What are sediment materials

Translation of "Sedimentmaterial" in English

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Process and system for cleaning contaminated Sediment material.
Sediment material, which consists of at least 50% material created by inorganic chemical processes in the sedimentation basin (EarthMaterial), includes inorganic silicate, carbonate, evaporite, iron and phosphate sediments.
Sedimentary material that of at least 50 percent material produced by inorganic chemical processes within the basin of deposition. Includes inorganic siliceous, carbonate, evaporite, iron-rich, and phosphatic sediment classes.
Sediment material, in which at least 50% of the primary and / or recrystallized components consist of one (or more) of the carbonate minerals calcite, aragonite and dolomite and were created as particles in a basin.
Sedimentary material in which at least 50 percent of the primary and / or recrystallized constituents are composed of one (or more) of the carbonate minerals calcite, aragonite and dolomite, in particles of intrabasinal origin.
Sediment material of an indeterminate state of solidification, at least 50% of the particles of which were created by erosion, weathering or mass movement of already existing earth materials (EarthMaterial) and have been transported mechanically (by water, wind, ice or gravity) to the deposition site.
Sedimentary material of unspecified consolidation state in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.
Sediment materialwhich consists of at least 50% silicate minerals which have been deposited by direct chemical or biological processes on the formation surface or in particles formed by chemical or biological processes in the sedimentation basin.
Sedimentary material that consists of at least 50 percent silicate mineral material, deposited directly by chemical or biological processes at the depositional surface, or in particles formed by chemical or biological processes within the basin of deposition.
Preferably is formulated Sediment material (so-called reconstituted, artificial or synthetic sediment).
Formulated sediment (also called reconstituted, artificial or synthetic sediment) should preferably be used.
The raw material for this is anhydrite, a dry, plaster-like material Sediment material.
The raw material for these is anhydrite, a dry, gypsum-like sedimentary material.
In addition to the total dry weight, the ash-free dry weight can also be determined, as described in (49), in order to also remove inorganic components from the Sediment material to be considered in the digestive tract of the worms.
In addition to the total dry weight, the ash-free dry weight may be determined as described in (49) in order to account for inorganic components originating from ingested sediment present in the alimentary tract of the worms.
Microstructure according to one of the preceding claims, characterized in that sections I, II, III, IV are present in the chamber structure (10, 110) which have different depths and can be used to Sediment material or to capture and release other particles.
Microstructure in accordance with any of the previous claims characterized in that in said chamber structure (10,110) has sections I, II, III, IV which have different depths and which can be used to trap and release sedimenting material or other particles.
Sediment materialcaused by the accumulation of solid fragments deposited by air, water or ice or by other natural accumulation, e.g. by precipitation or secretion of organisms.
material formed by accumulation of solid fragmental material deposited by air, water or ice, or material that accumulated by other natural agents such as chemical precipitation from solution or secretion by organisms.
Sediment material, in which at least 50% of the primary material consists of organic carbon.
Sedimentary material in which 50 percent or more of the primary sedimentary material is organic carbon.
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