{"id":771,"date":"2018-02-09T19:02:30","date_gmt":"2018-02-10T00:02:30","guid":{"rendered":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/chapter\/18-2-industrial-minerals\/"},"modified":"2023-07-04T13:16:38","modified_gmt":"2023-07-04T17:16:38","slug":"industrial-minerals","status":"publish","type":"chapter","link":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/chapter\/industrial-minerals\/","title":{"raw":"18.2 Industrial Minerals","rendered":"18.2 Industrial Minerals"},"content":{"raw":"Metals are critical for our technological age, but other not-so-shiny materials are also needed to facilitate our way of life. For everything made out of concrete or asphalt, we need sand and gravel. To make the cement that holds concrete together, we also need limestone. For the glass in our computer screens and for glass-sided buildings, we need silica sand plus sodium oxide (Na<sub>2<\/sub>O), sodium carbonate (Na<sub>2<\/sub>CO<sub>3<\/sub>), and calcium oxide (CaO). Potassium is an essential nutrient for farming in many areas, and we also need various types of clay for a wide range of applications (e.g., ceramics and many industrial processes).\r\n<h1>Aggregate<\/h1>\r\nThe best types of <strong>aggregate<\/strong> (sand and gravel) resources are those that have been sorted by streams, and in Canada the most abundant and accessible fluvial deposits are associated with glaciation. That doesn\u2019t include till, because it has too much silt and clay, but it does include <strong>glaciofluvial outwash<\/strong> (deposits from glacier-derived rivers), which is present in thick deposits in many parts of the country (Figure 18.15).\r\n\r\n[caption id=\"attachment_768\" align=\"aligncenter\" width=\"550\"]<img class=\"wp-image-768\" src=\"https:\/\/opentextbc.ca\/kzlab\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1-300x155.jpg\" alt=\"\" width=\"550\" height=\"284\" \/> <strong>Figure 18.15<\/strong> Sand and gravel in an aggregate pit near Nanaimo, BC. Source: Steven Earle (2015), CC BY 4.0. <a href=\"https:\/\/opentextbc.ca\/geology\/wp-content\/uploads\/sites\/110\/2015\/08\/Sand-and-gravel-in-an-aggregate-pit.jpg\">Image source.<\/a>[\/caption]\r\n\r\nIn a typical gravel pit, materials are graded on-site according to size. They are then used in a wide range of applications from constructing huge concrete dams to filling children\u2019s sandboxes. Sand is also used to make glass, but for most types of glass, it has to be at least 95% quartz (which the sandy layers shown in Figure 18.15 are definitely not), and for high-purity glass and the silicon wafers used for electronics, the source sand has to be over 98% quartz.\r\n<h1>Limestone for Concrete<\/h1>\r\nApproximately 80 million tonnes of concrete are used in Canada each year\u2014a little over 2 tonnes per person. The cement used for concrete is made from approximately 80% calcite (CaCO<sub>3<\/sub>) and 20% clay. This mixture is heated to 1450\u00b0C to produce the required calcium silicate compounds (e.g., Ca<sub>2<\/sub>SiO<sub>4<\/sub>). The calcite typically comes from limestone quarries like the one on Texada Island, B.C. (Figure 18.16). Limestone is also used as the source material for many other products that require calcium compounds, including steel and glass, pulp and paper, and plaster products for construction.\r\n\r\n[caption id=\"attachment_769\" align=\"aligncenter\" width=\"550\"]<img class=\"wp-image-769\" src=\"https:\/\/opentextbc.ca\/kzlab\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1-300x157.jpg\" alt=\"\" width=\"550\" height=\"287\" \/> <strong>Figure 18.16<\/strong> Triassic Quatsino Formation limestone being quarried on Texada Island, B.C. Source: Steven Earle (2015), CC BY 4.0. <a href=\"https:\/\/opentextbc.ca\/geology\/wp-content\/uploads\/sites\/110\/2015\/08\/Triassic-Quatsino-Formation-limestone.jpg\">Image source.<\/a>[\/caption]\r\n<h1>Evaporite Minerals<\/h1>\r\nSodium is required for a wide range of industrial processes, and the most convenient source is sodium chloride (the mineral halite, also called rock salt), which is mined from evaporite beds in various parts of Canada. The largest salt mine in the world is at Goderich, Ontario, where salt is recovered from the 100 m thick Silurian Salina Formation. The same formation is mined in the Windsor area. Rock salt is also used as a source of sodium and chlorine in the chemical industry to melt ice on roads, as part of the process of softening water, and as a seasoning.\r\n\r\nUnder certain conditions, the mineral sylvite (KCl) accumulates in evaporite beds, and this rock is called <strong>potash<\/strong>. This happened across the Canadian prairies during the Devonian, creating the Prairie evaporite formation. Potassium is used as a crop fertilizer, and Canada is the world\u2019s leading supplier, with most of that production coming from Saskatchewan.\r\n\r\nAnother evaporite mineral, gypsum (CaSO<sub>4<\/sub>.2H<sub>2<\/sub>0), is the main component of plasterboard (drywall) that is widely used in the construction industry. One of the main mining areas for gypsum in Canada is in the Milford Station area of Nova Scotia, site of the world\u2019s largest gypsum mine.\r\n<h1>Building Materials<\/h1>\r\nRocks are quarried or mined for many different uses, such as building facades (Figure 18.17), countertops, stone floors, and headstones. In most of these cases, the favoured rock types are granitic rocks, slate, and marble. Quarried rock is also used in some applications where rounded gravel isn\u2019t suitable, such as the ballast (road bed) for railways, where crushed angular rock is needed.\r\n\r\n[caption id=\"attachment_770\" align=\"aligncenter\" width=\"550\"]<img class=\"wp-image-770\" src=\"https:\/\/opentextbc.ca\/kzlab\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1-300x221.jpg\" alt=\"\" width=\"550\" height=\"404\" \/> <strong>Figure 18.17<\/strong> Slate used as a facing material on a concrete building column in Vancouver Source: Steven Earle (2015), CC BY 4.0. <a href=\"https:\/\/opentextbc.ca\/geology\/wp-content\/uploads\/sites\/110\/2015\/08\/Slate-used-as-a-facing-material.jpg\">Image source.<\/a>[\/caption]\r\n\r\n<div class=\"textbox shaded\">\r\n\r\n<strong><a id=\"259\"><\/a>Do You Know Where to Find the Materials You Need?<\/strong>\r\n\r\n<div class=\"offline\">\r\n\r\n<strong>Which mineral do you need?<\/strong>\r\n<ol>\r\n \t<li>For high-purity glass and silicon wafers used in electronics, you need...<\/li>\r\n \t<li>For the cement in concrete you need...<\/li>\r\n \t<li>For sodium oxide for making glass windows, you need...<\/li>\r\n \t<li>To add drywall to your home renovation project, you need...<\/li>\r\n \t<li>For fertilizer, you need...<\/li>\r\n<\/ol>\r\nFill-in-the-blank options:\r\n<ul class=\"threecolumn\">\r\n \t<li>halite<\/li>\r\n \t<li>gypsum<\/li>\r\n \t<li>calcite<\/li>\r\n \t<li>sylvite<\/li>\r\n \t<li>quartz<\/li>\r\n<\/ul>\r\n<strong>To check your answers, navigate to the below link to view the interactive version of this activity.<\/strong>\r\n\r\n<\/div>\r\n[h5p id=\"185\"]\r\n<\/div>","rendered":"<p>Metals are critical for our technological age, but other not-so-shiny materials are also needed to facilitate our way of life. For everything made out of concrete or asphalt, we need sand and gravel. To make the cement that holds concrete together, we also need limestone. For the glass in our computer screens and for glass-sided buildings, we need silica sand plus sodium oxide (Na<sub>2<\/sub>O), sodium carbonate (Na<sub>2<\/sub>CO<sub>3<\/sub>), and calcium oxide (CaO). Potassium is an essential nutrient for farming in many areas, and we also need various types of clay for a wide range of applications (e.g., ceramics and many industrial processes).<\/p>\n<h1>Aggregate<\/h1>\n<p>The best types of <strong>aggregate<\/strong> (sand and gravel) resources are those that have been sorted by streams, and in Canada the most abundant and accessible fluvial deposits are associated with glaciation. That doesn\u2019t include till, because it has too much silt and clay, but it does include <strong>glaciofluvial outwash<\/strong> (deposits from glacier-derived rivers), which is present in thick deposits in many parts of the country (Figure 18.15).<\/p>\n<figure id=\"attachment_768\" aria-describedby=\"caption-attachment-768\" style=\"width: 550px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-768\" src=\"https:\/\/opentextbc.ca\/kzlab\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1-300x155.jpg\" alt=\"\" width=\"550\" height=\"284\" srcset=\"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1-300x155.jpg 300w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1-768x397.jpg 768w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1-65x34.jpg 65w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1-225x116.jpg 225w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1-350x181.jpg 350w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2018\/02\/Sand-and-gravel-in-an-aggregate-pit-1024x529-1.jpg 1024w\" sizes=\"auto, (max-width: 550px) 100vw, 550px\" \/><figcaption id=\"caption-attachment-768\" class=\"wp-caption-text\"><strong>Figure 18.15<\/strong> Sand and gravel in an aggregate pit near Nanaimo, BC. Source: Steven Earle (2015), CC BY 4.0. <a href=\"https:\/\/opentextbc.ca\/geology\/wp-content\/uploads\/sites\/110\/2015\/08\/Sand-and-gravel-in-an-aggregate-pit.jpg\">Image source.<\/a><\/figcaption><\/figure>\n<p>In a typical gravel pit, materials are graded on-site according to size. They are then used in a wide range of applications from constructing huge concrete dams to filling children\u2019s sandboxes. Sand is also used to make glass, but for most types of glass, it has to be at least 95% quartz (which the sandy layers shown in Figure 18.15 are definitely not), and for high-purity glass and the silicon wafers used for electronics, the source sand has to be over 98% quartz.<\/p>\n<h1>Limestone for Concrete<\/h1>\n<p>Approximately 80 million tonnes of concrete are used in Canada each year\u2014a little over 2 tonnes per person. The cement used for concrete is made from approximately 80% calcite (CaCO<sub>3<\/sub>) and 20% clay. This mixture is heated to 1450\u00b0C to produce the required calcium silicate compounds (e.g., Ca<sub>2<\/sub>SiO<sub>4<\/sub>). The calcite typically comes from limestone quarries like the one on Texada Island, B.C. (Figure 18.16). Limestone is also used as the source material for many other products that require calcium compounds, including steel and glass, pulp and paper, and plaster products for construction.<\/p>\n<figure id=\"attachment_769\" aria-describedby=\"caption-attachment-769\" style=\"width: 550px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-769\" src=\"https:\/\/opentextbc.ca\/kzlab\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1-300x157.jpg\" alt=\"\" width=\"550\" height=\"287\" srcset=\"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1-300x157.jpg 300w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1-768x401.jpg 768w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1-65x34.jpg 65w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1-225x118.jpg 225w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1-350x183.jpg 350w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Triassic-Quatsino-Formation-limestone-1024x535-1.jpg 1024w\" sizes=\"auto, (max-width: 550px) 100vw, 550px\" \/><figcaption id=\"caption-attachment-769\" class=\"wp-caption-text\"><strong>Figure 18.16<\/strong> Triassic Quatsino Formation limestone being quarried on Texada Island, B.C. Source: Steven Earle (2015), CC BY 4.0. <a href=\"https:\/\/opentextbc.ca\/geology\/wp-content\/uploads\/sites\/110\/2015\/08\/Triassic-Quatsino-Formation-limestone.jpg\">Image source.<\/a><\/figcaption><\/figure>\n<h1>Evaporite Minerals<\/h1>\n<p>Sodium is required for a wide range of industrial processes, and the most convenient source is sodium chloride (the mineral halite, also called rock salt), which is mined from evaporite beds in various parts of Canada. The largest salt mine in the world is at Goderich, Ontario, where salt is recovered from the 100 m thick Silurian Salina Formation. The same formation is mined in the Windsor area. Rock salt is also used as a source of sodium and chlorine in the chemical industry to melt ice on roads, as part of the process of softening water, and as a seasoning.<\/p>\n<p>Under certain conditions, the mineral sylvite (KCl) accumulates in evaporite beds, and this rock is called <strong>potash<\/strong>. This happened across the Canadian prairies during the Devonian, creating the Prairie evaporite formation. Potassium is used as a crop fertilizer, and Canada is the world\u2019s leading supplier, with most of that production coming from Saskatchewan.<\/p>\n<p>Another evaporite mineral, gypsum (CaSO<sub>4<\/sub>.2H<sub>2<\/sub>0), is the main component of plasterboard (drywall) that is widely used in the construction industry. One of the main mining areas for gypsum in Canada is in the Milford Station area of Nova Scotia, site of the world\u2019s largest gypsum mine.<\/p>\n<h1>Building Materials<\/h1>\n<p>Rocks are quarried or mined for many different uses, such as building facades (Figure 18.17), countertops, stone floors, and headstones. In most of these cases, the favoured rock types are granitic rocks, slate, and marble. Quarried rock is also used in some applications where rounded gravel isn\u2019t suitable, such as the ballast (road bed) for railways, where crushed angular rock is needed.<\/p>\n<figure id=\"attachment_770\" aria-describedby=\"caption-attachment-770\" style=\"width: 550px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-770\" src=\"https:\/\/opentextbc.ca\/kzlab\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1-300x221.jpg\" alt=\"\" width=\"550\" height=\"404\" srcset=\"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1-300x221.jpg 300w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1-768x565.jpg 768w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1-65x48.jpg 65w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1-225x165.jpg 225w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1-350x257.jpg 350w, https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/360\/2021\/08\/Slate-used-as-a-facing-material-1024x753-1.jpg 1024w\" sizes=\"auto, (max-width: 550px) 100vw, 550px\" \/><figcaption id=\"caption-attachment-770\" class=\"wp-caption-text\"><strong>Figure 18.17<\/strong> Slate used as a facing material on a concrete building column in Vancouver Source: Steven Earle (2015), CC BY 4.0. <a href=\"https:\/\/opentextbc.ca\/geology\/wp-content\/uploads\/sites\/110\/2015\/08\/Slate-used-as-a-facing-material.jpg\">Image source.<\/a><\/figcaption><\/figure>\n<div class=\"textbox shaded\">\n<p><strong><a id=\"259\"><\/a>Do You Know Where to Find the Materials You Need?<\/strong><\/p>\n<div class=\"offline\">\n<p><strong>Which mineral do you need?<\/strong><\/p>\n<ol>\n<li>For high-purity glass and silicon wafers used in electronics, you need&#8230;<\/li>\n<li>For the cement in concrete you need&#8230;<\/li>\n<li>For sodium oxide for making glass windows, you need&#8230;<\/li>\n<li>To add drywall to your home renovation project, you need&#8230;<\/li>\n<li>For fertilizer, you need&#8230;<\/li>\n<\/ol>\n<p>Fill-in-the-blank options:<\/p>\n<ul class=\"threecolumn\">\n<li>halite<\/li>\n<li>gypsum<\/li>\n<li>calcite<\/li>\n<li>sylvite<\/li>\n<li>quartz<\/li>\n<\/ul>\n<p><strong>To check your answers, navigate to the below link to view the interactive version of this activity.<\/strong><\/p>\n<\/div>\n<div id=\"h5p-185\">\n<div class=\"h5p-iframe-wrapper\"><iframe id=\"h5p-iframe-185\" class=\"h5p-iframe\" data-content-id=\"185\" style=\"height:1px\" src=\"about:blank\" frameBorder=\"0\" scrolling=\"no\" title=\"Minerals in industrial materials\"><\/iframe><\/div>\n<\/div>\n<\/div>\n","protected":false},"author":123,"menu_order":2,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-771","chapter","type-chapter","status-publish","hentry"],"part":752,"_links":{"self":[{"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/771","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/users\/123"}],"version-history":[{"count":10,"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/771\/revisions"}],"predecessor-version":[{"id":1946,"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/771\/revisions\/1946"}],"part":[{"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/parts\/752"}],"metadata":[{"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/771\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/media?parent=771"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapter-type?post=771"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/contributor?post=771"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/opentextbc.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/license?post=771"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}