TY - JOUR
T1 - Long-term trends in phosphorus leaching and changes in soil phosphorus with phytomining
AU - Svanbäck, A.
AU - Ulén, B.
AU - Bergström, L.
AU - Kleinman, P. J.A.
N1 - Publisher Copyright:
Copyright © 2015 Soil and Water Conservation Society. All rights reserved.
PY - 2015/3/1
Y1 - 2015/3/1
N2 - Few mitigation strategies exist to reduce phosphorus (P) losses in leachate once soil P has built up. "Phytomining," or harvesting a crop without application of fertilizer P to create a negative P balance, has been proposed as a strategy for lowering soil P levels and preventing P loss to runoff and leachate. In this study crops were grown and harvested over 7 to 16 years in undisturbed soil columns (105 cm [41 in] deep) with contrasting textures (loamy sand, sandy loam, silty clay loam, and clay) and high P levels, while P loss in leachate was measured. Soil test P in the topsoil (0 to 20 cm [0 to 8 in] depth) was significantly decreased from the beginning to the end of the study for all soils, while a significant decreasing trend in dissolved reactive P in leachate was only observed in one soil. Downward movement of P from the topsoil to deeper layers was indicated to occur in three out of four soils. Although phytomining lowered soil test P by 11% to 37% in topsoils over the 7 to 16 year period of the study, results indicate that soils with P content well above agronomic optimum may take a much longer time to reach the agronomic optimum.
AB - Few mitigation strategies exist to reduce phosphorus (P) losses in leachate once soil P has built up. "Phytomining," or harvesting a crop without application of fertilizer P to create a negative P balance, has been proposed as a strategy for lowering soil P levels and preventing P loss to runoff and leachate. In this study crops were grown and harvested over 7 to 16 years in undisturbed soil columns (105 cm [41 in] deep) with contrasting textures (loamy sand, sandy loam, silty clay loam, and clay) and high P levels, while P loss in leachate was measured. Soil test P in the topsoil (0 to 20 cm [0 to 8 in] depth) was significantly decreased from the beginning to the end of the study for all soils, while a significant decreasing trend in dissolved reactive P in leachate was only observed in one soil. Downward movement of P from the topsoil to deeper layers was indicated to occur in three out of four soils. Although phytomining lowered soil test P by 11% to 37% in topsoils over the 7 to 16 year period of the study, results indicate that soils with P content well above agronomic optimum may take a much longer time to reach the agronomic optimum.
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U2 - 10.2489/jswc.70.2.121
DO - 10.2489/jswc.70.2.121
M3 - Article
AN - SCOPUS:84924588129
SN - 0022-4561
VL - 70
SP - 121
EP - 132
JO - Journal of Soil and Water Conservation
JF - Journal of Soil and Water Conservation
IS - 2
ER -