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Titel Total and extractable Phosphorus concentrations at different depths in a soil fertilized with manure
VerfasserIn Rosane da Silva Días, Cleide Aparecida de Abreu, Roger Manuel Mestas Valero, José Manuel Mirás Avalos, Eva Vidal Vazquez
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250050667
 
Zusammenfassung
A number of extraction methods have been proposed to assess soil phosphorus availability. The aim of this study was to evaluate the phosphorus (P) concentration at several depths in a soil using different techniques. The research was carried out in Ribadeo (Lugo Province, NW Spain). The study area was 625 m2. A total of 36 soil samples were taken in 9 points at the following depths: 0-5; 5-10; 10-20; 20-40 cm. Total P content in soil was determined by microwave digestion with nitric acid, USEPA method 3051. Extractable P was measured by Mehlich-3 extraction followed by two different determination techniques (ICP and colorimetry, M3-ICP and M3-COL, respectively), anion exchange resin (AER) and Olsen (Ol). Data were compared using Tukey’s test and Pearson’s r coefficient. Extracted amounts of P (Table 1) were much higher than expected and they were also relatively high compared to those measured by other researchers in the same region. Note that thresholds for excess P contents using the Mehlich-3 and Olsen methods have been reported as 31 and 21 mg kg-1, respectively. The results obtained in this study exceeded these thresholds in every depth. However, our results were within the range reported by Sharpley et al. (2004), who observed P values extracted by Mehlich-3 within a range of 64 to 2822 mg kg-1 and 407 to 2480 mg kg-1 for total P depending on the type of manure used and at a depth of 0-5 cm. Phosphorus accumulation suggests long-term intensive application of organic manures. Table 1. Soil P concentrations as a function of depth and extraction method. Depth (cm) P Total(mg-ˆ•kg) P M3(mg-ˆ•kg) P AER(mg-ˆ•kg) P Ol(mg-ˆ•kg) ICP COL 0-5 1793 a 664 a 598 a 583,0 a 154,0 a 5-10 1814 a 669 a 607 a 600,0 a 156,0 a 10-20 1633 ab 652 a 606 a 625,0 a 146,0 a 20-40 1453 b 539 b 538 b 491,0 b 119,0 b Total: Total P, M3:Mehlich-3 (ICP and COlL: Colorimetry), AER: Resin and Ol: Olsen. On each column, different letters indicate statistically significant differences according to Tukey test (P -‰¤ 0.05). P values obtained by Mehlich-3 showed significant correlations with those from Olsen and resin methods (r values between 0.64 and 0.82). In addition, P measured by Olsen and resin were significantly correlated (r = 0.69). All the methods, except anion exchange resin, provided highest P concentrations were at the 5-10 cm depth, thought they were not significantly different than those measured at the 0.5 and 10-20 cm depths. At 20-40 cm depth, the significantly lower P concentrations were observed independently of the method used (Table 1). The relatively high concentrations of P at the 20-40 cm depth are thought to be caused by soil mixing during deep plowing, whereas more superficial tillage operations would cause maximum values at the 5-10 cm depth. Based on our results it would be advisable to cease manure additions to the study soil until the P level decreases. Sharpley, A.N., R.W. McDowell, and P.J.A. Kleinman. 2004. Amounts, forms, and solubility of phosphorus in soils receiving manure. Soil Sci. Soc. Am. J. 68:2048–2057.