{"id":313,"date":"2020-02-12T08:51:57","date_gmt":"2020-02-12T11:51:57","guid":{"rendered":"https:\/\/www.ufsm.br\/unidades-universitarias\/ccr\/msrs\/?page_id=313"},"modified":"2020-06-19T16:05:07","modified_gmt":"2020-06-19T19:05:07","slug":"minerais-2","status":"publish","type":"page","link":"https:\/\/www.ufsm.br\/museus\/msrs\/minerais-2","title":{"rendered":"Minerais"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-page\" data-elementor-id=\"313\" class=\"elementor elementor-313\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-ba8b74a elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"ba8b74a\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-0fd1d67\" data-id=\"0fd1d67\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-1b71215 elementor-widget elementor-widget-text-editor\" data-id=\"1b71215\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p style=\"text-align: center\"><strong>Principais minerais prim\u00e1rios nos solos do RS<\/strong><\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-e91b27e elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"e91b27e\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-49fad10\" data-id=\"49fad10\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-3168b18 elementor-widget elementor-widget-image\" data-id=\"3168b18\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"300\" height=\"225\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Quartzo-300x225.jpg\" class=\"attachment-medium size-medium wp-image-895\" alt=\"\" srcset=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Quartzo-300x225.jpg 300w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Quartzo-768x576.jpg 768w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Quartzo.jpg 894w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Quartzo - Grupo: Silicatos (tectossilicatos) Composi\u00e7\u00e3o qu\u00edmica: SiO2 Origem no solo: proveniente do intemperismo de praticamente todos os tipos de rochas, abundante nas rochas sedimentares. Import\u00e2ncia no solo: mineral n\u00e3o reativo altamente resistente ao intemperismo. Formador da fra\u00e7\u00e3o areia dos solos, conferindo a estes elevada porosidade e drenagem.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-169b656\" data-id=\"169b656\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-a9aa3ce elementor-widget elementor-widget-image\" data-id=\"a9aa3ce\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/elementor\/thumbs\/Calcedonea-or9dw3yhih81iz45rv4ilvicpfq6xm8jjp7bo8w2bu.jpg\" title=\"Calcedonea\" alt=\"Calcedonea\" loading=\"lazy\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Calced\u00f4nia -  Grupo: Silicatos (tectossilicatos) Composi\u00e7\u00e3o qu\u00edmica: SiO2 Origem no solo: proveniente do intemperismo de praticamente todos os tipos de rochas,onde se geralmente ocorrem em fendas, veios ou cavidades. Import\u00e2ncia no solo: mineral n\u00e3o reativo altamente resistente ao intemperismo. Formador da fra\u00e7\u00e3o areia dos solos, conferindo a estes elevada porosidade e drenagem.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-4819e1d elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"4819e1d\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-cba0f11\" data-id=\"cba0f11\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-61465df elementor-widget elementor-widget-image\" data-id=\"61465df\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"300\" height=\"225\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-ortocl\u00e1sio-300x225.jpg\" class=\"attachment-medium size-medium wp-image-897\" alt=\"\" srcset=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-ortocl\u00e1sio-300x225.jpg 300w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-ortocl\u00e1sio-768x576.jpg 768w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-ortocl\u00e1sio.jpg 894w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Feldspato (ortocl\u00e1sio) - Grupo: Silicatos (tectossilicatos) Composi\u00e7\u00e3o qu\u00edmica: KAlSI3O8 Origem no solo:proveniente do intemperismo de v\u00e1rias rochas, principalmente das rochas plut\u00f4nicas como granitos, xistos e gnaisses. Import\u00e2ncia no solo:embora seja um mineral resistente ao intemperismo, atua como formador de argila e fonte de K no solo.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-ac64805\" data-id=\"ac64805\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-36a02d4 elementor-widget elementor-widget-image\" data-id=\"36a02d4\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"300\" height=\"225\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-plagioclasio-300x225.jpg\" class=\"attachment-medium size-medium wp-image-898\" alt=\"\" srcset=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-plagioclasio-300x225.jpg 300w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-plagioclasio-768x576.jpg 768w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Feldspato-plagioclasio.jpg 894w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Feldspato (plagiocl\u00e1sio) - Grupo: Silicatos (tectossilicatos) Composi\u00e7\u00e3o qu\u00edmica: (Na-Ca)nAlSI3O8 Origem no solo: proveniente do intemperismo de rochas magm\u00e1ticas \u00e1cidas a alcalinas. Import\u00e2ncia no solo:atua como formador de argila e fonte de Na e Ca no solo.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-6a2a82c elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"6a2a82c\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-4d9d537\" data-id=\"4d9d537\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-5d144a0 elementor-widget elementor-widget-image\" data-id=\"5d144a0\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"300\" height=\"225\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Magnetita-300x225.jpg\" class=\"attachment-medium size-medium wp-image-899\" alt=\"\" srcset=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Magnetita-300x225.jpg 300w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Magnetita-768x576.jpg 768w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Magnetita.jpg 896w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Magnetita - Grupo: \u00d3xido de ferro Composi\u00e7\u00e3o qu\u00edmica: Fe3O4 Origem no solo: proveniente do intemperismo de rochas magm\u00e1ticas \u00e1cidas a alcalinas. Tamb\u00e9m pode ocorrer em rochas metam\u00f3rficas. Import\u00e2ncia no solo:resistente ao intemperismo, atua como formador de argila e fonte de Fe no solo.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-58a29cf\" data-id=\"58a29cf\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-51879f2 elementor-widget elementor-widget-image\" data-id=\"51879f2\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/elementor\/thumbs\/Mica-muscovita-or9dzi5ifpmhokcjywdrbt9y285e7fyk05twvwnc22.jpg\" title=\"Mica muscovita\" alt=\"Mica muscovita\" loading=\"lazy\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Mica (muscovita) - Grupo: Silicato (filossilicato) Composi\u00e7\u00e3o qu\u00edmica: KAl2Si3AlO10(OH,F)2 Origem no solo: proveniente do intemperismo de rochas magm\u00e1ticas, metam\u00f3rficas e sedimentares. Import\u00e2ncia no solo: atua como formador de argila e fonte de K no solo.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-cc972d0 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"cc972d0\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-82a270c\" data-id=\"82a270c\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-7599f4f elementor-widget elementor-widget-image\" data-id=\"7599f4f\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"300\" height=\"225\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Mica-biotita-300x225.jpg\" class=\"attachment-medium size-medium wp-image-901\" alt=\"\" srcset=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Mica-biotita-300x225.jpg 300w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Mica-biotita-768x576.jpg 768w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Mica-biotita.jpg 898w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Mica (biotita) - Grupo: Silicato (filossilicato) Composi\u00e7\u00e3o qu\u00edmica: K2(Mg,Fe2+)6-4(Fe3+,Al,Ti)0-2Si6-5Al2-3O20(OH,F)4 Origem no solo: proveniente do intemperismo de rochas magm\u00e1ticas, metam\u00f3rficas e sedimentares. Import\u00e2ncia no solo: atua como formador de argila e fonte de Fe, Mg e K no solo.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-8f58fd8\" data-id=\"8f58fd8\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-632150e elementor-widget elementor-widget-image\" data-id=\"632150e\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"300\" height=\"225\" src=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Turmalina-300x225.jpg\" class=\"attachment-medium size-medium wp-image-902\" alt=\"\" srcset=\"https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Turmalina-300x225.jpg 300w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Turmalina-768x575.jpg 768w, https:\/\/www.ufsm.br\/app\/uploads\/sites\/806\/2020\/06\/Turmalina.jpg 896w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Turmalina - Grupo: Silicato (ciclossilicato) Composi\u00e7\u00e3o qu\u00edmica: Na(Fe,Mn)3Al6B3Si6O27(OH,F)4 Origem no solo: proveniente do intemperismo de rochas metam\u00f3rficas. Import\u00e2ncia no solo: atua como formador de argila no solo, podendo aparecer tamb\u00e9m na fra\u00e7\u00e3o areia.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>Principais minerais prim\u00e1rios nos solos do RS Quartzo &#8211; Grupo: Silicatos (tectossilicatos) Composi\u00e7\u00e3o qu\u00edmica: SiO2 Origem no solo: proveniente do intemperismo de praticamente todos os tipos de rochas, abundante nas rochas sedimentares. Import\u00e2ncia no solo: mineral n\u00e3o reativo altamente resistente ao intemperismo. Formador da fra\u00e7\u00e3o areia dos solos, conferindo a estes elevada porosidade e drenagem. [&hellip;]<\/p>\n","protected":false},"author":867,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"categories":[],"tags":[],"class_list":["post-313","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/pages\/313","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/users\/867"}],"replies":[{"embeddable":true,"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/comments?post=313"}],"version-history":[{"count":0,"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/pages\/313\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/media?parent=313"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/categories?post=313"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.ufsm.br\/museus\/msrs\/wp-json\/wp\/v2\/tags?post=313"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}