The North extreme region of Tunisia is known by deep soil, high and strong agronomic potentialities. However, they are severely affected by the acidity which decreasing the meadows yield level in spite of its important surface. Besides,...
moreThe North extreme region of Tunisia is known by deep soil, high and strong agronomic potentialities. However, they are severely affected by the acidity which decreasing the meadows yield level in spite of its important surface. Besides, during the last decades several of them were converted in permanent meadows essentially cultivated by fescue, by clover and additionally by bluegrass. On all these lands the Forage crops is dependent to soil acidity which limits severely the yield level. Although it showed its ability in several similar regi the North of Tunisia yet. The lime eliminates the bad effects of the acidity by the improvement of soil fertility level and increases, consequently, the meadows capacity production. This study has for objective to evaluate the effect of the lime (CaCO and phosphorus uptake and the bluegrass shoot biomass. A pot trial of liming and mineral fertilization was conducted on the bluegrass cultivated on a arranged in randomized complete blocks design with 3 repetitions. Treatments were combinations of two doses of lime (CaCO 3), two doses of ammonium nitrate (NH (45 % P 2 O 5) and finally, two doses of potassium sulphate of (63 % K alone the lime, allowed to improve substantially nitrogenous and phosphate nutrition as well as the bluegrass shoot biomass. The exclusive effect of mineral fertilizers on these parameters was variable; on the other hand, the combined effect of the lime with three mineral fertilizers increased even more the plant nitrogen and phosphorus content and gave the highest shoot biomass. 1. Introduction The soil acidity limits severely the Tunisian north extreme region lands and meadows productivity. It hinders the soil fertility and offers a hostile environment to the crop growth. Results found by Ferguson (1936) reported that the soil acidity inhibits populating this area. The chemical behaviour of the acid soil is confidentially related to a strong aluminum concentration in the soil solution and on the adsorbing complex (Mehlich, 1948). The proliferation in the soil is often limited by the aluminum toxicity what justifies the low absorption of the nutriment (Adams, 1984). The soil pH is an essential factor in the crop nutrition; low values of the pH reduce the root activity and the nutri reported that the soil acidity decreases the pH below the tolerance threshold of plants, increases the aluminum, the iron, the copper, the zinc and the manganese concentration until toxic levels phosphorus availability and finally inhibits some biological activities such as the nitrification and the atmospheric nitrogen fixation. Organic acids form with the aluminum of the soil solution an insoluble complexes so decreasing its concen (Munns 1965; Maaro 2002; and Mitchell 2004) showed that the calcium (lime) amendment reduces considerably the aluminum in the soil solution and that the decline of the shoot biomass and of the clover recorded with a concentration of 200 micromoles of aluminum ion was significantly reduced