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Field Sampling<br />

CHAPTER 3<br />

METHODS<br />

Samples for sediment <strong>and</strong> geochronologic analyses were collected by two methods.<br />

Vibracores were used to collect deep sediment samples beneath <strong>the</strong> beach ridges. Additionally,<br />

whenever possible, trenches were excavated into selected ridges. All trenches were oriented<br />

perpendicular to <strong>the</strong> trend <strong>of</strong> <strong>the</strong> ridge crest. A total <strong>of</strong> 18 trenches were excavated. Samples for<br />

OSL dating were obtained by hammering 0.3 m sections <strong>of</strong> aluminum irrigation pipe horizontally<br />

into <strong>the</strong> vertical walls <strong>of</strong> <strong>the</strong> trenches or by subsampling sections <strong>of</strong> <strong>the</strong> aluminum vibracore<br />

tubes.<br />

For this investigation trenching was <strong>the</strong> preferred method <strong>of</strong> sample collection. However,<br />

sediment cores can also provide direct evidence <strong>of</strong> <strong>the</strong> lithologic character <strong>of</strong> <strong>the</strong> sediment.<br />

Vibracoring is one <strong>of</strong> many subsurface sediment acquisition techniques. Samples were collected<br />

by vibrating a core barrel into <strong>the</strong> sediment. By using this method it is possible to obtain cores <strong>of</strong><br />

up to 6.0 m in length in unconsolidated sediments. Vibratory corers have been in use for several<br />

decades <strong>and</strong> techniques have improved through <strong>the</strong> years as field experience has advanced. They<br />

are relatively simple devices comprised <strong>of</strong> a frame, coring tube, <strong>and</strong> drive head that consists <strong>of</strong><br />

ei<strong>the</strong>r a pneumatic, hydraulic or electrical vibrator. For this study a Stow vibrator powered by an<br />

8 horsepower Briggs <strong>and</strong> Stratton gas motor was used. The unit spins a flexible cable at a high<br />

speed that causes <strong>the</strong> unevenly weighted head to vibrate. The head was mounted by U bolts to<br />

an adaptor that was clamped to <strong>the</strong> 8-cm diameter aluminum core barrels. Once maximum<br />

penetration was achieved, <strong>the</strong> top <strong>of</strong> <strong>the</strong> core barrel was filled with water <strong>and</strong> capped. This<br />

created suction when <strong>the</strong> core was extracted <strong>and</strong> prevented <strong>the</strong> movement <strong>of</strong> sediment in <strong>the</strong> core<br />

barrel. A come-along <strong>and</strong> tripod were used to extract each core out <strong>of</strong> <strong>the</strong> ground. For this<br />

investigation, 8-cm diameter aluminum irrigation pipe cut into 3.0 to 6.0 m lengths was used.<br />

Vibracores were not logged because <strong>the</strong>y were opened under reduced light conditions for OSL<br />

sample collection. Figure 3.1 shows <strong>the</strong> sample collection methods employed in this<br />

investigation.<br />

33

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