Abstract

Production of surface casts of earthworms (dominantly Allolobophora caliginosa) varied markedly during 1975. Casting activity was restricted to the April to September period and reached a maximum in early June. Seasonal variations in cast production were attributed to fluctuations in soil moisture and temperature, and in food supply. Although the total P content of casts was essentially constant throughout the year, the inorganic P content decreased from a maximum in May to a minimum in August. The progressive decrease in the amount of inorganic P between May and August is attributed to a reduction in the conversion of organic to inorganic P because of the lower microbial and phosphatase enzyme activity as a result of declining soil temperature. Seasonal variations in the release of inorganic P from casts to solution and in the amounts of rapidly-exchangeable P were more closely related to the seasonal pattern of cast production than to changes in the amount of inorganic P in the casts. In contrast, seasonal changes in the release of inorganic P to solution and in the amount of rapidly-exchangeable P in underlying soil were small. A greater amount of inorganic P was extracted by 0.5 m NaHCO 3 than by water from freshly-deposited casts collected at different times of the year, indicating that NaHCO 3 extracts some chemisorbed inorganic P from casts. Water-extractable inorganic P accounted for approximately 90% of the difference between inorganic P in casts and underlying soil. Consequently, essentially all of the additional inorganic P in casts is retained by a more-physical sorption type. The results obtained are discussed in terms of the likely effects of surface casting on the P cycle in a soil-plant system.

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