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The estimation of losses of potassium and magnesium from chalky soils in southern England: laboratory studies
Author(s) -
Heming S. D.,
Rowell D. L.
Publication year - 1997
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/j.1475-2743.1997.tb00570.x
Subject(s) - leaching (pedology) , potassium , soil water , fertilizer , chemistry , magnesium , calcareous , lessivage , throughflow , environmental chemistry , soil science , agronomy , environmental science , geology , paleontology , organic chemistry , biology
. Ten chalk topsoils (0‐25 cm) were repacked into columns in the laboratory. After leaching similar to one year's throughflow in the field, loss of K was equivalent to between 9 and 74kg K/ha. This represented between 3 and 30% of the initial exchangeable K with which loss was poorly correlated. Loss was dependant on the soil solution concentration and was inversely proportional to potassium buffer power. The loss of magnesium in the same columns was between 10 and 22 kg Mg/ha (6‐21% of the initial exchangeable Mg). Magnesium loss was poorly correlated with exchangeable Mg. When KCl fertilizer was incorporated into the soils, the increase in leaching of potassium was 1–35% of the K addition. Application to the top of the column resulted in less leaching than when the K was incorporated. Leaching of magnesium was increased by up to 5 kg Mg/ha. Potassium leaching may be delayed by the underlying A/C horizon but pure chalk, with an extremely low buffer power for K, has little ability to retain K. Extremely calcareous topsoils were the most leaky although in practice it is the organic chalk soils on which it is most difficult to attain adequate K levels. On all chalk soils, maintenance of a high K level with K fertilizer is likely to cause unnecessary long‐term leaching losses. Annual, rather than biennial, fertilizer applications are to be preferred.