JEQ Journal of Natural Resources and Life Sciences Education
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Published online 1 March 2006
Published in J Environ Qual 35:599-610 (2006)
DOI: 10.2134/jeq2005.0135
© 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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TECHNICAL REPORTS

Surface Water Quality

Soil and Surface Runoff Phosphorus Relationships for Five Typical USA Midwest Soils

B. L. Allen, A. P. Mallarino*, J. G. Klatt, J. L. Baker and M. Camara

Department of Agronomy, Iowa State University, Ames, IA 50011

* Corresponding author (apmallar{at}iastate.edu)

Received for publication April 25, 2005. Excessively high soil P can increase P loss with surface runoff. This study used indoor rainfall simulations to characterize soil and runoff P relationships for five Midwest soils (Argiudoll, Calciaquaoll, Hapludalf, and two Hapludolls). Topsoil (15-cm depth, 241–289 g clay kg–1 and pH 6.0–8.0) was incubated with five NH4H2PO4 rates (0–600 mg P kg–1) for 30 d. Total soil P (TPS) and soil-test P (STP) measured with Bray-P1 (BP), Mehlich-3 (M3P), Olsen (OP), Fe-oxide-impregnated paper (FeP), and water (WP) tests were 370 to 1360, 3 to 530, 10 to 675, 4 to 640, 7 to 507, and 2 to 568 mg P kg–1, respectively. Degree of soil P saturation (DPS) was estimated by indices based on P sorption index (PSI) and STP (DPSSTP) and P, Fe, and Al extracted by ammonium oxalate (DPSox) or Mehlich-3 (DPSM3). Soil was packed to 1.1 g cm–3 bulk density in triplicate boxes set at 4% slope. Surface runoff was collected during 75 min of 6.5 cm h–1 rain. Runoff bioavailable P (BAP) and dissolved reactive P (DRP) increased linearly with increased P rate, STP, DPSox, and DPSM3 but curvilinearly with DPSSTP. Correlations between DRP or BAP and soil tests or saturation indices across soils were greatest (r ≥ 0.95) for FeP, OP, and WP and poorest for BP and TPS (r = 0.83–0.88). Excluding the calcareous soil (Calciaquoll) significantly improved correlations only for BP. Differences in relationships between runoff P and the soil tests were small or nonexistent among the noncalcareous soils. Routine soil P tests can estimate relationships between runoff P concentration and P application or soil P, although estimates would be improved by separate calibrations for calcareous and noncalcareous soils.

Abbreviations: BAP, bioavailable P • BP, Bray-P1 • DPSM3, degree of P saturation based on Mehlich-3 P, Fe, and Al • DPSox, degree of P saturation based on ammonium-oxalate P, Fe, and Al • DPSSTP, degree of P saturation based on soil-test P and a P sorption index • DRP, dissolved reactive P • FeP, P extracted with Fe-oxide-impregnated paper • M3P, Mehlich-3 P • OP, Olsen P • PSI, P sorption index • STP, soil-test P • TPR, total runoff P • TPS, total soil P • WP, water-extractable P




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