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Trace metals in phytoplankton from an area of coastal upwellingPequegnat, John Eugene 18 September 1974 (has links)
Short-term changes in the distribution, surface to 10 meters, of
phytoplankton-associated trace metals (Fe, Mn, Cr, Zn, Co, Ni, and
Cu) were studied in the near-shore waters off Humboldt Bay,
California, through the summer of 1971. The depth distribution of
phytoplankton-associated trace metals was related to local hydrography.
During periods of upwelling higher concentrations of
phytoplankton-associated Fe, Mn, Cr, and Zn were found at depth
(10 meters) than at the surface. During periods of non-upwelling
there was less stratification in their distribution. Phytoplankton-associated
Cu, Go, and Ni showed no significant increase with depth
during either period. The rate of change in trace metal distribution
patterns of Fe, Mn, Cr, and Zn were regulated by surface wind patterns
and hydrographic regimes. Again, Cu, Co, and Ni did not
fluctuate in a significant fashion.
The elements studied tended to fall into three ordered groups
based on their behavior with respect to 1) depth distribution,
2) correlation with other metals studied, and 3) correlation with biomass
indicators. The groupings were Fe, Mn, and Cr; Zn, Co, and
Ni; and finally Cu. This ordering is similar to the Irving- Williams
series and to the elements relative 'hardness" as a Lewis acid where
Fe(III), Cr(III), and Mn(II) are considered hard Lewis acids while
Zn(II), Co(II), Ni(II) and finally Cu(II) are considered borderline hard
to soft Lewis acids. These properties are related to the relative
affinities and selectivities of the elements for organic ligands. There
also appears to be some relation between the physical (dissolved
versus particulate form) and the chemical (oxidation state and ionic
potential) behavior of the elements in sea water and their behavior in
the phytoplankton.
There was a negative correlation between most phytoplankton-associated
trace metal concentrations (Fe, Mn, Cr, Zn, Co, and Ni)
and biomass during non-upwelling periods and a positive correlation
during upwelling periods. Copper, on the other hand, showed a positive
correlation during both periods. This aberrant behavior of copper
may be related to its high affinity for organic ligands and its relative
softness as a Lewis acid. Since no simple negative correlation was
found between phytoplankton biomass and phytoplankton-associated
trace metal concentrations, biological dilution does not appear to be as
important as the hydrographic regime and the chemical activities of
the element in determining the concentrations of trace metals in
near shore phytoplankton populations. / Graduation date: 1975
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Trace element chemistry of aging marine detritus derived from coastal macrophytesRice, Donald Lester 05 1900 (has links)
No description available.
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Trace element speciation in fresh waters (1) Technique development for determining zinc-organic ligand complexation (2) Arsenic speciation and redox cycling in a seasonally anoxic lake /Anderson, Linda Close Davis. January 1900 (has links)
Thesis (Ph. D.)--University of California, Santa Cruz, 1989. / Typescript. Includes bibliographical references.
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Supported liquid membranes with macrocyclic carriers mimicking the metal uptake mechanisms of microorganisms for determination of metal speciation /Wallace, Sean Maurice. January 1996 (has links)
Thesis (M.S.)--University of California, Santa Cruz, 1996. / Typescript. Includes bibliographical references.
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Determination of zinc in environmental samples by stripping voltammetry method.January 1996 (has links)
by Oi-Ming Cheng. / Thesis (M.Phil.)--Chinese University of Hong Kong, 1996. / Includes bibliographical references (leaves 104-108). / Chapter 1 --- INTRODUCTION / Chapter A) --- Sources of zinc and its functional role --- p.10 / Chapter B) --- Effects of excessive zinc intake --- p.11 / Chapter (a) --- Human --- p.11 / Chapter (b) --- Animal --- p.11 / Chapter (c) --- Fish --- p.12 / Chapter C) --- Techniques in zinc determination --- p.12 / Chapter 2 --- ANODIC STRIPPING VOLTAMMETRY / Chapter A) --- Basic principles --- p.16 / Chapter (a) --- Cell --- p.16 / Chapter (b) --- Electrodeposition and stripping --- p.20 / Chapter B) --- Major interferences in anodic stripping and the common solutions to these problems --- p.25 / Chapter (a) --- Intermetallic compound formation --- p.25 / Chapter (b) --- Overlapping peaks --- p.26 / Chapter (c) --- Organic compounds adsorbed at the electrode --- p.28 / Chapter 3 --- MUTUAL INTERFERENCE FROM ZINC AND COPPER / Chapter A) --- Introduction --- p.30 / Chapter B) --- Review of reported methods to remove copper interference --- p.31 / Chapter (a) --- Dual-working electrode approach --- p.31 / Chapter (b) --- Adjustment of the deposition potential --- p.31 / Chapter (c) --- Standard addition --- p.33 / Chapter (d) --- Addition of a third element --- p.33 / Chapter C) --- The proposed solution --- p.35 / Chapter 4 --- EXPERIMENTAL / Chapter A) --- Proposed method --- p.37 / Chapter (a) --- Apparatus --- p.37 / Chapter (b) --- Reagents --- p.38 / Chapter (c) --- Procedure --- p.40 / Chapter B) --- Reference method --- p.45 / Chapter (a) --- Apparatus --- p.45 / Chapter (b) --- Reagents --- p.45 / Chapter (c) --- Procedure --- p.47 / Chapter 5 --- RESULTS AND DISCUSSION / Chapter A) --- Optimization of instrumental parameters and working conditions --- p.49 / Chapter (a) --- Effect of plating potential on zinc peak current --- p.49 / Chapter (b) --- Effect of plating time on zinc peak current --- p.53 / Chapter (c) --- Effect of holding time and holding potential on zinc peak current --- p.56 / Chapter (d) --- Effect of sweep rate on zinc peak current --- p.58 / Chapter (e) --- Effect of final potential and strip time on zinc peak current --- p.61 / Chapter (f) --- Effect of pH on the peak current and recovery of zinc in the presence of copper after the sulphide treatment --- p.63 / Chapter (g) --- Effect of the concentration of buffer on the peak current --- p.66 / Chapter (h) --- Effect of the reaction time of sulphide with copper on the zinc recovery --- p.68 / Chapter B) --- "Calibration graph, precision and detection limit" --- p.71 / Chapter C) --- Effect of copper on the zinc determination by the proposed method --- p.78 / Chapter D) --- Interference studies --- p.80 / Chapter E) --- Recovery tests --- p.84 / Chapter F) --- Determination of zinc in real samples using the proposed method --- p.86 / Chapter (a) --- Clean water samples such as sea water and tap water --- p.86 / Chapter (b) --- Contaminated natural water and domestic wastewater samples --- p.91 / Chapter (c) --- Air samples --- p.93 / Chapter (d) --- Oyster tissue samples --- p.96 / Chapter (e) --- Sewage sludge and sediment samples --- p.99 / Chapter 6 --- CONCLUSION --- p.102 / REFERENCES --- p.104
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Trace metal cycling in the central equatorial Pacific : results from the U.S. JGOFS EqPac survey cruises /Chapin, Thomas P., January 1997 (has links)
Thesis (Ph. D.)--University of Washington, 1997. / Vita. Includes bibliographical references (p. [200]-229).
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Trace metal cycling in the central equatorial Pacific results from the U.S. JGOFS EqPac survey cruises /Chapin, Thomas P., January 1997 (has links)
Thesis (Ph. D.)--University of Washington, 1997. / Includes bibliographical references (leaves [200]-229).
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Chromium in San Francisco Bay inorganic speciation, distribution, and geochemical processes /Abu-Saba, Khalil Elias. January 1994 (has links)
Thesis (M.S.)--University of California, Santa Cruz, 1994. / Typescript. Includes bibliographical references (leaves 159-166).
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Characterization of trace iron species in natural waterJohnson, James Robert 01 January 1977 (has links)
The distribution and speciation of trace metals in natural waters is only slightly, at best, understood. Interactions with organic substances can effectively distribute the metals throughout many ill-defined physical and chemical. To better comprehend the complexity of metal-organic interactions this work focused on the delineation of trace iron species present in a natural system. The separation of Fe(II) and Fe(III) was successfully accomplished using a variation of an ion exchange method involving resin-loaded filter paper. The quantitation of the various iron species was determined using linear scan voltammetry and atomic absorption. The total iron concentration, determined as the sum of the various separate species, compares favorably with the total iron concentration as determined directly using atomic absorption methods.
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Assessment of trace element contamination in streambed sediment and spatial associations in Palolo Valley watershed, Honolulu, Oʻahu, HawaiʻiHotton, Veronica K. January 2005 (has links)
Thesis (M.A.)--University of Hawaii at Manoa, 2005. / Includes bibliographical references (leaves 146-156).
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