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In Situ and Remote Methods for Resource Characterization Chapter | 7 185


             and so can remain on station for extended periods of time, sampling around the
             clock.
                Various forms of vessel sampling are introduced in the following sections.
             However, one form of vessel measurement that has already been covered is a
             hull-mounted ADCP (Section 7.1.4). Therefore, this is not considered further in
             this section.



             7.4.1 Vertical Profiling

             In many circumstances, it is useful to make measurements that resolve the
             vertical structure of the water column. The most widely used instrument for
             vertical profiling is the conductivity, temperature, and depth (CTD) (Fig. 7.18).
             A CTD consists of a cluster of sensors that measure properties of the water
             column and either log internally (for subsequent download) or, more frequently,
             transmit the data directly to the ship through a data cable attached to the
             instrument package. The CTD is lowered on a steel cable to the sea bed,
             and variables continuously sampled throughout the water column. A CTD
             measures the electrical conductivity and temperature of the water, and from
             these two properties salinity can be calculated. The depth of each measurement
             is determined by a pressure sensor. Although regions of strong wave and tidal
             activity that could be suitable for generating electricity are generally well-
             mixed, there will be some amount of periodic (e.g. due to regions of freshwater
             influence) or seasonal stratification. Further, the density of the water is required
             to make accurate calculations of the marine energy resource and to provide
             a more thorough characterization of the resource than velocity measurements
             alone will provide.
                It is common for other instruments to be integrated into a CTD cluster, such
             as a transmissometer or optical backscatter (OBS) (both measure suspended
             sediment concentrations), or instruments that measure biological properties
             such as dissolved oxygen or chlorophyll fluorescence (an indication of the
             concentration of phytoplankton in the water column). In addition, an instrument
             of the design shown in Fig. 7.18 allows water sampling bottles to be added to the
             CTD. The operator can fire these bottles at predetermined water depths to collect
             water samples for subsequent processing; for example, the water samples can be
             filtered for either SPM or chlorophyll concentrations to calibrate the electronic
             SPM and chlorophyll sensors, respectively.



             7.4.2 Point Sampling
             Ships are useful platforms for making point measurements of dynamical water
             properties that vary both temporally and spatially (e.g. plankton), and properties
             of the sea bed that could be considered relatively static over longer timescales
             (e.g. sea-bed sediments).
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