todorokite structure 钡镁锰矿型结构
The transformation of birnessite→buserite→todorokite is an important pathway for todoroktie formation.
水钠锰矿→布塞尔矿→钙锰矿的转化是钙锰矿形成的一个重要途径。
参考来源 - 钙锰矿的研究进展The manganese-dominant mineral of Cobalt-rich crusts in this area isδ-MnO_2, for the three main manganese minerals of todorokite, birnessite andδ-MnO_2 in deep seas,δ-MnO_2 is the most thorough oxidized mineral, the O/Mn are 1.74~1.87,1.87~2.00,1.99.
3.研究区富钴结壳的锰矿物为δ-MnO_2,前人研究表明:在最主要的三种深海锰矿物钡镁锰矿、钠水锰矿和δ-MnO_2中,δ-MnO_2是氧化最彻底的矿物,三者的O/Mn值依次为1.74~1.87,1.87~2.00,1.99。
参考来源 - 西太平洋海山富钴结壳中富锰矿物的组分及结构研究·2,447,543篇论文数据，部分数据来源于NoteExpress
以上来源于: WordNet
The major components of manganese nodules are todorokite with a tunnel-like structure and also buserite and birnessite with layered structures.
锰结核的主要矿物是具有隧道孔结构的钙锰矿以及具有层状结构的似水锰矿和水钠锰矿。
These results can provide theoretical clues for further revealing the origination of todorokite in environments and for prompting applications of todorokite in the area of material science.
这进一步明确了钙锰矿的生成条件，可为阐明钙锰矿的形成机制和促进其在材料科学中的应用提供理论依据。
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