caa a22 4500 463208781 CHVBK 20180405153134.0 cr unu---uuuuu 170326e20070301xx s 000 0 eng 10.1007/s10705-006-9066-2 doi (NATIONALLICENCE)springer-10.1007/s10705-006-9066-2 The Olsen P method as an agronomic and environmental test for predicting phosphate release from acid soils [Elektronische Daten] [Maria Horta, José Torrent] The role of soil phosphorus (P) in the eutrophication of fresh water systems is well established. It is crucial therefore to assess the potential loss of P from soil in the various scenarios where soil can come into contact with water. To date, such assessment has often been based on soil P tests that are used for agronomic purposes (e.g. fertilizer recommendations). The purpose of this work was to examine the usefulness of one such test (viz. the Olsen test, which is based on extraction with bicarbonate) for predicting not only the amount of soil P available to plants, but also that which can be desorbed to water in a group of 32 Portuguese soils, of which 29 were acid and 3 calcareous. To this end, we (i) assessed the total amount of phytoavailable P in soil by successively pot-cropping Chinese cabbage, buckwheat and rye; and (ii) measured the amount of phosphate-P desorbed to a dilute electrolyte mimicking fresh water over periods of up to 218days at soil:solution ratios of 1:100, 1:1000 and 1:10000. Total phytoavailable P and Olsen P were found to bear a quadratic relationship, with Olsen's extractant underestimating the content in phytoavailable P of soils with high Olsen P contents relatively to soils with low contents. The "change point” at which phytoavailable P began to increase rapidly per unit change in Olsen P was 53mg Olsen Pkg−1 soil. For the acid soils, a significant quadratic relationship was found between the amount of P desorbed to water and Olsen P at the three soil:solution ratios studied. However, these relationships became less significant when only the soils with an Olsen P value of less than 50mgkg−1 were considered. For the acid soils, the change point at which P input to water began to increase rapidly per unit change in Olsen P was 20, 61 and 57mgkg−1 at the 1:100, 1:1000 and 1:10000 ratio, respectively. At comparable Olsen P values, the calcareous soils released more phosphate to water than the acid soils. On the basis of our results, we suggest the following environmental threshold values for Olsen P in acid soils: 20mgkg−1 for P desorption scenarios where the soil:solution ratio is high (e.g. drainage water) and 50mgkg−1 for desorption scenarios where the soil:solution ratio is low (e.g., runoff, water in reservoirs). Both values are higher than the agronomic threshold above which plants are well supplied with P. Springer Science+Business Media B.V., 2006 Acid soils nationallicence Eutrophication nationallicence Olsen P nationallicence Phosphate nationallicence Phosphorus nationallicence Soil P test nationallicence Horta Maria Escola Superior Agrária, Quinta Sra., 6000, Mércules, Castelo Branco, Portugal aut Torrent José Departamento de Ciencias y Recursos Agrícolas y Forestales, Universidad de Córdoba, Edificio C4, Campus de Rabanales, 14071, Cordoba, Spain aut Nutrient Cycling in Agroecosystems Kluwer Academic Publishers 77/3(2007-03-01), 283-292 1385-1314 77:3<283 2007 77 10705 https://doi.org/10.1007/s10705-006-9066-2 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/s10705-006-9066-2 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Horta Maria Escola Superior Agrária, Quinta Sra., 6000, Mércules, Castelo Branco, Portugal aut NATIONALLICENCE 700 1- Torrent José Departamento de Ciencias y Recursos Agrícolas y Forestales, Universidad de Córdoba, Edificio C4, Campus de Rabanales, 14071, Cordoba, Spain aut NATIONALLICENCE 773 0- Nutrient Cycling in Agroecosystems Kluwer Academic Publishers 77/3(2007-03-01), 283-292 1385-1314 77:3<283 2007 77 10705 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer