Journal Article10.1306/D4269774-2B26-11D7-8648000102C1865D
Nomenclature Based on Sand-silt-clay Ratios
1.8K
TL;DR: In this paper, an attempt is made to standardize nomenclature of sediment types relative to sand, silt, and clay content, and a triangle diagram with boundaries between types is submitted and compared with other systems which have been used for the purpose.
read more
Abstract: Following a canvassing of sedimentationists an attempt is made to standardize nomenclature of sediment types relative to sand, silt, and clay content. A triangle diagram with boundaries between types, which met with general approval, is submitted and compared with other systems which have been used for the purpose. The new system uses old well established names and has a simplicity and symmetry which make it easily remembered. The boundaries appear to be well located for description of sediments such as those that have been analyzed in large volume from the investigations of the northern Gulf of Mexico (API Project 51), but it is inadequate in describing well sorted sediments with median diameters near the boundaries of sand and silt or silt and clay. The nomenclature suggested applie only to sediment grade sizes so that other names should be used depending on other characteristics of the sediments. Furthermore, the nomenclature should not be applied to sediments containing large percentages of gravel.
read more
Chat with Paper
AI Agents for this Paper
Find similar papers on Google Scholar, PubMed and Arxiv
Write a critical review of this paper
Analyze citations of this paper to find unaddressed research gaps
Citations
Chemistry of Southern Chesapeake Bay sediments
TL;DR: In this paper, the depositional and early diagenetic environments in southern Chesapeake Bay are interpreted in terms of horizontal and vertical variations of percent content by weight of sediment of (1) organic and inorganic arbon, (2) total phosphorus, (3) total iron, (4) calcium and magnesium, (5) sodium and potassium, and (6) Kjeldahl nitrogen.
6
Revealing monsoonal variability of the last 2,500 years over India using sedimentological and foraminiferal proxies
TL;DR: A 2m-long shallow-water sediment core, representing the last 2,500 years, collected from the tropical Arabian Sea from the inner shelf (22 m water depth) off Karwar, near the mouth of the Kali River, has been studied for sedimentological proxies (granulometry) and foraminiferal tracers of paleomonsoons.
6