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a Norwegian Centre for Soil and Environmental Research, Jordforsk, Frederik A. Dahls vei 20, N-1432 Aas, Norway
b USDA-ARS, Pasture Systems and Watershed Management Research Unit, Curtin Road, University Park, PA16802-3702
* Corresponding author (marianne.bechmann{at}jordforsk.no)
Received for publication November 8, 2004. Concern over nonpoint source P losses from agricultural lands to surface waters in frigid climates has focused attention on the role of freezing and thawing on P loss from catch crops (cover crops). This study evaluated the effect of freezing and thawing on the fate of P in bare soils, soils mixed with dairy manure, and soils with an established catch crop of annual ryegrass (Lolium multiflorum L.). Experiments were conducted to evaluate changes in P runoff from packed soil boxes (100 by 20 by 5 cm) and P leaching from intact soil columns (30 cm deep). Before freezing and thawing, total P (TP) in runoff from catch-cropped soils was lower than from manured and bare soils due to lower erosion. Repeated freezing and thawing significantly increased water-extractable P (WEP) from catch crop biomass and resulted in significantly elevated concentrations of dissolved P in runoff (9.7 mg L1) compared with manured (0.18 mg L1) and bare soils (0.14 mg L1). Catch crop WEP was strongly correlated with the number of freezethaw cycles. Freezing and thawing did not change the WEP of soils mixed with manures, nor were differences observed in subsurface losses of P between catch-cropped and bare soils before or after manure application. This study illustrates the trade-offs of establishing catch crops in frigid climates, which can enhance P uptake by biomass and reduce erosion potential but increase dissolved P runoff.
Abbreviations: DRP, dissolved reactive phosphorus FTC, freeze/thaw cycle ICP-AES, inductively coupled plasmaatomic emission spectrometry SS, suspended solids TP, total phosphorus WEP, water extractable phosphorus
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