Cradle to Consumer
Identity ID
a6c2735b-6ef9-423b-94d9-b0aba0c23b12
Materials
Associated ID
f0d80c76-624d-4557-bb23-cf2e25ac98a1
Included activities starts
Included activities ends
Description
This is a market dataset representing the consumption market in the region. It includes transportation of the product from the factory gate to consumption, with transport services calculated according to the regional transportation conditions for the product.
Activity Description
This dataset is a market activity dataset. Each market represents a consumption mix of products within a specific region, connecting suppliers with consumers of the same product within that region. Markets encompass both producers and importers of the product within the same geographical area. Additionally, markets account for the transportation of products to consumers, as well as losses occurring during the transport process.
Process Description
Vanadium-titanium magnetite is a complex associated mineral primarily composed of iron, vanadium, and titanium, accompanied by various valuable elements (such as chromium, cobalt, nickel, copper, scandium, gallium, and platinum group elements), with high contents of valuable elements. It is an important industrial mineral raw material with high development and comprehensive utilization value. In nature, vanadium-titanium magnetite mainly forms in mafic and ultramafic rock bodies. Common valuable ore minerals in the resulting deposits are mainly titanomagnetite and ilmenite, along with minor amounts of magnetite, hematite, and sulfides. Ilmenite is a magnetite containing solid solution exsolutions such as ilmenite, ulvospinel, and magnesio-aluminate spinel, which can crystallize into ilmenite and magnetite through regional metamorphism. Vanadium-titanium magnetite typically contains 1%–15% TiO₂ and 0.1%–2% V₂O₅. The chemical composition of ilmenite is FeTiO₃, and ilmenite contains 52% TiO₂. 66%, with Fe2+ capable of complete isomorphous substitution with Mg2+ or Mn2+, forming the FeTiO3-MgTiO3 or FeTiO3-MnTiO3 series. When FeO is dominant, it is called ilmenite; when MgO is dominant, it is called geikielite; and when MnO is dominant, it is called pyrophanite. Ilmenite has a Mohs hardness of 5–6, a specific gravity of 4.70–4.78, exhibits weak magnetism, and has a magnetic susceptibility of 1173.33–224.56×10⁻⁹ m³/kg.
Time period
2022
2026
Geography
China,Sichuan
Geography comment
Form Sichuan average data by merging multiple datasets.
Macroeconomic value
Business-as-Usual
Data validation
Yes
Technology
Current Technology
Technology comment
Not specified