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Relation between soil P test values and mobilization of dissolved and particulate P from the plough layer of typical D anish soils from a long‐term field experiment with applied P fertilizers
Author(s) -
Glæsner N.,
Kjaergaard C.,
Rubæk G. H.,
Magid J.
Publication year - 2013
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/sum.12060
Subject(s) - plough , loam , particulates , leaching (pedology) , soil water , chemistry , eutrophication , fertilizer , environmental chemistry , zoology , agronomy , environmental science , soil science , nutrient , biology , organic chemistry
Accumulation of phosphorus ( P ) in agricultural topsoils can contribute to leaching of P which may cause eutrophication of surface waters. An understanding of P mobilization processes in the plough layer is needed to improve agricultural management strategies. We compare leaching of total dissolved and particulate P through the plough layer of a typical D anish sandy loam soil subjected to three different P fertilizer regimes in a long‐term field experiment established in 1975. The leaching experiment used intact soil columns (20 cm diameter, 20 cm high) during unsaturated conditions. The three soils had small to moderate labile P contents, expressed by water‐extractable P (3.6–10.7 mg/kg), Olsen P (11–28 mg/kg) and degree of P saturation ( DPS ) (25–34%). Mobilization of total dissolved P ( TDP ) increased significantly ( P < 0.05) from the intact soil columns with increasing labile P , whereas the increase in particulate P ( PP ) with increasing labile P content was modest and statistically insignificant. We found concentrations up to 1.5 mg TP/L for the plough layer of this typical D anish sandy loam soil. This highlights that even a moderate labile P content can be a potential source of TDP from the plough layer, and that a lower concentration margin of optimum agronomic P levels should be considered.