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示波极谱法测量电锌液中微量镍 总被引:1,自引:0,他引:1
提出在丁二酮肟-亚硝酸钠-氨水-氯化铵体系中,准确测定电锌液中微量镍的新方法:克服原子吸收光谱法测定微量镍回收率偏低问题。 相似文献
23.
全省上表铁矿111处,总储量32.16亿吨,其中有11.27亿吨暂不能使用.而且,富铁矿少,难选矿多,分布边远,难以满足经济发展需求.必须解决菱铁矿、高磷矿选矿问题,以及有远景磁异常补充深部找矿问题,可望取得突破. 相似文献
24.
江西大布铀矿床溶浸地质条件及溶浸方法研究 总被引:1,自引:1,他引:0
本文围绕溶浸采矿这个主题 ,从岩、矿石的物质成分 ;矿石结构构造 ;铀的存在形式 ;岩、矿石物理力学参数 ;矿体形态、产状、规模及矿床水文地质等诸多方面阐述了大布铀矿床溶浸的天然地质条件 ,并通过一系列矿石铀浸出工艺试验 ,获得大量溶浸工艺参数 ,提出大布铀矿床以原地破碎浸出辅以堆浸为最佳采矿方案。 相似文献
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François Farges 《Physics and Chemistry of Minerals》2009,36(8):463-481
Cr K-edge XANES spectra were obtained for a variety of Cr-bearing model compounds containing Cr(II), Cr(III), Cr(IV), Cr(V) and Cr(VI), in which the Cr-site symmetry is D4h, Oh and Td. The centroid position of the pre-edge feature is a better indicator of the Cr valence than the edge position. In Cr-rich oxides, higher-energy transitions must be excluded in order to refine a robust valence for Cr. The pre-edge for chromates is not unique and varies as a function of the CrO4 2? moiety distortion, which is often related to Cr-polymerization (monochromate vs. dichromate). Both the analogy with the Mn K-pre-edge information and ab initio FEFF calculations of the pre-edge feature for Cr(III) and Cr(VI) confirm the experimental trends. This methodology is applied to the Cr K-edge pre-edge feature collected in gems (emerald, spinel and ruby), the layered minerals fuchsite and kämmererite, two Cr-bearing aqueous solutions and a set of sodo-calcic silicate glasses used for bottling sparkling white wine. In emerald and fuchsite, the Cr-site is differently distorted than its ruby or spinel counterpart. In a Cr(III)-bearing aqueous solution and sodo-calcic glass, no evidence for Cr(III) with Td and C3v symmetry is detected. However, minor amounts of chromate moieties (most likely monomeric) are detected in a glass synthesized in air. Preliminary spectra for the wine bottle glass suggest that only trace amounts of chromates might possibly be present in these glasses. 相似文献
28.
柴达木盆地中深层混积岩储层形成机制 总被引:9,自引:1,他引:9
通过岩心观测、普通薄片、铸体薄片、扫描电镜、电子探针和岩石物性等分析,系统阐述了柴达木盆地典型中深层(西北区南翼山构造E32-N1)混积岩的岩石学、储集空间/物性和成岩作用等特征,在此基础上讨论了储层形成机制。结果表明,混积岩以(泥质)泥晶灰岩、钙质含量较高的砂岩和粉砂岩及其混积岩为主;储集空间以溶蚀改造的裂缝和粒间溶蚀孔隙为特征,物性总体表现为低孔-特低孔、超低渗-非渗透;有利于形成储层的成岩作用是溶蚀和构造裂缝作用;储层形成机制可归纳为"岩性是基础,裂缝是条件,溶蚀是关键"。这可为区域中深层混积岩储层,乃至陆相湖泊混合沉积储层的研究与油气勘探开发提供借鉴与参考。 相似文献
29.
卢伙胜 《广东海洋大学学报》1995,(2)
在假设手纲、空纲成直线状,浮纲、沉纲呈悬链线状的前提下,利用悬链线各因素与手纲冲角之间的相互制约关系,确立了计算单船底拖网作业手纲冲角近似值的逐步校正法。并推广应用于双船底拖网作业中的曳纲水平冲角、空纲的水平冲角、上袖端的内倾率、上片网衣在沉纲前上方的遮盖面积以及遮盖率等的近似值计算。 相似文献
30.
The halite-bearing Barbastro Formation crops out in the core of the Barbastro Anticline (Ebro Tertiary Basin). This anticline
is traversed perpendicularly by some of the most important Pyrenean drainages such as the Cinca and Noguera-Ribagorzana Rivers.
The terrace sequences of these fluvial systems have been used as markers to identify and assess dissolution-induced subsidence
and salt tectonics. In the limbs of the anticline, terrace deposits underlain by detrital bedrock do not show any evidence
of deformation and have a consistent thickness of less than 10 m. The deposits of certain terrace levels of the Noguera-Ribagorzana
River and its tributary, the Lo Reguer Creek, are locally thickened filling basins generated by dissolution-induced synsedimentary
subsidence up to several kilometers long and more than 100 m deep. Conversely, terraces of the Cinca River do not show anomalously
high thicknesses, but local uplifts related to differential upward flow of the halite-bearing bedrock. Locally, a minimum
uplift rate of 0.3 mm/year has been estimated from a 64-ka terrace tilted away from the valley. The subsidence hazards occur
chiefly in areas where the ground receives artificial water recharge. Serviceability of some canals has been notoriously affected
by evaporite karstification. The problem has been mitigated to acceptable levels by grouting. Numerous buildings of Ivars
de Noguera are severely damaged by dissolution subsidence, and possibly, by hydrocompaction of gypsiferous silts. The pipe
network has been replaced to ameliorate the subsidence risk. In the Cinca River valley, cavities with a total volume of about
180,500 m3 have been created by solution mining at depths greater than 500 m. No investigation methods are applied in the brine field
to monitor the distribution and evolution of artificial voids. Substantial increase in salinity of the Cinca River is another
evidence of subjacent evaporite dissolution. 相似文献