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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.
l-liter polyethylene bottles.
2.1

Water samples were collected in

PROCEDURES AT THE LABORATORY
The edible portions of the food plants were separated from the in-

edible 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

Samples of supporting plant systems and grass were pre-

.

'

for counting.

pared in the same fashion,

Fresh water samples were acidified and evaporated to dryness.
The residue was taken up in water and theslurry transferred to a

planchet for drying, weighing, and counting.

The radioactivity was

isolated from ocean water samples by (a) buffering with NH,C1 to hold
magnesium in solution, and (b) precipitating the natural calcium with

Na,CO,.

The resultingflocculation was allowed to settle overnight and

the bulk of the supernatant was removed by suction or decantation.

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.

The

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 dried

overnight at 110°C, ashed for 24 hr at 500°C, pulverized, and mounted

in aluminum planchets.

DOE ARCHIVES

After mounting, the samples were counted with a gas-flow propor-

tional counter at 26 per cent geometry as determined with a U,O

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

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