“…For example, large quantities of CO2 liberated by the rhizosphere occupants form carbonic acid which causes a solubilization of insoluble, inorganic nutrients, that would not be readily available to the plant. This process effectively increases the supply of assimilable inorganic nutrients such as phcsphcrus, potassium, magnesium, and calcium, and thus improves crop nutrition /AlAvonHAr 1Q'77\ (Ebing and Schuphan, 1979;Kloskowski et al, 1981;Scheunert et al, 1983;Bellin and O'Connor, 1990;Malik and Drennan, 1990;Lee et al, 1991;Nair et al, 1993;Shimp et al, 1993). Enhanced degradation of nonagricultural chemicals has been noted to occur in vegetated soils (Rasolomanana and Balandreau, 1987;Federle and Schwab, 1989;Aprill and Sims, 1990).…”