Jcd. Milton et al., CL-36 IN THE LAURENTIAN GREAT-LAKES BASIN, Nuclear instruments & methods in physics research. Section B, Beam interactions with materials and atoms, 92(1-4), 1994, pp. 440-444
We have measured the relative concentration of Cl-36 in the five major
lakes of the Laurentian Great Lakes by AMS techniques at the Chalk Ri
ver TASCC facility. The ratio of Cl-36 to stable chloride decreases fr
om 1300 CLU (1 CLU is a ratio of Cl-36/Cl of 1 x 10(-15)) in Lake Supe
rior to 300 CLU in Lake Ontario. However, the salt content increases r
apidly from Superior to Ontario so that the concentration of Cl-36 inc
reases from a low of 3.3 +/- 0.3 x 10(7) in Lake Superior to a high of
11.7 +/- 1.7 x 10(7) atoms/l in Lake Ontario. The results are compare
d to a model that includes the contribution of Cl-36 from the bomb tes
ts in the 1950s as determined from ice-core data taken in Greenland. I
t is found that there is too little Cl-36 in Lake Superior to be consi
stent with current ideas on Cl-36 in precipitation.