Dispersed Sedimentary Matter of the Atmosphere

Author(s):  
Vladimir P. Shevchenko ◽  
Alexander P. Lisitsyn ◽  
Anna A. Vinogradova ◽  
Dina P. Starodymova ◽  
Vladimir B. Korobov ◽  
...  
Keyword(s):  

2014 ◽  
Vol 456 (2) ◽  
pp. 709-713 ◽  
Author(s):  
A. P. Lisitsyn ◽  
V. N. Lukashin ◽  
A. N. Novigatskii ◽  
A. K. Ambrosimov ◽  
A. A. Klyuvitkin ◽  
...  


2018 ◽  
Vol 480 (1) ◽  
pp. 689-693 ◽  
Author(s):  
L. L. Demina ◽  
D. F. Budko ◽  
A. P. Lisitzin ◽  
A. N. Novigatsky


1862 ◽  
Vol 4 ◽  
pp. 582-583
Author(s):  
Archibald Geikie

After referring to a previous communication to the Society, in which the author had given an outline of the chronology of the igneous rocks of Scotland, he proceeded in the present paper to describe in detail the character of the volcanic phenomena in one district—that of the carboniferous system of the Forth basin. The igneous rocks of this district consist partly of doleritic and felspathic lava-form masses, and partly of various kinds of ash or traptuff. These materials present a considerable diversity in their modes of arrangement. But the author had found that all the volcanic hills of the district might be reduced to three types of structure:—1. A simple cone of ash, round and over which the ordinary sedimentary accumulation of the carboniferous period had been deposited. 2. A cone of ash with the crater filled up by a neck or plug of basalt. 3. Sheets of different lavas with intercalated ash or sedimentary matter.



2015 ◽  
Vol 464 (1) ◽  
pp. 956-962 ◽  
Author(s):  
A. P. Lisitzin ◽  
V. N. Lukashin


2011 ◽  
Vol 1 (6) ◽  
pp. 22
Author(s):  
Madhav Manohar

The movement of sedimentary matter along the coastal regions of the land has always been a problem in coastal and harbour engineering. Erosion and accretion of the shore and the sea bottom and the silt charge from the rivers discharging into the sea contribute the necessary sediment that moves along the coast.



2018 ◽  
Vol 479 (1) ◽  
pp. 384-389
Author(s):  
A. N. Novigatsky ◽  
A. P. Lisitzin ◽  
A. A. Klyuvitkin ◽  
V. P. Shevchenko ◽  
M. D. Kravchishina ◽  
...  


Author(s):  
В. Денисов ◽  
V. Denisov ◽  
Ю. Ткаченко ◽  
Yu. Tkachenko

Using sediment traps (ST) in marine research expeditions from 1986 to 2010, 188 samples of suspended matter were analyzed. All the samples were received from the shallow-water area (2 to 50 meters depth) of the Black sea shelf. Sedimentary matter from the catch basins was singled out by means of direct, high vacuum, membranous ultrafiltration with nuclear filters having 0,45 μm diameter pinholes produced by the United Institute of Nuclear Investigations in Dubna (UINI). The suspended matter received was dried till weight stabilizing, scaled and underwent analytical research. The material composition of the sedimentary matter is represented by the clayed-carbonated-micaceous matter. Biogenous minerals are represented by three carbon types: tiff, aragonite and siderite. The amount of the chiselly biogenous minerals has a subordinate meaning and serves as adulteration in suspended matter. The amount of ore minerals in the suspended matter compositionreaches 2–3 % (ferric oxide – 1 %, ferric hydroxide – up to 2 %, etc.). Geochemical composition of the suspended matter is tightly related to the bioproduction and biofiltration, impact of river flow, shallow-water sediment detachment and inflow of aerosolized matter. The industrial factor plays an important part in formation of modern chemical suspended matter composition.



2021 ◽  
pp. 278-286
Author(s):  
A.N. Novigatsky ◽  
◽  
A.P. Lisitzin ◽  
V.P. Shevchenko ◽  
A.A. Klyuvitkin ◽  
...  

The monthly, seasonal and annual quantity estimates of vertical fluxes of sedimentary matter from the surface layer of the Arctic Ocean, performed out over the years by various researchers, are the basis for direct calculations of incoming chemical components, minerals, and various pollutants to the surface layer of bottom sediments.



2017 ◽  
Vol 472 (2) ◽  
pp. 252-255 ◽  
Author(s):  
A. P. Lisitzin ◽  
A. N. Novigatsky ◽  
V. P. Shevchenko ◽  
A. A. Klyuvitkin ◽  
M. D. Kravchishina ◽  
...  


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