The content presented here represents the most current version of this section, which was printed in the 24th edition of Standard Methods for the Examination of Water and Wastewater.
Abstract: 4500-SiO2 A. Introduction

1. Occurrence and Significance

Silicon does not occur free in nature, but rather as free silica (SiO2) in coarsely crystalline (quartz, rock crystal, amethyst, etc.) and microcrystalline (e.g., flint, chert, jasper) varieties of quartz, the major component of sand and sandstone. Silicon is found in combination with other elements in silicates, represented by feldspar, hornblende, mica, asbestos, and other clay minerals. Silicates also occur in rocks, such as granite, basalt, and shale. Silicon therefore is usually reported as silica (SiO2) when rocks, sediments, soils, and water are analyzed. The average abundance of silica in different rock types is 7% to 80%, in typical soils 50% to 80%, and in surface and groundwater 14 mg/L.

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CITATION

Standard Methods Committee of the American Public Health Association, American Water Works Association, and Water Environment Federation. 4500-sio2 silica In: Standard Methods For the Examination of Water and Wastewater. Lipps WC, Baxter TE, Braun-Howland E, editors. Washington DC: APHA Press.

DOI: 10.2105/SMWW.2882.095

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