39-14 A Biologically-Based Approach to Evaluating Soil Phosphorus Availability Across Complex Landscapes.

See more from this Division: SSSA Division: Forest, Range & Wildland Soils
See more from this Session: Forest, Range & Wildland Soils: I (includes student competition)

Monday, November 16, 2015: 1:00 PM
Minneapolis Convention Center, 103 F

Thomas H. DeLuca1, David L. Jones2, Melissa R Pingree1, Helen C Glanville3, Matthew Harris3 and Bridget Emmett4, (1)School of Environmental and Forest Sciences, University of Washington, Seattle, WA
(2)School of the Environment & Natural Resources, Bangor University, Bangor Gwynedd, United Kingdom
(3)School of Environment, Natural Resources and Geography, Bangor University, Bangor, United Kingdom
(4)Centre for Ecology and Hydrology, National Environmental Research Council, Bangor, United Kingdom
Abstract:
Plants employ a range of strategies to increase phosphorus (P) availability in soil. Current soil P extraction methods (e.g. Olsen P), however, often fail to capture the potential importance of rhizosphere processes in supplying P to the plant. This has led to criticism of these standard approaches, especially in non-agricultural soils of low P status and when comparing soil types across diverse landscapes. Similarly, more complex soil P extraction protocols (e.g. Hedley sequential fractionation) lack functional significance from a plant ecology perspective. In response to this, we present a novel procedure using a suite of established extraction protocols to explore the concept of a P protocol based on biologically significant P pools, fluxes and transformations. The biologically based P (BBP) extraction was conducted by using four extractions in parallel:  (1) 10 mM CaCl2 (soluble P); (2) 10 mM citric acid (chelate extractable P); (3) phytase and phosphatase solution (enzyme extractable organic P); (4) 1 M HCl (mineral occluded P). To test the integrated protocol, we conducted the analyses on a total of 204 soil samples collected as part of a UK national ecosystem survey (Countryside Survey) in 1998 and repeated again in 2007. In the survey, Olsen P showed a net decline in national soil P levels during this 10 year period. In accordance with these results, soluble P, chelate extractable P and mineral occluded P were all found to decrease over the 10 year study period. In contrast, enzyme extractable organic P increased over the same period likely due to the accumulation of P as organic inputs to the mineral soil. This new method is simple and inexpensive and therefore has the potential to greatly improve our ability to characterise and understand changes in soil P status across complex landscapes

See more from this Division: SSSA Division: Forest, Range & Wildland Soils
See more from this Session: Forest, Range & Wildland Soils: I (includes student competition)