The Continuous Sediment Sampling and Analysis System
Scott Noakes - Center for Applied Isotope Studies, University of
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The CAIS survey conducted at Lake Pontchartrain during September 1996 was designed to provide a reconnaissance characterization of the elemental constituents of surficial lakebed sediments, with resulting data used to delineate areas of greatest concern for further, more detailed study. Samples were collected using the CAIS-developed Continuous Sediment Sampling and Analysis System, or CS3 which samples the plume of surficial sediments generated by the movement of a towed sled along the sediment surface. The CS3 sled-mounted submersible pump delivers an uninterrupted stream of sediment slurry to a shipboard processor, where the fine sediment fraction is separated, dewatered, and deposited as a sample on a quartz fiber wafer. Using the USGS vessel R/V G.K. Gilbert, more than 750 surficial sediment samples were collected over a 9-day period, using a close (approximately 1.9 km, or three-quarter mile) grid spacing that covered the entire Lake Pontchartrain area.
CAIS Rapid Survey Systems
The CAIS has been actively involved in the development and application of multi-sensor survey systems for data collection and mapping in aquatic environments for almost two decades. (Noakes and Harding, 1992; Noakes et al., 1991a). The CAIS systems consist of sensors, mounted on a towed sled, which continuously measure parameters at the sediment/water interface and collect surficial sediment samples as the vessel is underway. Shipboard instrumentation for data and sample processing, analysis, and storage enable real time or near real time mapping of bathymetric, radiometric, elemental, sediment distribution, and water quality parameters. The CAIS rapid survey systems provide an effective means of rapid geochemical and environmental characterization of the sediment/water interface over large regions, and in many different types of aquatic environments. Operable at water depths of up to 100 m, the CAIS rapid survey systems permit data collection in most nearshore areas (including lakes, rivers, estuaries), including a large portion of the continental shelf.
The various CAIS sensor systems may be used individually or as a comprehensive survey package. The CS3 system used in the Lake Pontchartrain survey is the component specifically designed for continuous sample collection as the vessel is underway (Culp et al., 1991; Noakes et al., 1985; Noakes and Harding, 1982). Other sensor components that may be added include the Gamma Isotope Mapping System (GIMS), which uses a NaI(Tl) gamma radiation detector for the identification of naturally occurring or man-made radioisotopes present in seafloor sediments (Noakes et al., 1991b; Noakes and Harding, 1974). The GIMS shipboard spectrometer records gamma radiation levels for selected radionuclides, yielding an isotopic signature that is indicative of the sediment lithology (Emery and Uchipi, 1972). A water quality data logging device may also be integrated with the CS3 sediment slurry flow, providing continuous measurements of bottom water parameters including temperature, dissolved oxygen, conductivity, salinity, and pH (Noakes et al., 1991c). Synoptically collected bathymetric and navigational data facilitate the real time or near real time generation of two- and three-dimensional profiles for many seafloor parameters when an immediate return of data is desired.
The components of the CS3 towed sled are configured in a cylindrical housing approximately 1.2 m in length and 28 cm in diameter (Figure 1). Umbilical connectors include a tow cable, a power cable, and sediment slurry transport hose. The sled is towed along the seafloor surface, perturbing the sediments in its path to a depth of approximately 4-6 cm and forming a plume from which sediments are sampled. The CS3 is designed specifically for preferential sampling the fine sediments that are the ultimate sink for most aquatic contaminants and the primary site of the sorption reactions which govern their fate and persistence.
|The CS3 submersible pump, made of Delrin® plastic, delivers a continuous stream of surface sediments to the survey vessel via a rubber transport hose. The sediment slurry passes unobstructed through a sample processor consisting entirely of plastic and rubber parts (Figure 2), first flowing through a centrifugal cone where the fine sediment fraction (<200 µm) is selectively separated for sample analysis. Samples are collected on demand at intervals determined by the requirements of the survey. At the recommended towing speed of three knots, a maximum collection of approximately three samples per km is possible. For sample collection, the continuously flowing fine fraction slurry is diverted to a collection chamber, where it is dewatered by vacuum filtration and deposited as a sediment wafer onto a quartz fiber wafer (Figure 3).|
Samples are keyed to time and location and air dried. Non-destructive elemental analyses for up to 8 selected major and trace elements can be performed simultaneously aboard ship using a wavelength-dispersive x-ray fluorescence spectrometer (XRF), or samples may be returned to the laboratory for a broader spectrum of analyses using an energy-dispersive XRF instrument.
Other CS3 shipboard components include a differential Global Positioning System (DGPS) navigational system, portable computer, fathometer, printer, and plotter (Figure 4). Custom software compiles information from the fathometer and DGPS system each time a CS3 sample is collected. Survey transects and bathymetry may be viewed in real time on a color monitor (Figure 5). The data, along with the results of XRF analyses, are used to generate two- and three-dimensional profiles of bathymetry and elemental concentrations (Figure 6, Water depth and bathymetric profile)
CS3 Survey Operations
A minimum crew of three persons is required for CS3 operations. The actual time required for collection of 757 samples during the Lake Pontchartrain survey encompassed a period of approximately 80 hours over the nine-day survey. Normally, the CS3 may be operated around the clock for an efficient and time-minimizing schedule, but working time during the Pontchartrain survey was restricted to daylight hours due to the fuel requirements of the research vessel, and to safety concerns associated with operations in the heavily trafficked lakefront area.
The CS3 sled can be deployed manually or using a hydraulic crane. The sled is towed at variable speeds between 3 and 8 knots along designated transects. At a speed of 3 knots, the sled descends to the bottom, perturbing surficial sediments and enabling the collection of a sample on demand at the appropriate sampling station. Between sample stations, the ship's speed is increased to approximately 8 knots so that the sled was towed well above the sediment surface in the water column. This towing method is efficient and safe, as it permits a rapid coverage of survey transects while ensuring minimum opportunity for entanglement at the sediment/water interface. The method also reduced the possibility for cross-contamination of samples due to the cleansing effect from continuous pumping of water through the system between collection stations.
Survey transects and CS3 sample collection stations are designated in
advance to ensure a nonbiased distribution of data for preparation of the resulting
elemental constituent maps (see Figure 7, Sampling
Stations). Sampling stations are located using DGPS. At each sample collection point, the
sample number, navigational coordinates, and time of collection are recorded in the survey
logbook and on computer diskette. The sediment wafer samples collected may be dried at
ambient temperature and stored in stainless steel containers for transport to the
analytical laboratory, or may be dried using hot air and analyzed immediately using a
shipboard XRF. The Lake Pontchartrain samples were returned to the CAIS laboratory where a
suite of 20 major and trace elements were analyzed using a Kevex 770 Analyst
energy-dispersive XRF unit. This XRF instrument employs a variety of excitation
conditions, secondary targets, and filters during each run to enhance analytical peaks.
Selected target analytes and detection limits for the XRF instrument are presented in
|Element||Reporting Unit||Detection Limit|
The CS3 sediment wafer samples are analyzed directly, without any treatment prior to analysis. Standard protocols for XRF analysis are observed, including detector calibrations for each batch of 15 samples using a reference disc of stainless steel, and a reference monitor to ensure that the specific conditions required for secondary target excitation for the XRF unit did not vary from batch to batch. The reference monitor consists of sediment filter wafer samples that have been made up from NIST reference material SRM2704. For interlaboratory calibration, repeat analyses were performed for certified reference materials MESS-1, BEST-1, PACS-1, and USGS standard MAG-1. For the Lake Pontchartrain survey, four separate samples from widely-spaced portions of the lakebed were split and analyzed in duplicate with the remainder of each split sent to the USGS for analysis.
Detection limits are quoted at 3s over background and were determined using NIST 2704 standard reference material.
The precision and accuracy determined by the replicate analyses on the 2704 NIST reference standard are presented in Appendix A. Also included in Appendix A are steps taken to normalize the data to achieve consistent concentration totals and results of an interlab sample comparison utilizing analytical methods other than the XRF methods used for this study. It was determined that the elemental concentration would be normalized to 90% total concentration to minimize sample variability. XRF data may not directly correlate with data compiled by other methods, but the results of the interlab sample comparison showed that the XRF data related the same relative patterns in elemental concentration. The sample locations, water depth, and elemental analyses from the 1996 sediment mapping survey are found below in Appendix B. More recent data, including sample stations, water depth, and elemental analyses, from a follow-up survey conducted in the summer of 1997 are found in Appendix C. The two- and three-dimensional maps generated by the 1997 data are displayed in the 1996-1997 comparison figures below.
Appendices B and C are tables available here in both Microsoft Excel and Corel Quattro Pro for viewing or downloading:
|Microsoft Excel versions||Corel Quattro Pro versions|
|1996 Lake Pontchartrain XRF Elemental Data||Appendix B||Appendix B|
|1997 Lake Pontchartrain XRF Elemental Data||Appendix C||Appendix C|
Figures for CS3
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Noakes, J.E. and J.L. Harding, 1976. Locating offshore minerals by natural radioactive measurements. Marine Technology Society Journal 8(5): 36-39.
Emery, K.O. and A. Uchipi, 1972. Western Atlantic Ocean. American Association of Petroleum Geologists Memoir No. 17.
Noakes, J.E., S.E. Noakes, R.A. Culp, 1991c. Comparison of data logger parameters aboard ship and towed on the seafloor. Proceedings of the 23rd Annual Offshore Technology Conference, Houston, Texas, May 6-9, 1991. OTC 6545: 411-416