Available data on the content of radioactive elements in recent marine sediments and sea water

10.3133/tem49 ◽  
1947 ◽  
Keyword(s):  
Marine Sediments ◽  
Sea Water ◽  
Radioactive Elements

scholarly journals Distribution of Radionuclides among Green Alga, Marine Sediments and Sea Water

1977 ◽  
Vol 18 (4) ◽  
pp. 322-330 ◽  
Author(s):  
R. NAKAMURA ◽  
Y. SUZUKI ◽  
T. UEDA
Keyword(s):  
Green Alga ◽  
Marine Sediments ◽  
Sea Water

The Yorkshire Dogger: III. Upper Eskdale

1943 ◽  
Vol 80 (6) ◽  
pp. 209-230 ◽  
Author(s):  
R. H. Rastall ◽  
J. E. Hemingway
Keyword(s):  
Shallow Water ◽  
Sea Level ◽  
Marine Sediments ◽  
Sea Water ◽  
Second Phase ◽  
Faunal Assemblage ◽  
Chemical Changes ◽  
Main Series ◽  
Uplift And Erosion ◽  
Shallow Water Sediments

1. A sequence of strata is determined in the Dogger of Upper Eskdale and its tributary valleys. The rocks fall into three main series, which are subdivided into groups.2. The underlying Yeovilian sediments, originally included with the Dogger, are mapped and briefly described. The unconformity between them and the Dogger is emphasized.3. The Dogger is marine throughout but only the oldest yields an adequate faunal assemblage, similar to that of the Glaisdale Oolite Series (upper opalinum). The greater part of the Dogger of this area is therefore younger than that of the Yorkshire Coast.4. Chemical changes in the sea-water caused the deposition of siderite to characterize the earliest phase (Glaisdale Oolite Series). This was succeeded by a phase of dominantly chamosite deposition (the Chamositic Series) followed by a reversion to siderite deposition (the Ajalon Series).5. Earth-movement controlled sedimentation over the area. During the first phase an eastern tilt to the region held the centre and west above or near sea-level, where it received no sediment. The second phase saw general depression with the accumulation of shallow water sediments. This was followed by uplift and erosion when a broad shallow valley was cut. Partial depression then flooded the valley with derived marine sediments.

Influence of major cations of sea water on the desorption of137Cs from marine sediments

1994 ◽  
Vol 187 (3) ◽  
pp. 197-205 ◽  
Author(s):  
D. V. M. Desai ◽  
Sathi S. Kumar ◽  
K. C. Pillai
Keyword(s):  
Marine Sediments ◽  
Sea Water ◽  
Major Cations

Chromatographic Analysis of Hydrocarbons in Marine Sediments and Sea water

1975 ◽  
Vol 13 (11) ◽  
pp. 535-540 ◽  
Author(s):  
W. E. May ◽  
S. N. Chesler ◽  
S. P. Cram ◽  
B. H. Gump ◽  
H. S. Hertz ◽  
...  
Keyword(s):  
Marine Sediments ◽  
Chromatographic Analysis ◽  
Sea Water

The occurrence of thallium in sea water and marine sediments

1970 ◽  
Vol 6 ◽  
pp. 149-152 ◽  
Author(s):  
A.D. Matthews ◽  
J.P. Riley
Keyword(s):  
Marine Sediments ◽  
Sea Water

scholarly journals Oil Spill Biodegradation by Bacteria Isolated from Jakarta Bay Marine Sediments

2016 ◽  
Vol 21 (1) ◽  
pp. 29
Author(s):  
Angga Dwinovantyo ◽  
Tri Prartono ◽  
Restya Rahmaniar ◽  
Nico Wantona Prabowo ◽  
Santi Susanti
Keyword(s):  
Oil Spill ◽  
Marine Sediments ◽  
Sea Water ◽  
Carbon Number ◽  
Carbon Chain ◽  
Plate Count ◽  
Water Medium ◽  
Biodegradation Process ◽  
Constant Of Biodegradation ◽  
Number Of Bacteria

A laboratory study was conducted with the aim to isolate and identify bacteria from sea sediment and test their biodegradation ability in two place where contaminated with oil spill. Five sediment samples were dissolved by using sterile sea water, and then bacteria isolated with total plate count (TPC) method. Isolates bacteria was cultivated, and adapted using the nutrient conditioned sea water medium. Biodegradation process was done by mixing the bacteria with crude oil and shaken for few days. The number of bacteria isolated varied from 2 x 102 CFU ml-1 to 6 x 106 CFU ml-1 and apparently increased after cultivation and adaptation with oily media. Bacteria identified during this study were Fundibacter sp., Alcanivorax sp., and Marinobacter sp.. The result of biodegradation process was statistically analyzed and obtained that the bacteria are effective in degrading oil in seven days with constant of biodegradation rate was 0.1766. GC-MS analysis was conducted to prove the decomposition of carbon chain by bacteria and revealed oil degradation in carbon number 11 to 27. Based on all analysis, marine sediment bacteria can degrade the oil spill. Keywords : Bacteria, Biodegradation, GC-MS, Marine Sediments, Oil spill.

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