strong> spruce and p<strong>in</strong>e stands on bedrocks <strong>of</strong> basalt<br />

type (bedrock type 8 – median value <strong>of</strong> P <strong>in</strong> <strong>the</strong> current needles <strong>of</strong> 1.5 mg P/g) and <strong>the</strong><br />

lowest on <strong>the</strong> calcareous type (bedrock type 1 – median values were 1.2 mg/g for<br />

spruce and 1.3 mg/g for p<strong>in</strong>e (BMELF 1997).<br />

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