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source sediments - vertaling naar russisch

SEDIMENT FROM MARINE WATERS
Marine sediments; Marine Sediment; Ocean sediment; Ocean sediments; Seafloor sediment; Seafloor sediments; Seabed sediment; Deep sea sediment; Coastal sediments; Coastal sediment
  • url = https://archimer.ifremer.fr/doc/2008/publication-3900.pdf}}</ref>}} In this diagram the youngest parts of the ocean crust are coloured red. These young parts are found either side of the [[mid-ocean ridge]]. New crust emerges and spreads out from this ridge, which traverses central parts of the ocean.
  • Benthic diatom}}
  •  [[Bioturbation]] and bioirrigation in the sediment at the bottom of a coastal ecosystems
  •  [[Black smoker]] hydrothermal vent. The "smoke" consists of dissolved particles that precipitate into solids when exposed to colder water
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  •  Calcareous sediment can only accumulate in depths shallower than the calcium carbonate compensation depth (CCD). Below the CCD, calcareous sediments dissolve and will not accumulate. The lysocline represents the depths where the rate of dissolution increases dramatically.
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  • colonization by plants]], which – through their effects on erosion and sedimentation – brought about significant climatic change.
  • <small>The red–orange–yellow fractions of organic matter have a different lability</small>}}
  •  Hydrothermal vents occur mostly along the [[mid-ocean ridge]]s
  • see below ↓]]</small>}}
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  • Geologic time represented by a geological clock, showing the relative lengths<br />of the eons of Earth's history and noting major events}}
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  • Thickness of marine sediments}} The sediments sit on top of the ocean crust, and are thick (green and yellow) along the continental shelves and down the continental slopes. They are at their thinnest (dark blue) near and along the mid-ocean ridge.
  • 10.1594/PANGAEA.115344}}</ref>
  • The drainage basins of the principal oceans and seas of the world are marked by [[continental divide]]s. The grey areas are [[endorheic basin]]s that do not drain to the ocean.
  • 50px]] Modified text was copied from this source, which is available under a [https://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International License].</ref>}} (1) Organic matter settling from the water column is deposited at seafloor (donor control; fixed flux upper boundary condition).<br />(2) Sediments in the photic zone are inhabited by benthic microalgae that produce new organic matter in situ and grazing animals can impact the growth of these primary producers.<br />(3) Bioturbating animals transfer labile carbon from the sediment surface layer to deeper layers in the sediments. (Vertical axis is depth; horizontal axis is concentration)<br />(4) Suspension-feeding organisms enhance the transfer of suspended particulate matter from the water column to the sediments (biodeposition).<br />(5) Sponge consume dissolved organic carbon and produce cellular debris that can be consumed by benthic organisms (i.e., the [[sponge loop]]).<ref name=Middelburg2018 />
  •  The face of blue glacial ice melting into the sea
  •  Animation of Pangaea [[rifting]]
  • Eruption of the Mayon Volcano, Philippines, in 1984. Much of the material spewed from a volcanic eruption may eventually make its way into the oceans
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  • rounding]] (horizontal)}}
  • [[Scanning electron micrograph]] showing grains of [[silica sand]]
  • doi-access = free}}</ref>
  •  Well-sorted sediments (left) have particles that are all of a similar size. Poorly sorted sediments (right) consist of particles of a wide range of sizes
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  •  A plume of wind-borne particles from Sudan (left) blow over the Red Sea
  • Tektite-like glass found in western Russia
  • The [[Wentworth scale]] classifies sediment by [[grain size]]}}
  •  River discharge in the Yukon Delta, Alaska. The pale color demonstrates the large amounts of sediment released into the ocean via the rivers.
  •  doi-access = free }}</ref>

source sediments      

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  •  url-status = dead}}</ref><!-- See http://cm.bell-labs.com/cm/cs/who/dmr/ctut.pdf for original.-->
COLLECTION OF COMPUTER INSTRUCTIONS WRITTEN USING SOME HUMAN-READABLE COMPUTER LANGUAGE
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исходная программа
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  •  url-status = dead}}</ref><!-- See http://cm.bell-labs.com/cm/cs/who/dmr/ctut.pdf for original.-->
COLLECTION OF COMPUTER INSTRUCTIONS WRITTEN USING SOME HUMAN-READABLE COMPUTER LANGUAGE
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Definitie

Open Source Definition
<standard> (OSD) Definition of distribution terms for {open source} software, promoted by the Open Source Initiative. http://opensource.org/osd.html. (1999-11-28)

Wikipedia

Marine sediment

Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor. These particles have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea. Additional deposits come from marine organisms and chemical precipitation in seawater, as well as from underwater volcanoes and meteorite debris.

Except within a few kilometres of a mid-ocean ridge, where the volcanic rock is still relatively young, most parts of the seafloor are covered in sediment. This material comes from several different sources and is highly variable in composition. Seafloor sediment can range in thickness from a few millimetres to several tens of kilometres. Near the surface seafloor sediment remains unconsolidated, but at depths of hundreds to thousands of metres the sediment becomes lithified (turned to rock).

Rates of sediment accumulation are relatively slow throughout most of the ocean, in many cases taking thousands of years for any significant deposits to form. Sediment transported from the land accumulates the fastest, on the order of one metre or more per thousand years for coarser particles. However, sedimentation rates near the mouths of large rivers with high discharge can be orders of magnitude higher. Biogenous oozes accumulate at a rate of about one centimetre per thousand years, while small clay particles are deposited in the deep ocean at around one millimetre per thousand years.

Sediments from the land are deposited on the continental margins by surface runoff, river discharge, and other processes. Turbidity currents can transport this sediment down the continental slope to the deep ocean floor. The deep ocean floor undergoes its own process of spreading out from the mid-ocean ridge, and then slowly subducts accumulated sediment on the deep floor into the molten interior of the earth. In turn, molten material from the interior returns to the surface of the earth in the form of lava flows and emissions from deep sea hydrothermal vents, ensuring the process continues indefinitely. The sediments provide habitat for a multitude of marine life, particularly of marine microorganisms. Their fossilized remains contain information about past climates, plate tectonics, ocean circulation patterns, and the timing of major extinctions.

Vertaling van &#39source sediments&#39 naar Russisch