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pack over a large flat paved parking area was chosen as a
test site and found to contain consistent one finger resist-
ancesnowover auniform 2.1 m depththroughouttheentire
area. Footpenetration wasabout 2-3 cm. Theforcerequired
to penetrate the snow with a probe was consistent and
typical of an avalanche deposit.
The areawas divided into a series of identical corridors
the width of a 9 member probe line and 50 m in length.
The probers were instructed to probe at a realistic rate
which they felt they could maintain for an extended pe-
riod ("at least an hour non-stop"). The number of steps
was controlled and recorded andthus the exact number of
probe holes could be determined. The time for the team to
complete each 50 metre stretch was recorded.
Four different sets of tests were conducted, each em-
ploying a variation of probing technique. Each 50 metre
plot was repeated four times and the probing times were
averaged.
Two basic techniques were compared. Two tests em-
ployed 9 probers in the traditional coarse probe spacing.
The alternative technique employed 3 probers spaced
openly to cover thesame areaas above howevereachprober
placed 3 holes per step. This is a variation of the open-
spaced techniquedescribed in Perla andMartinelli (1976, Figure 2 Probe spacing in vertical plane for 3-hole-per-
step probing. Optimal spacing occurs approximately 1 m
p. 192) and McClung and Schaerer (1993, p. 191). below surface. All dimensions in cm.
Bilgiri probes were used. Fulldepth probes employed 4
sections (3.25 m). The probes were shortenedto 3 sections THREE-HOLE-PER-STEP PROBING
(2.45 m) for three of the tests. One test was full depth (to The open-spaced technique illustrated in McClung and
ground) 2.1 m. The remainder were to a depth of 1.5 m. Schaerer (1993, p. 191) shows each rescuer probing twice
The probes were marked with tape to indicate 1.5 m. per step. In the technique employed in these tests, each
The usual probemaster was employed to direct the 9 person probed three times each step, to the left, in center,
member probe line. In one of the open spaced tests the and then right.
team was instructed to proceed at their own individual In reality if the prober reaches to the side, the probe
paces. will usually enter the snow at an angle. If he tries to main-
tain the 75 cm spacingthe anglemay be 10-15 degreesfrom
FIELD TEST RESULTS vertical. However if the probers space themselves finger-
Times were averaged for each technique and the rates of tip to finger-tip apart (~175 cm) the resulting lateral spac-
probing were calculated(table 1). ing of probe holes is reducedto about 60 cm at a depth of
1 m andthe anglesof the probe holeson eachside are slight.
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