Effect of soil acidity and nutrient deficiencies on the growth and persistence of subterranean clover in pastures grown on sandy soils near Esperance, Western Australia

Most of the sandy soils near Esperance, W.A., were cleared of native vegetation and sown to subterranean clover in the 1950s and 1960s. Over the past 20-30 years, pH values of the topsoil (1:5, soil: water) have decreased from 6.5-7.0 to 5.0-5.5. The application of 2 t/ha of agricultural lime increased the soil pH (1:5, 0.01 CaCl2) from 5.5 to 5.8, from 4.9 to 5.6, and from 5.1 to 5.5 at three sites that had been sown to subterranean clover for 10, 20 and 40 years respectively. However, lime had no effect on either dry matter production or seed yield of subterranean clover. Additions of calcium in a further experiment also did not affect the seed yield of subterranean clover. Irrespective of the lime treatments, the addition of nutrients (phosphorus, potassium, sulfur, copper, zinc, molybdenum, cobalt, manganese and boron) significantly (P<0.05) improved dry herbage yields by a factor of 1.3, 1.7 and 1.4 at the 10-, 20- and 40-year-old sites. However, the addition of nutrients did not affect seed yields of subterranean clover. In other experiments, the omission of sulfur, potassium and, for the deepest sandy site, phosphorus reduced dry herbage yields by between 10-30%. The omission of molybdenum from treatments of the 20- and 40-year-old pasture reduced herbage yields by 21 and 16% respectively. However, omission of molybdenum in the experiment sited on the 10-year-old pasture did not affect yields. Thus, as the acidification of the sandplain soils continues, molybdenum may become deficient and may limit herbage yields of subterranean clover.