68-15 Phosphorus Plant Availability and Spatial Variability in Northern Siberian Permafrost-Affected Soils.
See more from this Division: SSSA Division: Pedology
See more from this Session: Pedology: I (includes student competition)
Abstract:
In this research, we investigate the influence of permafrost thawing on decomposition rates, spatial variability and availability of phosphorus (P) for plants in permafrost-affected soils at the taiga-tundra boundary ecosystem in the northern Siberia.
The spatially referenced soil samples were taken with a soil corer (50 mm Ø, 34 cm long) at six sites with different active layer depths at the Little Grawijka Creek catchment (67°28.933’ N, 86°25.682’ E), Krasnoyarsk Krai, Russian Federation. In total, 732 soil samples were collected; 122 soil samples per site from two depth increments, 0-10 cm and 10-30 cm. Four P fractions (NaHCO3-Pi; NaOH-Pi; HCl-Pi and H2SO4-Pi fractions) and the total P were measured using the sequential P fractionation method, based on the Hedley et al. (1982) and modified by Kuo (1996), on a continuous-flow analyzer.
Plant nutrient deficiency symptoms were observed at the sites with a shallow active layer (AL) during field work, which were confirmed by lower plant-available P concentrations (6-48 mg/kg) in contrast to the permafrost soils with a deeper AL (5-81 mg/kg). However, the total P concentrations are higher in soils with a shallow AL (209-683 mg/kg) than with a deep AL (170-525 mg/kg). The spatial variability of P decreases on the sites with a deeper AL as a result of permafrost thaw. In conclusion, permafrost thawing increases plant‐available P in permafrost soils leading to an increase in abundance of site-specific vascular species.
See more from this Division: SSSA Division: Pedology
See more from this Session: Pedology: I (includes student competition)