Besides the radioactive contamination on Janet, there was also some chemical contamination by

beryllium contained in rocket engine fuel. The engine was being tested in 1968 on a pad near
Hardtack Station 1312 when it malfunctioned, damaging Station 1312 and contaminating the area
with beryllium. The combination of decontamination efforts at the time of the incident and erosion
since then should have removed most of the beryllium before the radiological cleanup began.
1972 Survey Results

Because of its size and importance to the Enewetak people, Janet was sampled intensively during the

1972 survey. Out of a total of 140 soil sampling locations, ten were profile sampled to 185 em, two

were 125 em profiles, one was a 65 em profile, one was a 35 em profile, and the remaining 126 were

0-15 em core samples. To help investigate relationships between radioactivity in the soil and in the

food chain, a numberof plant and animal samples were taken.

The 239,240py activity in profile samples generally declined steeply with depth, falling to less than 1
BSi/g by 30 em or shallower. Of three locations which were exceptions to the pattern, two had no
39,240py activity greater than 1 pCi/g at depth even though the activity was rising. The third
location with an anomalous pattern was near the Easy and xoRay sites, where buried contamination
wasalready suspected to exist. Table 7-3 summarizes the 239,240 py results for Janet.

The depth distribution of 137Cs and 99Sr was similar to the pattern for 239,240py, although activity

of these two isotopes did not decline_as steeply as 239,240py activity. The one profile which showed
a significant increase in
Cs and 9p activity below 30 cm was the same location near Easy and
X-Ray which had the anomalous 239,240pu depth distribution. Summaries of the 37Cs and 90sr
results are in Tables 7-1] and 7-2, respectively.
In 1975, as part of the follow-up on the 1972 survey, Lawrence Livermore Laboratory established a
garden plot on Janet to study radionuclide uptake in food plants. The results would aid in building
dose-assessment models, and specifically to help determine when Janet might again be suitable for
agriculture and habitation. Additional] soil samples were also collected in the garden area to provide
better information on soil-to-plant transfer coefficients for radionuclides. A study of radionuclides
in groundwater was also begun at this time; this involved drilling several wells and taking water
samples.

Both the garden and groundwater studies continued throughout and beyond the radiological cleanup,

so care was taken during cleanup to try to avoid damageto the study areas.
Surface Characterization

Because Janet wasthefirst island measured with the in situ system, several preliminary experiments

and sets of IMP measurements were done on Janet to develop procedures and evaluate the system.
Details of these early efforts are in Section 6.4. After the initial break-in period, a 25 m grid,

known as the Test Grid, was staked and measured in August 1977 to provide a test of the data
collecting system

and also data for

preliminary

statistical analyses.

Although

the

absolute

coordinates of the Test Grid were never established, its approximate boundaries are shown in Figure
7-65.

As described in Section 6.4, the statistical analysis of the Test Grid data led to the conclusion that
50 m spacing for the Janet grid would give enough data for acceptable estimates. Meanwhile, part

of the west tip of the island had already been staked at 25 m spacing and the IMP had nearly

completed measurements in that area. (This 25 m grid was inadvertently shifted from its intended
location. See Section 6.4). The IMP survey of the 25 m grid was therefore completed at that spacing

in September 1977, and that block of data was handled separately in the statistical analyses. The

remainder of Janet was initially staked and measured at 50 m spacing. The 50 m grid was located

correctly, so it was extended far enough west to makecertain that estimates of TRU activity from
the 25 m and 50 m grids would completely cover the island. It was further concluded that the kriging
method (see Section 5.1) gave acceptable estimates, and the data satisfied the assumptions made in
using this method.

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