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Glauconite is a greenish, micaceous mineral that is primarily composed of potassium, iron, magnesium, and aluminum. It is a type of glauconite-group mineral, which is formed under low-temperature and low-pressure conditions, typically in marine environments. Glauconite is often found in sedimentary rocks such as shale, sandstone, and limestone, and it is known for its ability to expand when heated due to the presence of water within its structure. This property makes it useful in various industrial applications, including as a catalyst in the production of certain chemicals and as a component in drilling mud for oil and gas extraction. Additionally, glauconite has been used as a source of potassium for fertilizers and as a pigment in paints and ceramics. Its unique properties and formation process make glauconite an interesting and valuable mineral in both geological and industrial contexts.

1317-57-3

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1317-57-3 Usage

Check Digit Verification of cas no

The CAS Registry Mumber 1317-57-3 includes 7 digits separated into 3 groups by hyphens. The first part of the number,starting from the left, has 4 digits, 1,3,1 and 7 respectively; the second part has 2 digits, 5 and 7 respectively.
Calculate Digit Verification of CAS Registry Number 1317-57:
(6*1)+(5*3)+(4*1)+(3*7)+(2*5)+(1*7)=63
63 % 10 = 3
So 1317-57-3 is a valid CAS Registry Number.

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1317-57-3Related news

Formation and evolution of GLAUCONITE (cas 1317-57-3) in the Demerara Contourite depositional system related to NADW circulation changes during late Quaternary (French Guiana)08/20/2019

The Demerara Plateau is a marginal plateau which forms a bathymetric relief on the sea floor. Here, contourite deposits have been studied in detail, following the recent discovery of contourite sequences likely related to the bottom currents and linked both to contour current and peculiar sea-fl...detailed

Origin of the GLAUCONITE (cas 1317-57-3) from the Middle Eocene, Qarara Formation, Egypt08/19/2019

Although the Middle Eocene sediments at the Nile Valley, Egypt have been extensively studied, the origin of glauconites in these sediments is still questionable. In this paper, the glauconites that occur in the Qarara Formation were subjected to petrographical and mineralogical studies to assess...detailed

Weathering of GLAUCONITE (cas 1317-57-3) in an alkaline environment — A case study from Krakow area, Poland08/17/2019

The purpose of the study was to investigate glauconite weathering in regolith profile developed on Santonian marls in Zabierzów (South Poland) most likely during Paleogene. Because of the high carbonates content the studied regolith appears to constitute a unique case where glauconite underwent...detailed

Weathering of GLAUCONITE (cas 1317-57-3) in alkaline soils of temperate climate: A case study from Górniki, eastern Poland08/15/2019

The aim of the present study was to investigate the process of glauconite weathering in an alkaline soil under temperate climatic conditions. Calcaric Cambisol developed on Miocene sand in eastern Poland, and the sand containing parent glauconite, were sampled and analyzed using optical microsco...detailed

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