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This volume contains descriptions of sediments recovered by the R/V Polar Duke during two cruises made in 1990 to study the coastal and shelf regions of Antarctica, including core recovery and processing
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How to fill out SEDIMENT DESCRIPTIONS

01
Identify the sediment type (e.g., sand, silt, clay).
02
Describe the color of the sediment using standardized classifications.
03
Note the texture (grain size, shape, and distribution) of the sediment.
04
Evaluate the structure (e.g., layering, compactness) of the sediment.
05
Record the presence of any biological components (e.g., shells, organic material).
06
Document the moisture content (dry, wet, saturated).
07
Include any observations about odor or other distinct characteristics.

Who needs SEDIMENT DESCRIPTIONS?

01
Geologists conducting sedimentary research.
02
Environmental scientists assessing site conditions.
03
Engineers involved in construction and land development.
04
Regulatory agencies monitoring environmental compliance.
05
Researchers studying sediment transport processes.
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Tea leaves settling in the water. Soil settling at the pond of water. water treatment plants. Sewage treatment plants. Sand traps. Alluvium. Aeolian deposits (dunes). Sedimentary Islands.
Sediment is solid material that is moved and deposited in a new location. Sediment can consist of rocks and minerals, as well as the remains of plants and animals. It can be as small as a grain of sand or as large as a boulder. Sediment moves from one place to another through the process of erosion.
Sedimentary rocks are formed from deposits of pre-existing rocks or pieces of once-living organism that accumulate on the Earth's surface. If sediment is buried deeply, it becomes compacted and cemented, forming sedimentary rock.
There are four types: lithogenous, hydrogenous, biogenous and cosmogenous. Lithogenous sediments come from land via rivers, ice, wind and other processes. Biogenous sediments come from organisms like plankton when their exoskeletons break down. Hydrogenous sediments come from chemical reactions in the water.
Sediment texture is concerned with the grain-size and its distribution, morphology and surface features of grains, and the fabric of the sed- iment. Induration and weathering (see Section 4.7), and colour (see Section 4.8) are also considered in this chapter.
Sedimentation is the deposition of rock fragments, soil, organic matter, or dissolved material that has been eroded, that is, has been transported by water, wind, ice, or gravity.
Sedimentary rocks are formed from pre-existing rocks or pieces of once-living organisms. They form from deposits that accumulate on the Earth's surface. Sedimentary rocks often have distinctive layering or bedding.
There are four types: lithogenous, hydrogenous, biogenous and cosmogenous. Lithogenous sediments come from land via rivers, ice, wind and other processes. Biogenous sediments come from organisms like plankton when their exoskeletons break down. Hydrogenous sediments come from chemical reactions in the water.

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Sediment descriptions refer to the systematic analysis and documentation of sediment characteristics, including composition, texture, and other physical properties of sediment in a specific area.
Individuals or organizations involved in geological studies, environmental assessments, or projects that impact land and water bodies may be required to file sediment descriptions, including engineers, geologists, and environmental consultants.
To fill out sediment descriptions, one should collect sediment samples, analyze them for physical and chemical properties, and document the findings in a standardized format, ensuring to include details like sample location, depth, and observations about the sediment layers.
The purpose of sediment descriptions is to provide critical information for environmental assessments, land use planning, and resource management, helping to understand sediment composition and behavior in various contexts.
Essential information includes sample location and depth, sediment type and classification, physical characteristics (such as grain size and texture), chemical composition, and any relevant environmental context or observations.
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