Measurements of 18O‐Pi uptake indicate fast metabolism of phosphate in tree roots

Phosphorus (P) nutrition of beech ecosystems depends on soil processes, plant internal P cycling and P acquisition. P uptake of trees in the field is currently not validated due to the lack of an experimental approach applicable in natural forests. Application of radiolabelled tracers such as ³³P and ³²P is limited to special research sites and not allowed in natural environments. Moreover, only one stable isotope of P, namely ³¹P, exists. One alternative tool to measure P acquisition in the field could be the use of ¹⁸O‐labelled ³¹P‐phosphate (³¹P¹⁸O₄ ^3?). Phosphate (P_i) uptake rates calculated from the ¹⁸O enrichment of dried root material after application of ³¹P_i ¹⁸O₄ ^3? via nutrient solution was always lower compared to ³³P incorporation, did not show increasing rates of P_i uptake at P deficiency under controlled conditions, and did not reveal seasonal fluctuations in the field. Consequently, a clear correlation between ³³P‐based and ¹⁸O‐based P_i uptake by roots could not be established. Comparison of P_i uptake rates achieved from ³³P‐P_i and ¹⁸O‐P_i application led to the conclusion of high P_i metabolism in roots after P_i uptake. The replacement of ¹⁸O by ¹⁶O from water in ¹⁸O‐P_i during root influx, but most probably after P_i uptake into roots, due to metabolic activities, indicates high and fast turnover of P_i. Hence, the use of ¹⁸O‐P_i as an alternative tool to estimate P_i acquisition of trees in the field must consider the increase of ¹⁸O abundance in root water that was disregarded in dried root material.