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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Oceanography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (634 pages)
    Edition: 3rd ed.
    ISBN: 9783527613991
    DDC: 551.4601
    Language: English
    Note: Intro -- Methods of Seawater Analysis -- Contents -- List of contributors -- 1 Sampling -- 1.1 Introduction -- 1.2 Sampling strategy -- 1.3 Sampling techniques -- 1.3.1 Surface water sampling -- 1.3.2 Water samplers for major hydrochemical variables -- 1.3.3 Water samplers for trace constituents -- 1.3.3.1 Trace elements -- 1.3.3.2 Trace organic compounds -- 1.3.4 Specific samplers -- 1.3.5 Collection of marine particles -- 1.3.5.1 Collection of suspended particulate matter (SPM) -- 1.3.5.2 Collection of sinking particulates -- 1.4 Sampling errors -- 1.5 Quality control -- 1.5.1 Precision -- 1.5.2 Accuracy -- 1.5.3 Limit of detection -- References to Chapter 1 -- 2 Filtration and storage -- 2.1 Filtration -- 2.1.1 General remarks -- 2.1.2 Filters -- 2.1.3 Filtration techniques -- 2.1.3.1 Vacuum filtration -- 2.1.3.2 Pressure filtration -- 2.1.3.3 In situ filtration -- 2.1.3.4 Centrifugation -- 2.2 Storage -- 2.2.1 General remarks -- 2.2.2 Storage for the determination of major compounds -- 2.2.3 Storage for the determination of nutrients -- 2.2.3.1 General remarks -- 2.2.3.2 Refrigeration -- 2.2.3.3 Poisoning -- 2.2.4 Storage for the determination of trace elements -- References to Chapter 2 -- 3 Determination of salinity -- 3.1 Introduction -- 3.2 Symbols and abbreviations -- 3.3 Definition of salinity -- 3.3.1 Early concepts -- 3.3.2 The practical salinity scale of 1978 (PSS78) -- 3.4 Measurement of the conductivity ratio -- 3.5 Salinity from bench salinometers -- 3.5.1 Purpose -- 3.5.2 Standard seawater -- 3.5.3 Sampling -- 3.5.4 The Guildline AUTOSAL Model 8400 B -- 3.5.5 The Beckman Model RS1O -- 3.5.6 Data logging -- 3.5.7 Substandards -- 3.6 Salinity from in situ measurements: CTD profilers -- 3.6.1 Principles -- 3.6.2 Operation of CTD-rosette sampler systems -- 3.6.3 Calibration -- 3.6.4 Data processing -- References to Chapter 3. , 4 Determination of oxygen -- 4.1 Introduction -- 4.2 Principle of the determination -- 4.3 Error sources and interferences -- 4.4 Reagents -- 4.5 Instruments -- 4.6 Procedure -- 4.6.1 Standardization of the thiosulphate solution -- 4.6.2 Subsampling and fixation of dissolved oxygen -- 4.6.3 Storage -- 4.6.4 Titration -- 4.6.5 Determination of the reagent blank -- 4.6.6 Calculation of the result -- 4.6.7 Accuracy and precision -- References to Chapter 4 -- 5 Determination of hydrogen sulphide -- 5.1 Introduction -- 5.2 Units -- 5.3 Analytical methods -- 5.3.1 Method by Fonselius -- 5.3.1.1 Reagents -- 5.3.1.2 Special apparatus -- 5.3.1.3 Sampling -- 5.3.1.4 Preservation of samples -- 5.3.1.5 Procedure -- 5.3.1.6 Analysis -- 5.3.1.7 Dilution of samples -- 5.3.1.8 Standardization of the method -- 5.3.1.9 Calibration of the method -- 5.3.2 Method by Cline -- 5.3.2.1 Reagents -- 5.3.2.2 Special apparatus -- 5.3.2.3 Sampling -- 5.3.2.4 Procedure -- 5.3.2.5 Analysis -- 5.3.2.6 Standardization and calibration of the method -- 5.3.3 Titration methods -- 5.3.4 Methods using mercury compounds -- References to Chapter 5 -- 6 Determination of thiosulphate and sulphur -- 6.1 Introduction -- 6.2 Principle of the determination of thiosulphate -- 6.2.1 Apparatus -- 6.2.2 Reagents -- 6.2.3 Sampling and storage -- 6.2.4 Procedure -- 6.2.4.1 Standardization of the thiosulphate solution -- 6.2.4.2 Titration of the sample -- 6.2.5 Calculation of the thiosulphate content of the sample -- 6.2.6 Interferences -- 6.3 Principle of the determination of sulphur -- 6.3.1 Apparatus -- 6.3.2 Reagents -- 6.3.3 Sampling and storage -- 6.3.4 Procedure -- 6.3.5 Calculations -- 6.3.6 Interferences -- 6.4 Other methods -- References to Chapter 6 -- 7 Determination of pH -- 7.1 Introduction -- 7.2 List of symbols -- 7.3 Definition of pH -- 7.4 pH scales in seawater. , 7.5 Measurement of pH -- 7.5.1 Potentiometry -- 7.5.1.1 Theory -- 7.5.1.2 Tris buffers -- 7.5.1.3 Practical considerations -- 7.5.2 Spectrophotometry -- 7.5.2.1 Theory -- 7.5.2.2 Indicator pK values for seawater -- 7.5.2.3 Measurement procedures -- 7.5.3 Comparison of the various techniques -- 7.5.4 Correction of pH to in situ conditions -- 7.5.4.1 Empirical equations for correction to in situ temperature -- 7.5.4.2 Empirical equations for correction to in situ pressure -- References to Chapter 7 -- 8 Determination of total alkalinity and total dissolved inorganic carbon -- 8.1 Introduction -- 8.2 List of symbols -- 8.3 Sampling and reference materials -- 8.3.1 Sampling -- 8.3.2 Standard reference materials -- 8.4 Total alkalinity -- 8.4.1 Definition -- 8.4.2 Potentiometric titrations -- 8.4.2.1 Instrumentation -- 8.4.2.2 Analytical procedure -- 8.4.2.3 Evaluation procedures -- 8.4.3 Back titration method -- 8.4.3.1 Reagents -- 8.4.3.2 Analytical procedure -- 8.4.3.3 Calculation of results -- 8.4.3.4 Precision and accuracy -- 8.5 Total dissolved inorganic carbon -- 8.5.1 Potentiometric titrations -- 8.5.2 Coulometric determination technique -- 8.5.2.1 Instrumentation -- 8.5.2.2 Analytical procedure -- 8.5.2.3 Calculation and expression of results -- 8.6 Thermodynamic calculations of the C02 system in seawater -- 8.6.1 Equations describing the C02 system in seawater -- 8.6.2 Selection of stability constants -- 8.6.3 Calculations with two measured C02 parameters -- 8.6.3.1 Calculations with pH and AT measured -- 8.6.3.2 Calculations with pH and f(C02) measured -- 8.6.3.3 Calculations with pH and CT measured -- 8.6.3.4 Calculations with AT and CT measured -- 8.6.3.5 Calculations with AT and f(C02) measured -- 8.6.3.6 Calculations with CT and f(C02) measured -- 8.6.4 Errors arising from the calculations -- References to Chapter 8 -- Appendix 8A. , 9 Determination of carbon dioxide partial pressure (p(CO2)) -- 9.1 Introduction -- 9.2 Principle of the measurement -- 9.3 Apparatus for continuous mode of operation -- 9.3.1 The equilibrator -- 9.3.2 The analytical system -- 9.4 Reagents -- 9.4.1 Calibration gases -- 9.4.2 Gas purification reagents -- 9.5 Calculation of results -- 9.6 Accuracy -- References to Chapter 9 -- 10 Determination of nutrients -- 10.1 Introduction -- 10.1.1 Oceanic distributions of nutrients -- 10.1.2 Chemistry of nutrients in the marine environment -- 10.2 Analytical methods -- 10.2.1 Pretreatment of samples -- 10.2.2 The matrix -- 10.2.3 References and standard materials -- 10.2.4 Calibration, blank determination and calculation procedures -- 10.2.5 Determination of dissolved inorganic phosphate -- 10.2.5.1 Principle of the method -- 10.2.5.2 Range and precision -- 10.2.5.3 Interferences -- 10.2.5.4 Reagents -- 10.2.5.5 Analytical procedures -- 10.2.6 Determination of dissolved inorganic phosphate in the presence of arsenic -- 10.2.6.1 Principle of the method -- 10.2.6.2 Reagents -- 10.2.6.3 Analytical procedures -- 10.2.7 Determination of dissolved inorganic phosphate by an extraction procedure (high-sensitivity method) -- 10.2.7.1 Principle of the method -- 10.2.7.2 Range and precision -- 10.2.7.3 Interferences -- 10.2.7.4 Reagents -- 10.2.7.5 Analytical procedure -- 10.2.8 Determination of nitrite -- 10.2.8.1 Principle of the method -- 10.2.8.2 Range and precision -- 10.2.8.3 Interferences -- 10.2.8.4 Reagents -- 10.2.8.5 Analytical procedures -- 10.2.9 Determination of nitrate -- 10.2.9.1 Principle of the method -- 10.2.9.2 Range and precision -- 10.2.9.3 Interferences -- 10.2.9.4 Reagents -- 10.2.9.5 Preparation of the reductor -- 10.2.9.6 Analytical procedures -- 10.2.10 Determination of ammonia -- 10.2.10.1 Principle of the method -- 10.2.10.2 Range and precision. , 10.2.10.3 Interferences -- 10.2.10.4 Reagents -- 10.2.10.5 Analytical procedures -- 10.2.1 1 Determination of dissolved inorganic silicate -- 10.2.11.1 Principle of the method -- 10.2.11.2 Range and precision -- 10.2.11.3 Interferences -- 10.2.11.4 Reagents -- 10.2.11.5 Analytical procedures -- 10.2.12 Determination of nitrogen, phosphorus and silicon in particulate and dissolved organic matter -- 10.2.12.1 Equipment -- 10.2.12.2 Calibration and calculation of total and organic nutrients -- 10.2.13 Determination of total and organic phosphorus by acid persulphate oxidation -- 10.2.13.1 Reagents -- 10.2.13.2 Analytical procedure -- 10.2.14 Determination of total and organic phosphorus by alkaline persulphate oxidation -- 10.2.14.1 Reagents -- 10.2.14.2 Analytical procedure -- 10.2.14.3 Dilution factors (see Section 10.2.12.2) -- 10.2.15 Determination of polyphosphates -- 10.2.15.1 Analytical procedure -- 10.2.16 Determination of total and organic nitrogen after persulphate oxidation -- 10.2.16.1 Range and precision of the method -- 10.2.16.2 Reagents -- 10.2.16.3 Analytical procedure -- 10.2.17 Simultaneous oxidation of nitrogen and phosphorus compounds with persulphate -- 10.2.17.1 Range and precision of the method -- 10.2.17.2 Oxidizing reagent -- 10.2.17.3 Analytical procedure -- 10.2.18 Determination of total silicon -- 10.2.18.1 Principle of the method -- 10.2.18.2 Reagents -- 10.2.18.3 Analytical procedure -- 10.2.19 Determination of total silicon by carbonate fusion -- 10.2.19.1 Reagents -- 10.2.19.2 Analytical procedure -- 10.3 Automated nutrient analysis -- 10.3.1 Principle of automated analysis -- 10.3.2 The sampler -- 10.3.3 The proportioning pump -- 10.3.4 The analytical manifold -- 10.3.4.1 Standard manifold components -- 10.3.4.2 Heating and cooling -- 10.3.4.3 Special devices -- 10.3.4.4 The flow-through spectrophotometer. , 10.3.5 Data acquisition.
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  • 2
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    Elsevier
    In:  Deep Sea Research Part I: Oceanographic Research Papers, 40 (2). pp. 257-266.
    Publication Date: 2018-03-21
    Description: A method for the collection of large-volume samples of oceanic particles is described. Near-surface seawater is pumped from below the ship to a continuous-flow centrifuge at rates of up to 1.2 m3 h−1. The seawater is in contact with polyethylene, polypropylene, Teflon and titanium materials only. The retention efficiency of the centrifuge for marine particles is the same as for standard membrane filters, as shown by comparisons with separate samples from Go-Flo bottles. The pumping system is non-contaminating with respect to both particulate and dissolved species. Several subsampling facilities for additional chemical constituents and other parameters can be supplied simultaneously due to the modular design of the system and the high flow rates
    Type: Article , PeerReviewed
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  • 3
    Publication Date: 2018-03-07
    Description: In February 1988, 60 near surface samples were taken on a track between 2°W in the English Channel, the Pentland Firth and the inner German Bight. Determinations were made on filtered and unfiltered samples. Concentrations of dissolved metals in the North Sea normalized to a salinity of 34.5 were Al 31, Cd 0.13, Co 0.13, Cu 3.4, Mn 6.2 and Ni 3.9 nM. In July 1984 the equivalent concentrations were Al 11, Cd 0.15, Co 0.15, Cu 4.3, Mn 12 and Ni 3.6 nM. Distinct regional differences were detectable which can be related to the origin of the water, differing river inputs, and solution-solid phase exchange reactions. The degree of the influence of exchange reactions was investigated through the concept of Kd, the distribution coefficient. A Kd of 105 ml g−1 for Al is consistent with other observations and explains the relatively high concentrations of dissolved Al detected in the English Channel on this cruise. The data suggest a higher Kd for Mn approaching 106 ml g−1. The high Mn Kd coupled to higher suspended sediment loads in winter may be sufficient to explain the lower concentration of dissolved Mn in winter. Comparison of concentrations across the shelf break suggests that for all the metals studied, the European Shelf is a source of dissolved metals to the deep sea. Calculations based on the limited available data indicate that this export is of similar magnitude to the fresh water input of dissolved metals.
    Type: Article , PeerReviewed
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  • 4
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    Elsevier
    In:  Deep Sea Research Part I: Oceanographic Research Papers, 40 (6). pp. 1155-1168.
    Publication Date: 2018-03-05
    Description: Particulate fluxes of aluminium, cadmium, cobalt, copper, iron, manganese, nickel, phosphorus, lead, vanadium and zinc in the northeast subtropical Atlantic Ocean have been determined from sediment trap samples collected between 1 December 1986 and 30 April 1987 at 1020 and 4120 m below the ocean surface. The fluxes of most elements (except Cd and P) show small variations between the different layers, and are closely associated with the vertical transport of aluminium. Elemental composition and flux rates suggest that aerosol loadings from northeast trade winds are the major contributor of these elements to depositing material. Extremely low fluxes of copper, lead and zinc also indicate that anthropogenic perturbations are of insignificant importance in this region.
    Type: Article , PeerReviewed
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  • 5
    Publication Date: 2018-03-15
    Description: CO2 partial pressure in surface water was measured in the Northeast Atlantic and in the Hebride Shelf/North Sea area during a cruise with R.V. Poseidon in June 1991. A mean pCO2 of 303 μatm was found in the Atlantic between 50°N and 60°N. For an atmospheric CO2 content of 357.5 ppm(v) this corresponds to a partial pressure difference of −55 μatm. This supports the view that the subarctic Atlantic is a significant sink within the CO2 cycle between the ocean and the atmosphere. A comparison of our measurements with other data reveals that the pCO2 distribution changes significantly during May/June. This explained by seasonal warming, CO2 exchange with the atmosphere and biomass production. The contribution by each of these processes to the seasonal variations is calculated. It was found that during a plankton bloom the production of biomass is the dominating factor and may lower seawater pCO2 by almost 100 μatm. The shelf areas are charactrized by strong pCO2 gradients which are explained by water exchange with the Atlantic, temperature effects and biomass production.
    Type: Article , PeerReviewed
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  • 6
    Publication Date: 2017-10-05
    Description: Water samples from surface and bottom waters of two bights of the Baltic Sea were analysed for dissolved and/or particulate concentrations of Al, Cd, Co, Cu, Fe, Hg, Mn, Ni, Pb and Zn, in addition to the main oceanographic variables, at 27 stations during six cruises between February 1990 and July 1992. The metal values show distinct regional differences, with maximum concentrations at the near-shore stations, The levels of total Hg exhibit a significant negative relationship with salinity. In surface layers, seasonal differences due to biogenic uptake of elements could not be detected for any of the dissolved metals. In bottom waters, however, summer-time concentrations of a number of metals are in clear excess of winter levels either due to diffusion of metals (Go, Fe, Mn) from the sediments under low-oxygen or anaerobic conditions, or due to mineralization processes (Cd, Zn) of recently sedimented biogenic particulates. With the exception of Fe and Pb, the particulate fractions are of minor importance, with slight variabilities between the seasons only. The K-D values (ratio between metal concentrations in the particulate and dissolved fractions) decrease by more than two orders of magnitude in the order Fe-Pb-Mn-Co-Zn-Cd-Cu-Ni. Finally, the results are discussed with regard to a trace metal monitoring programme in the area.
    Type: Article , PeerReviewed
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  • 7
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    Elsevier
    In:  Deep Sea Research Part I: Oceanographic Research Papers, 48 (12). pp. 2541-2567.
    Publication Date: 2020-08-05
    Description: In September 1993 (M26) and June/July 1996 (M36), a total of 239 surface samples (7 m depth) were collected on two transects across the open Atlantic Ocean (224 samples) and northwest European shelf edge area. We present an overview of the horizontal variability of dissolved Cd, Co, Zn, and Pb in between the northwest and northeast Atlantic Ocean in relation to salinity and the nutrients. Our data show a preferential incorporation of Cd relative to P in the particulate material of the surface ocean when related to previously published parallel measurements on suspended particulate matter from the same cruise. There is a good agreement with results recently estimated from a model by Elderfield and Rickaby (Nature 405 (2000) 305), who predict for the North Atlantic Ocean a best fit for αCd/P=[Cd/P]POM/[Cd/P]SW of 2.5, whereas the approach of our transect shows a αCd/P value of 2.6. The Co concentrations of our transects varied from 〈5 to 131 pmol kg−1, with the lowest values in the subtropical gyre. There were pronounced elevations in the low-salinity ranges of the northwest Atlantic and towards the European shelf. The Co data are decoupled from the Mn distribution and support the hypothesis of marginal inputs as the dominant source. Zinc varied from a minimum of 〈0.07 nmol kg−1 to a maximum of 1.2 and 4.8 nmol kg−1 in regions influenced by Labrador shelf or European coastal waters, respectively. In subtropical and northeast Atlantic waters, the average Zn concentration was 0.16 nmol kg−1. Zinc concentrations at nearly three quarters of the stations between 40°N and 60°N were 〈0.1 nmol kg−1. This suggests that biological factors control Zn concentrations in large areas of the North Atlantic surface waters. The Pb data indicated that significant differences in concentration between the northwest and northeast Atlantic surface waters presently (1996) do not exist for this metal. The transects in 1993 and 1996 exhibited Pb concentrations in the northeast Atlantic surface waters of 30 to 40 pmol kg−1, about a fifth to a quarter of the concentrations observed in 1981. This decline is supported by our particle flux measurements in deep waters of the same region.
    Type: Article , PeerReviewed
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