Wg. Kiflom et al., Variation of plant p,p '-DDT uptake with age and soil type and dependence of dissipation on temperature, ENVIRON INT, 25(4), 1999, pp. 479-487
The extent to which DDT may be absorbed and translocated from C-14-p,p'-DDT
contaminated soils into cowpeas plant tissues, and the variation of uptake
of p,p'-DDT by the plants in relation to the dissipation of p,p'-DDT in th
e soils was studied using a radioisotope technique for three months (90 d).
Substantial absorption and accumulation of residues was observed for the c
owpeas grown in two different sites, namely, in the coastal province Mombas
a and highland region, Nairobi. The degree of uptake varied with soil type
and growing conditions. Total residue levels ranging from 0.945+/-0.040 mg/
kg to 7.765+/-0.211 mg/kg were obtained for 2 to 12 week old Mombasa plants
. However, Nairobi plant values fell in the range of 1.136+/-0.038 mg/kg to
3.239+/-0.007 mg/kg. The Mombasa plants gave a range of residue levels fro
m 0.800+/-0.065 mg/kg to 6.110+/-0.038 mg/kg and 0.084+/-0.001 mg/kg to 1.3
90+/-0.003 mg/kg for extractable and non-extractable (bound) residue, respe
ctively. The corresponding values for Nairobi samples were 1.034+/-0.011 mg
/kg to 2.241+/-0.014 mg/kg and 0.080+/-0.002 mg/kg to 0.411+/-0.007 mg/kg,
respectively. Further, results suggest that the higher the water retention
by the soil, the higher the rate of evaporation of DDT. Extractable DDT in
soils decreased with temperature while soil-bound DDT increased with temper
ature. Coastal region soil-p,p'-DDT samples indicated p,p'-DDE to be the ma
jor metabolite over a period of 292 d. The levels of DDT decreased with tim
e. The reverse was true for DDE, as expected. First order rate constant for
DDT dissipation in soils was confirmed by half-life measurements. The rate
constants (k), calculated from the data, for Mombasa and Nairobi, were 5.6
x 10(-6) min(-1) and 5.1 x 10(-6) min(-1), respectively. Within a period o
f 90 d, DDT residue in the plants ranged from 0.94 to 7.73 mg/kg, while tha
t in soils ranged from 88.9 to 32.0 mg/kg. (C) 1999 Elsevier Science Ltd.