A negative influence of manure on calcareous soils

Summary On a soil rich in CaCO₃ in a semiaride climate in Algeria a hard soil layer, impermeable for plant roots, was formed in a depth of 20–40 cm after farmyard manure application and irrigation. To find the reason soil samples of this field were taken and leaching experiments were carried out in the laboratory, with the result that much more Caions and HCO₃-ions were leached out of the soils with farmyard manure application than from the soils without manure. Probably the high amount of CO₂, being liberated by the organic matter, and the irrigation water dissolved the CaCO₃ in the soil, and the formed Ca- and HCO₃-ions followed the movement of water in the soil. Where the Ca(HCO₃)₂ reached soil layers with a less amount of CO₂, CaCO₃ precipitated and formed the hard soil layer. In order to avoid the formation of such calcareous crusts on irrigated, limy soils in a dry climate it is recommended to fertilize rather often small quantities instead of rarely big quantities of farmyard manure.