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Updated: Mar 25, 2026

Measuring Phosphorus Release in Laboratory Microcosms for Water Quality Assessment
Published on: July 22, 2019
Phosphorus resorption by young beech trees and soil phosphatase activity as dependent on phosphorus availability
Kerstin Hofmann1, Christine Heuck1, Marie Spohn2
1Department of Soil Ecology, Bayreuth Center of Ecology and Environmental Research (BayCEER), University of Bayreuth, Bayreuth, Germany.
Forests with low phosphorus (P) availability enhance P recycling through efficient leaf resorption and increased acid phosphatase activity. Fertilization impacts P recycling differently based on soil P levels.
Area of Science:
- Forest Ecology
- Plant Physiology
- Soil Science
Background:
- Decreasing foliar phosphorus (P) concentrations in Fagus sylvatica L. forests indicate potential P limitation.
- Understanding P recycling is crucial for forest health and sustainable management.
Purpose of the Study:
- To investigate phosphorus (P) recycling mechanisms in Fagus sylvatica L. forests with contrasting soil P availability.
- To assess the impact of P fertilization on P resorption and phosphatase activity.
Main Methods:
- Mesocosm experiment using juvenile Fagus sylvatica L. trees and soils from P-poor and P-rich forest sites.
- Measurement of P resorption efficiency from senesced leaves.
- Assay of acid and alkaline phosphatase activity in rhizosphere and bulk soil.
Main Results:
- P resorption efficiency was significantly higher (70%) in P-poor sites compared to P-rich sites (48%).
- P fertilization reduced P resorption efficiency in P-poor sites but not in P-rich sites.
- Acid and alkaline phosphatase activities were higher in the rhizosphere of P-poor soils. Acid phosphatase activity was concentrated in the rhizosphere in P-poor soils, and in bulk soil in P-rich soils.
Conclusions:
- Fagus sylvatica demonstrates enhanced P resorption efficiency under low soil P availability.
- Acid phosphatase activity in the rhizosphere is a key indicator of P limitation in Fagus sylvatica forests.
- Microbial phosphatases play a more significant role in P cycling in P-rich soils compared to P-poor soils.
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