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Published online 27 October 2006
Published in J Environ Qual 35:2236-2243 (2006)
DOI: 10.2134/jeq2006.0156
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Using Simulated Rainfall to Evaluate Field and Indoor Surface Runoff Phosphorus Relationships

A. R. Guidrya, F. V. Schindlerb,*, D. R. Germanc, R. H. Geldermand and J. R. Gerwingd

a East Dakota Water Development District, 132 B Airport Drive, Brookings, SD 57006
b Chemistry Department, Southwest Minnesota State University, Marshall, MN 56258
c Water Resources Institute, Agricultural Engineering, Box 2120, Room 211, South Dakota State University, Brookings, SD 57007
d Plant Science Department, Agricultural Hall, Box 2207A, South Dakota State University, Brookings, SD 57007


Figure 1
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Fig. 1. Relationship between total dissolved P in runoff [TP(<0.45)] concentrations in surface runoff (mg P L–1) and Olsen-P (mg P kg–1) for simulation method and the (A) Vienna (n = 10), (B) Kranzburg (n = 9), (C) Poinsett (n = 10), and (D) Barnes (n = 10) soils. Olsen-P and surface runoff TP(<0.45) relationships for the field plots and packed boxes were based on 0- to 5-cm probe and bulk soil samples, respectively. {dagger} Regression significant at the P = 0.0001 probability level. {ddagger} Regression significant at 0.001 < P < 0.002 probability level.

 

Figure 2
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Fig. 2. Relationship between outdoor total dissolved P in runoff [TP (<0.45)Field] and indoor total dissolved P in runoff [TP (<0.45)Indoor] concentrations for Vienna, Kranzburg, Poinsett, and Barnes soils. *** Regression significant at the P < 0.001 probability level.

 





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