3篇
您的检索式：作者名="Linbo Shang"
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| 1 | An experimental study of tin partition between melt and aqueous fluid in F/Cl-coexisting magma显示文摘为了调查听矿石的形成机制,与忍受 F 花岗石联系了,在忍受 F 之间的听分区的试验性的研究花岗石融化,共存的忍受 HCl 水的液体与接近 NNO 的 fo 2 在 850 ° C 和 100MPa 被进行。锡的 Geochemical 行为被变化在以不同氧化铝浸透索引 ASI 开始稳固的材料跟踪,在 F 内容并且在开始各种各样的 HCl 集中的液体。结果显示出那 D 有 ASI 的 Sn 增加融化并且每铝土融化为进在 F/Cl-coexisting 系统的水的液体的听分区是有利的。更高的 HCl 集中的水的液体为锡的丰富是有益的。而且,在玻璃跑产品的氯内容在岩浆与 F 和 Cl 内容断然相关。在 F/Cl-coexisting 系统,花岗石在能为听矿石的形成用作一座水库的 melt 与内容(>∼1 wt%) 能提取并且充实的高 F 融化锡。然而,当在 melt 的 F 内容在 1 wt% 下面时,锡的分配系数将显著地增加。因此, F 内容的减少对进有高 HCl 内容的水的液体的锡的分区有利,因此支持热水的听矿石的免职。 | HU XiaoYan BI XianWu SHANG LinBo HU RuiZhong CAI GuoSheng CHEN YouWei | 2009 | Chinese Science Bulletin2009，54，6： | 4 |
| 2 | An experimental study on the solubility of copper bichloride in water vapor显示文摘Using the solubility method, the solubility of CuCl2 in liquid-undersaturated HCl-bearing water vapor was investigated experimentally at temperatures of 330-370 ℃ and pressures of 4.2-10 MPa. The re-sults have shown that hydration could significantly enhance copper solubility and the concentrations of copper were positively correlated with PH2O. The solubility of copper in vapor phase increased with increasing PH2O at the constant temperature. CuCl2 was transported as hydrated species CuCl2(H2O)ngas in water vapor. The formation of complexes is proposed to be the result of the following reaction: CuCl2solid + nH2Ogas = CuCl2 (H2O)ngas The hydration number n decreased slightly with increasing temperature. Statistical hydration numbers are 4.0, 3.6 and 3.3 at 330, 350 and 370 ℃ , respectively. | SHANG LinBo BI XianWu HU RuiZhong FAN WenLing | 2007 | Chinese Science Bulletin2007，52，3： | 3 |
| 3 | Copper partitioning between granitic silicate melt and coexisting aqueous fluid at 850°C and 100 MPa显示文摘Experiments on the partitioning of Cu between different granitic silicate melts and the respective coexisting aqueous fluids have been performed under conditions of 850 °C, 100 MPa and oxygen fugacity(f O_2) buffered at approaching Ni–Ni O(NNO). Partition coefficients of Cu(DCu= cfluid/cmelt) were varied with different alumina/alkali mole ratios [Al_2O_3/(Na_2O·K_2O), abbreviated as Al/Alk], Na/K mole ratios, and Si O_2 mole contents. The DCu increased from 1.28 ± 0.01 to 22.18 ± 0.22 with the increase of Al/Alk mole ratios(ranging from 0.64 to 1.20)and Na/K mole ratios(ranging from 0.58 to 2.56). The experimental results also showed that DCuwas positively correlated with the HCl concentration of the starting fluid.The DCuwas independent of the Si O_2 mole content in the range of Si O_2 content considered. No DCuvalue was less than 1 in our experiments at 850 °C and 100 MPa, indicating that Cu preferred to enter the fluid phase rather than the coexisting melt phase under most conditions in the melt-fluid system, and thus a significant amount of Cu could be transported in the fluid phase in the magmatichydrothermal environment. The results indicated that Cu favored partitioning into the aqueous fluid rather than themelt phase if there was a high Na/K ratio, Na-rich, peraluminous granitic melt coexisting with the high Cl-fluid. | Shuilong Wang Hui Li Linbo Shang Xianwu Bi Xinsong Wang Wenlin Fan | 2016 | Acta Geochimica2016，35，4： | 3 |
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