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Original Articles

TETANY POTENTIAL OF ORCHARDGRASS AND TALL FESCUE AS INFLUENCED BY FERTILIZATION WITH DAIRY MANURE OR COMMERCIAL FERTILIZER

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Pages 1501-1525 | Published online: 14 Feb 2007
 

ABSTRACT

The main objective of this study was to compare potassium (K), calcium (Ca), and magnesium (Mg) utilization and grass tetany potential of orchardgrass (Dactylis glomerata L.) and tall fescue (Festuca arundinaceae Schreb.) fertilized with dairy manure or commercial fertilizer. The study was conducted from 1994 through 2000 in Willsboro, NY on a Kingsbury clay soil (very-fine, illitic, mesic Aeric Ochraqualf) of somewhat poor drainage. The design was a split-plot in a randomized complete block with two manure rates (16.8 Mg ha−1 and 33.6 Mg ha−1) and one fertilizer treatment (84 kg N ha−1 at spring greenup and 56 kg N ha−1 prior each regrowth harvest) as the main plots and grass species as subplots replicated six times. Potassium concentration and uptake increased after two years of manure application compared to commercial fertilizer treatment and residual effects of manure were large at least three years following manure application. Calcium concentration and uptake decreased after two years of manure application compared to the commercial fertilizer treatment, but there were no differences in treatments three years after manure application had ceased. Magnesium concentration and uptake at the high manure rate did not differ from fertilizer treatment in all years. Orchardgrass was more grass tetany prone than tall fescue as a result of dairy manure application. The K/(Ca+Mg) ratio in plant tissue was as high as 3.26 for orchardgrass and as high as 2.11 for tall fescue for spring harvests at the highest manure rate. The K/(Ca+Mg) ratio in plant tissue was in the range of 0.34–1.74 (below the 2.20 critical level) for all three years with no manure application. Soil K increased in manure treatments from an initial 76.8 kg ha−1 (1993) to 171.7 kg ha−1 (1997) in the highest manure treatment. After three years of no manure applications, soil K had been reduced to the initial level.

ACKNOWLEDGMENTS

The authors are grateful to Mike Davis, Mike LaDuke, Del Meseck, and Norm Wade for their help with field experiments. Samuel Beer is gratefully acknowledged for his assistance in laboratory analyses. Karen Grace-Martin (Office of Statistical Consulting in the Division of Nutritional Sciences at Cornell University) consulted on statistical analyses. Financial support for this study was provided by the Northern New York Agricultural Development Program, Cornell University.

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