Abstract
The potential effects of freezing on phosphorus (P) chemistry in Finnish soils are not well known. We studied the effects of multiple freeze-thaw cycles on soil P chemistry in a laboratory incubation experiment with one organic and one mineral surface soil. The soils were incubated at +5°C or at alternating +5/20°C temperatures for 24 weeks, either without amendment or amended with pig slurry or with commercial compound fertilizer (NPK 2039). After incubation, the soils were analyzed for water-soluble reactive and unreactive P, and acid ammonium acetate soluble P (PAAA). Freezing and thawing of soils during the incubation had no significant effect on any of the water-soluble P fractions or PAAA. The outcome was most likely a consequence of the good P status of the soils, which masked the gentle effects of freezing. According to these results, the time of soil sampling (fall vs. spring) has no effect on P test results on soils with a good P status. Concentrations of soluble P after incubation were roughly twice as high in the slurry treatments than in the fertilizer treatments, demonstrating potentially better long-term availability of slurry P.;
Highlights
Phosphorus (P) is a critical nutrient in agricultural soils, both in terms of crop growth and environmental effects of production
The effect of freeze-thaw cycles on soil P in the organic and mineral soils amended with pig slurry or NPK fertilizer was investigated in a laboratory incubation experiment
A possible explanation for the insignificant effects of freezing in this experiment is the long incubation time that allowed effective sorption of P, which led to small recoveries of water-extractable P (Table 4) and probably increased the variability of the results
Summary
Phosphorus (P) is a critical nutrient in agricultural soils, both in terms of crop growth and environmental effects of production. A multitude of factors affect soil P status and P fertilization. Freezing of soil is possibly one of the factors influencing soil P chemistry at Nordic conditions, yet not well examined. Freezing of soil is known to affect soil conditions through various physical, physico-chemical, and biological mechanisms (Edwards and Cresser 1992). The effects of freezing on the physical properties of soil (Miller 1980) have been studied more extensively than the mechanisms affecting soil chemistry. In Finland, where most soils freeze annually, the effects of freezing on soil physics have created interest (Sillanpää 1961, Kivisaari 1979), but hard-
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