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| 1 | Distribution Characteristics of Cobalt-rich Ferromanganese Crust Resources on Submarine Seamounts in the Western Pacific显示文摘在西方的太平洋,基于五个海底的海底山省(链) 的调查数据充满钴的铁锰合金外壳资源的分发特征被使用相对引用数据并且使用热点并且 seafloor 传播的理论在这篇论文研究了。获得的主要研究结果如下:在学习区域的合作富人外壳厚度逐渐地从东方正在增加到西方并且从南方到向北有否定关联(r =? 0.59 ) 与经度和积极关联(r = 0.48 ) 与纬度。沿着经度和纬度变化的外壳厚度被热点并且 seafloor 传播影响。在学习区域的西北部分的海洋的外壳和海底山更旧,并且外壳资源比在东南部分的那些优异。深入地 < 1500 m, 15002000 m,在学习区域的 20002500 m,钴外壳厚度是分别地 5.45 厘米, 4.34 厘米和 3.55 厘米,并且深入地 25003000 m 和 30003500 m 的,它分别地落下到 2.84 厘米和 3.37 厘米。合作富人外壳资源主要深入地在海底山顶点边缘和上面的胁腹被集中 < 2500 m。有强壮的否定关联(r =? 0.67 ) 在钴外壳丰富和在 0 的斜坡的海底山, 75 kg/m2 和 50 kg/m2 的斜坡之间 ? 瑳条 ? 整摮 ? 潴猠慴楢楬敺吗?? | ZHANG Fuyuan ZHANG Weiyan ZHU Kechao GAO Shuitu ZHANG Haisheng ZHANG Xiaoyu ZHU Benduo | 2008 | Acta Geologica Sinica(English Edition)2008，82，4： | 6 |
| 2 | Designing high-strength titanium alloy using pseudo-spinodal mechanism through diffusion multiple experiment and CALPHAD calculation显示文摘This study used the pseudo-spinodal mechanism to obtain the ultrafineαphase for designing highstrength titanium alloy.Diffusion multiple experiments were designed to find the composition range of TM-x Mo-y V alloy(TM:Ti-4.5 Al-2 Cr-2.5 Nb-2 Zr-1 Sn)for obtaining ultrafineαphase.CALPHAD results confirm that when the alloy composition is located near the intersection of theαandβphase free energy curves,the alloy will undergo pseudo-spinodal transformation and obtain the ultrafineαphase.The designed TM-6 Mo-3 V alloy has a yield strength of 1411 MPa and an elongation of 6.5%.The strength of the alloy depends on the thickness,fraction of theαphase and the solid solution strengthening effect of the alloying elements.The deformation mechanism of the alloy is the dislocation slip of theαandβphases and the twin deformation of theαphase.The large number ofα/βinterfaces produced by the fineαphase is the main reason for limiting the ductility of the alloy.The use of the pseudo-spinodal mechanism combined with diffusion multiple experiments and CALPHAD is an effective method for designing high-strength titanium alloys. | Di Wu Libin Liu Lijun Zeng Wenguang Zhu Wanlin Wang Xiaoyong Zhang Junfeng Hou Baoliang Liu Jiafeng Lei Kechao Zhou | 2021 | Journal of Materials Science & Technology2021，，15： | 3 |
| 3 | Recovery of yttrium from deep-sea mud显示文摘Deep-sea mud rich in rare earth yttrium has received lots of attention from the international community as a new resource for Y. A novel process, which mainly includes acid leaching, solvent extraction, and oxalic acid precipitation-roasting, is proposed for recovery of Y from deep-sea mud. A series of experiments were conducted to inspect the impacts of various factors during the process and the optimum conditions were determined. The results show that the Y of deep-sea mud totally exists in apatite minerals which can be decomposed by hydrochloric acid and sulfuric acid solution. The highest leaching efficiency of Y is 94.53% using hydrochloric acid and 84.38% using sulfuric acid under the conditions of H^+concentration 2.0 mol/L, leaching time 60 min, liquid-solid ratio 4:1 and room temperature 25 ℃(only in case of sulfuric acid, when using hydrochloric acid, the leaching temperature should be 60 ℃). Because of the much lower leaching temperature, sulfuric acid leaching is preferred. The counter current extraction and stripping tests were simulated by a cascade centrifugal extraction tank device. Using 10 vol% P204,15 vol% TBP and 75 vol% sulfonated kerosene as extractant, 98.79% Y^(3+) and 42.60% Fe^(3+) are extracted from sulfuric acid leaching liquor(adjusted to pH = 2.0) after seven-stage counter current extraction with O/A ratio of 1:1 at room temperature, while other metals ions such as Al^(3+), Ca^(2+), Mg^(2+)and Mn^(2+) are almost not extracted. The Y^(3+) in loaded organic can be selectively stripped using 50 g/L sulfuric acid solution and the stripping efficiency reaches 99.86% after seven-stage counter current stripping with O/A ratio of 10:1 at room temperature, while only 2.26% co-extracted Fe^(3+) is stripped. The Y^(3+) of loaded strip liquor can be precipitated by oxalic acid to further separate Y^(3+) and Fe^(3+). The precipitation efficiency of Y^(3+) in loaded strip liquor can be 98.56% while Fe^(3+) is not precipitated under the conditions of oxalic acid solution concentration 200 g/L, quality ratio of oxalic acid to Y of 2, and precipitation time 0.5 h. And the precipitate was roasted at 850 ℃ for 3 h to obtain the oxide of Y in which the purity of Y_2 O_3/REO is 79.02% and the contents of major non-rare earth impurities are less than 0.21%.Over the whole process included acid leaching, solvent extraction, and oxalic acid precipitation-roasting,the yttrium yield is 82.04%. | Kuifang Zhang Zhiqiang Liu Changyong Sun Hongyang Cao Kechao Zhu Wei Zhu Wei Li | 2018 | Journal of Rare Earths2018，36，8： | 2 |
| 4 | Geochemical characteristics and metal element enrichment in crusts from seamounts of the Western Pacific显示文摘元素的地球化学是理解矿化作用机制的必要部分。在这份报纸, 544 钴外壳的一个数据集合从西方的太平洋的海底山取样被用来学习金属元素的丰富特征。REE 正规化被利用揭示外壳的起源;公司丰富和矿物质质量上的 phosphatization 的影响上的水深度的效果被讨论获得这些的进化海洋的矿藏,它支持进一步的资源评价。结论如下被得出:1 ) 元素的丰富,内部元素的关系,和为从不同地点的磷酸盐穷人外壳的使页岩正常化的 REE 模式反映外壳的 hydrogenetic 起源。REE 的 EF (丰富系数) 从表面沉积展出指数的增加到磷钙土到 polymetallic 小瘤到外壳,建议 hydrogeneous 起源的改进的度导致 REE 的丰富。2 ) 在西方的太平洋的外壳,通过生产 guyots 落后于的热点形成了,比那些有相对更低的 REE 在中间和平。后者能被归因于 intraplate 火山作用形成的海底山的古怪海底的地形学。3 ) non-phosphatized 更年轻的外壳层比 phosphatized 有 40% 更高的公司更旧的层。这由 phosphatization 在这些外壳中显示元素的作文的修正。象 P, Ca, Ba,和 Sr 的公司, Ni,和 Mn 和丰富那样的氢氧化物主导的元素的一般弄空在 phosphatized 外壳中是明显的,而更年轻的产生外壳是的 non-phosphatized 富于源自陆地的铝矽酸盐由岩屑形成的物质。4 ) 在在有不到 2,500 m 的水深度的海底山区域的到超过 0.65% 的从不到 0.53% 的碳酸盐赔偿深度(电荷耦合器件) 上面的公司增加,在海水列建议碳酸盐的溶解的意义到外壳的生长和作文。 | Xiaoyu ZHANG Kechao ZHU Yong DU Fuyuan ZHANG Weiyan ZHANG Xiangwen REN Binbin JIANG Dasong HUANG | 2016 | Frontiers of Earth Science2016，10，1： | 1 |
| 5 | 显示文摘 | Huang Suping Zhou Kechao Zhu Wu | 2006 | Journal of Applied Polymer Science2006，101，3： | 1 |
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