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                                                               Chapter 7 Obtaining and Preparing Samples for Analysis  197





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                                   Sea bottom                                           Figure 7.5
                                    Sedimentary layers                                  Schematic diagram of grab sampler. When
                                                                                        the sampler reaches the sediment, the jaws
                                                                                        of the grab sampler are closed, collecting a
                                                                                        sample of the sediment.




                 Sample Collection  Solids are usually heteroge-
                 neous, and samples must be collected carefully if
                 they are to be representative of the target popula-
                 tion. As noted earlier, solids come in a variety of
                 forms, each of which is sampled differently.
                     Sediments from the bottom of streams, rivers,
                 lakes, estuaries, and oceans are collected with a bot-
                 tom grab sampler or with a corer. Grab samplers are
                 equipped with a pair of “jaws” that close when they
                 contact the sediment, scooping up sediment in the
                 process (Figure 7.5). Their principal advantages are
                 ease of use and the ability to collect a large sample.
                 Disadvantages include the tendency to lose finer-
                 grained sediment particles as water flows out of the
                 sampler and the loss of spatial information, both lat-
                 erally and with depth, due to mixing of the sample.
                     An alternative method for sampling sediments
                 uses a cylindrical coring device (Figure 7.6). The
                 corer is dropped into the sediment, collecting a col-
                 umn of sediment and the water in contact with the
                 sediment. With the possible exception of sediment
                 at the surface, which may experience mixing, sam-
                 ples collected with a corer maintain their vertical
                 profile. As a result, changes in the sediment’s com-
                 position with depth are preserved. The main disad-
                 vantage to a corer is that only a small surface area is
                 sampled. For this reason sampling with a corer usu-                    Figure 7.6
                 ally requires more samples.
                                                                                        Schematic diagram of a piston corer in
                     Soil samples collected at depths of up to 30 cm are easily collected with  operation. The weight of the corer is
                 scoops or shovels, although the sampling variance is generally high. A better  sufficient to cause its penetration into the
                 method for obtaining soil samples near the surface is to use a soil punch. This  sediment, while the upward motion of the
                                                                                        piston allows water pressure to help force
                 thin-walled steel tube retains a core sample when it is pushed into the soil and  the sediment column into the barrel of the
                 removed. Soil samples collected at depths greater than 30 cm are obtained by  corer.
                 digging a trench and collecting lateral samples with a soil punch. Alternatively,
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