“…Natural environmental radioactivity arises mainly from primordial radionuclides, such as 40 K, and the radionuclides from the 232 Th and 238 U series, and their decay products are considered to be the main contributor to internal radiation dose (Yassine et al, 2003;Bunzl and Trautmannsheimer, 1999;Merian, 1991;Sheppard and Evenden, 1988;Aguirre et al, 1997;Al-Masri et al, 2002;Pulhani et al, 2005). Several studies on transfer of natural radionuclides from soil to plant have been carried out in different regions in the world (Aguirre et al, 1997;Simon and Ibrahim, 1987;Tracy et al, 1983;Paul and Pillai, 1986;Pulhani et al, 2005;Veselsky, 1997;Bunzl and Trautmannsheimer, 1999;Martinez-Aguirre and Perianez, 1998;Staven et al, 2003;Ewers et al, 2003;Blanco Rodriguez et al, 2006;Tome et al, 2003). However, there seem to be few data on transfer of natural radionuclides from soil to plant in semiarid environments.…”