CHAPTER

2

GROSS ACTIVITY IN PLANTS, SOIL, CORAL, ALGAE, AND WATER
At the time of their collection in the field, the representative plant,
soil, coral, and algae samples were placed in individual plastic bags
for shipment to this laboratory. Water samples were collected in
l-liter polyethylene bottles.
2.1

PROCEDURES AT THE LABORATORY

The edible portions of the food plants were separated from the inedible portions with every precaution being taken to ensure a low probability of cross-contamination. Weighed samples of the food were
dried at 110°C and then ashed in a muffle furnace at 500°C. The ash
was transferred to tared aluminum planchets, weighed, and prepared
for counting. Samples of supporting plant systems and grass were prepared in the same fashion.
Fresh water samples were acidified and evaporated to dryness.
The residue was taken up in water and the slurry transferred to a
planchet for drying, weighing, and counting. The radioactivity was

isolated from ocean water samples by (a) buffering with NH,Cl1 to hold
magnesium in solution, and (b) precipitating the natural calcium with

Na,CO,.

The resultingflocculationwas allowed to settle overnight and

the bulk of the supernatant was removed by suction or decantation. The
remaining slurry was transferred to lustroid tubes and centrifuged. The
precipitate was washed once with water, transferred to an aluminum
planchet, and dried at 110°C. Analysis of the supernatants from the
more active samples showed that recovery of activity by precipitation
ran from 80 to 90 per cent.
Soil and lagoon-bottom silt samples were dried and mounted in
aluminum planchets for counting. Coral and algae samples were cried

overnight at 110°C, ashed for 24 hr at 500°C, pulverized, and mounted
in aluminum planchets.

After mounting, the samples were counted with a gas-flow proportional counter at 26 per cent peometry as determined with a U,30%
standard or with a 1.9 mg/sq cm, end-window, G-M tube and scaler at
14 per cent geometry as determined with a U,O, standard. Absorption
and scattering corrections were determined empirically by counting
varying weights of individual samples and extrapolating the specific

pot

arcnsvee

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