LAND-USE AND FERTILIZATION EFFECTS ON P-FORMS IN 2 EUROPEAN SOILS - RESIN EXTRACTION AND P-31-NMR ANALYSIS

Macroporous anion-exchange resin extraction and P-31-NMR spectroscopy of dialysed NaOH extracts were used to investigate the effects of land use (Taubenberg, Bavaria: spruce forest, deciduous forest, permanent grass, arable) and fertilization (Askov, Denmark: unmanured, mineral f ertilizer, animal manure) on forms of phosphorus in soil with emphasis on the potentially labile organic (P-o) and inorganic (P-i) pools. Ca rbon content ranged from 12.5-118.1 g kg(-1) and total P (P-t) content from 511 to 2063 mg kg(-1). For all soils, the C:P-o ratios of SOM de creased in the order: whole soil, 150:1-44:1; alkali extract, 57:1-41: 1; resin extract, 20:1-9:1; suggesting an increasing P functionality o f the OM with increasing P-o lability. Analysis of functional relation showed a close relation between resin P-o and P-31-NMR estimates for diester-P including teichoic acid-P, indicating that these species con tributed significantly to the labile P-o pool as determined by the res in method. The most marked effects of land-use were an increase in P-i under grass and arable, a concurrent sequestration of P-o and SOM und er grass, and a depletion of P-o under arable. The amount of resin P-i appeared to be a function primarily of fertilization, and amounted to around 100 mg kg(-1) in the fertilized soils irrespective of the SOM content and P source. The forest soil and the unfertilized agricultura l soil had much smaller resin P-i values. The soil under grass had the largest amounts in resin P-o and diester-P including teichoic acid-P, indicating a rapid turnover of P-o with build-up of a large potential ly labile, microbially derived P-o pool. P-31 NMR also showed large pr oportions of labile P-o species in soils where microbial activity is r estrained by acidity (Taubenberg spruce forest, phosphonates) or where highly microbially altered OM is relatively enriched (Taubenberg arab le, diester-P including teichoic acid-P). We conclude that the resin u sed in this study isolates a structurally and functionally reasonably uniform pool of potentially labile soil P-o.