Cheesman,A.W., Dunne,E.D., Turner,B.L. and Reddy,K.R.(2010): Soil phosphorus forms in hydrologically isolated wetlands and surrounding pasture uplands. J. Environ. Qual., 39, 1517-1525.

『水文学的に隔離された湿地とそれを取り巻く牧草の高地における土壌リンの形態』


(Abstract)
 Newly created and restored wetlands play an important role in sequestering excess nutrients at the landscape scale. In evaluating the long-term efficacy of nutrient management strategies in increase wetland capacity for sequestering P, information is needed on the forms of P found across the upland-wetland transition. To assess this, we studied soils (0-10 cm) from four wetlands within cow-calf pastures north of Lake Okeechobee, FL. Wetlands contained significantly (P<0.05) greater concentrations of organic matter (219 g C kg-1), total P (371 mg P kg-1), and metals (Al, Fe) relative to surrounding pasture. When calculated on an aerial basis, wetland surface soils contained significantly greater amounts of total P (236 kg ha-1) compared with upland soils (114 kg ha-1), which was linked to the concomitant increase in organic matter with increasing hydroperiod. The concentration of P forms, determined by extraction with anion exchange membranes, 1 mol L-1 HCl, and an alkaline extract (0.25 mol L-1 NaOH and 50 mmol L-1 ethylenediaminetetraacetic acid [EDTA]) showed significant differences between uplands and wetlands but did not alter as a proportion of total P. Speciation of NaOH-EDTA extracts by solution 31P nuclear magnetic resonance spectroscopy revealed that organic P was dominated by phosphomonoesters in both wetland and pasture soils but that myo-inositol hexakisphosphate was not detected in any sample. The tight coupling of total C and P in the sandy soils of the region suggests that the successful management of historically isolated wetlands for P sequestration depends on the long-term accumulation and stabilization of soil organic matter.』

Abbreviations
(Introduction)
Materials and methods
 Site description
 Soil sampling
 Hydroperiod determination
 Soil physical and chemical properties
 Phosphorus characterization
 Solution 31P NMR spectroscopy
 Data analysis
Results and discussion
 Soil physicochemical characteristics
 Soil phosphorus pools
 Solution 31P NMR spectroscopy
 Impact of hydroperiod
 Phosphorus storage
Conclusions
Acknowledgments
References

※リンの抽出には、Reddy et al.(1998)などを使用。


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