{"id":295232,"date":"2024-10-19T20:04:44","date_gmt":"2024-10-19T20:04:44","guid":{"rendered":"https:\/\/pdfstandards.shop\/product\/uncategorized\/bs-iso-25962006\/"},"modified":"2024-10-25T17:20:10","modified_gmt":"2024-10-25T17:20:10","slug":"bs-iso-25962006","status":"publish","type":"product","link":"https:\/\/pdfstandards.shop\/product\/publishers\/bsi\/bs-iso-25962006\/","title":{"rendered":"BS ISO 2596:2006"},"content":{"rendered":"

This International Standard specifies the following four test methods for the determination of the hygroscopic moisture content of test samples:<\/p>\n

Method 1 – Gravimetric method;<\/p>\n

Method 2 – Karl Fischer volumetric method;<\/p>\n

Method 3 – Karl Fischer coulometric method;<\/p>\n

Method 4 – Mass-loss method.<\/p>\n

Any of these methods is applicable wherever the analytical value of a chemical constituent is to be calculated to a dried sample basis in the following ore types.<\/p>\n

    \n
  1. \n

    Processed ores containing metallic iron (direct reduced iron).<\/p>\n<\/li>\n

  2. \n

    Natural or processed ores in which the sulfur content is greater than 0,2 % (mass fraction).<\/i><\/p>\n<\/li>\n

  3. \n

    Natural or processed ores in which the combined water is greater than 2,5 % (mass fraction).<\/p>\n<\/li>\n<\/ol>\n

    Any of these methods is applicable to a concentration range of 0,05 % (mass fraction) to 4,5 % (mass fraction) hygroscopic moisture.<\/p>\n

    \n

    NOTE 1 Where the reportable moisture content of a commercial consignment of ore is required, the procedure in ISO 3087 is used.<\/p>\n<\/blockquote>\n

    \n

    NOTE 2 With natural or processed ores outside the field of application specified in a), b) or c), a determination of a constituent at any level of concentration may be conducted using any of these methods, or as specified in ISO 7764.<\/p>\n<\/blockquote>\n

    \n

    NOTE 3 Alternatively, the loss or ignition content may be measured as an estimate of the combined water content.<\/p>\n<\/blockquote>\n","protected":false},"excerpt":{"rendered":"

    Iron ores. Determination of hygroscopic moisture in analytical samples. Gravimetric, Karl Fischer and mass-loss methods<\/b><\/p>\n\n\n\n\n
    Published By<\/td>\nPublication Date<\/td>\nNumber of Pages<\/td>\n<\/tr>\n
    BSI<\/b><\/a><\/td>\n2006<\/td>\n42<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n","protected":false},"featured_media":295237,"template":"","meta":{"rank_math_lock_modified_date":false,"ep_exclude_from_search":false},"product_cat":[1049,2641],"product_tag":[],"class_list":{"0":"post-295232","1":"product","2":"type-product","3":"status-publish","4":"has-post-thumbnail","6":"product_cat-73-060-10","7":"product_cat-bsi","9":"first","10":"instock","11":"sold-individually","12":"shipping-taxable","13":"purchasable","14":"product-type-simple"},"_links":{"self":[{"href":"https:\/\/pdfstandards.shop\/wp-json\/wp\/v2\/product\/295232","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pdfstandards.shop\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/pdfstandards.shop\/wp-json\/wp\/v2\/types\/product"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/pdfstandards.shop\/wp-json\/wp\/v2\/media\/295237"}],"wp:attachment":[{"href":"https:\/\/pdfstandards.shop\/wp-json\/wp\/v2\/media?parent=295232"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/pdfstandards.shop\/wp-json\/wp\/v2\/product_cat?post=295232"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/pdfstandards.shop\/wp-json\/wp\/v2\/product_tag?post=295232"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}