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核聚变与等离子体物理 1992年第4期12卷 218-225页

作者：邓柏权谢中友施汉文 h.h.abou-gabal G.A.Emmert 核工业西南物理研究院 University of Alexandria Egypt University of Wisconsin U.S.A

本文用Monte Carlo方法模拟了偏滤器扁平抽气收集板附近区域的氦原子输运。考虑了氦原子被电子碰撞电离,氦原子与等离子体离子之间的弹性散射等原子过程以及离子的热运动和沿磁力线的流动。计算表明当偏滤器等离子体密度在7cm距离内从... 详细信息

本文用Monte Carlo方法模拟了偏滤器扁平抽气收集板附近区域的氦原子输运。考虑了氦原子被电子碰撞电离,氦原子与等离子体离子之间的弹性散射等原子过程以及离子的热运动和沿磁力线的流动。计算表明当偏滤器等离子体密度在7cm距离内从里向靶板逐渐增加约4.7倍,而温度分布保持不变时,氦灰返回靶板的几率比密度在7cm内向靶板递减4.7倍的通常正分布提高约45％。磁力线与靶板的交角、靶板的温度,边缘等离子体鞘层电位以及不同的靶材料对氦返回靶板几率的影响作了比较。得到的结果对托卡马克聚变裂变增殖堆孔栏和偏滤器工程设计有参考价值。

关键词：氦输运偏滤器蒙特卡洛模拟

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Geology and geochemistry of the granitic rocks and associated dykes,East gabal Nuqra,South Eastern Desert,Egypt

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Chinese Journal Of Geochemistry 2012年第4期31卷 376-389页

作者： Ibrahim h.Ibrahim Mostafa E.Darwish Nuclear Material Authority 530 P.O.El MaadiCairoEgypt

A crescent-shape granitic stock and associated dykes is located to the East gabal Nuqra at the extreme western part of Wadi Natash,South Eastern Desert,*** examined granites are classified as alkali-feldspar granites and mainly consist of quartz,potash feldspars,plagioclases,and ***,zircon,apatite and allanite are accessories representing the source of Y,U,Th and REEs in these *** granites are characterized by high K2O,Na2O and Zn contents and Rb/Sr ***,they are highly enriched in high field strength elements(hFSE),especially Zr(1529×10-6),Nb(100×10-6),hf(91×10-6) and Y(624×10-6) and light rare-earth elements(LREE,141×10-6) concentrations and strongly depleted in Ca,Mg,Sr and Eu *** features suggest that they are similar to A-type granites(type-2).The rhyolite dykes and granites have similar geochemical characteristics whereas the chondrite-normalized REE patterns show a LREE enriched feature with strong negative Eu-anomaly,whereas the REE pattern of trachydacites show slightly fractionated pattern with no *** is suggested that the trachydacites were generated by small degree of partial-melting deep-seated basic *** liquid,when subjected to fractional crystallization involving separation of plagioclases as residue,generated the alkali-feldspar *** further fractional crystallization gave rise to the alkali *** igneous rock suite originated from metaluminous to alkaline trachytic magma,and was developed in a within-plate tectonic *** extension caused by NW-SE right-lateral shear in area led to the emplacement of the alkali-feldspar *** later extrusion of the alkali rhyolite and trachydacite dykes was due to cauldron subsidence.

关键词：碱长花岗岩地球化学特征堤坝沙漠埃及轻稀土元素碱性流纹岩元素富集特征

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Potash Breakdown of Poly-Mineralized Niobium-Tantalum-Lanthanides Ore Material

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American Journal of Analytical Chemistry 2019年第3期10卷 103-111页

作者： Mona N. El hazek Nawal h. Mohamed Azza A. Gabr Chemistry Department Faculty of Science Jazan University Jizan Saudi Arabia Nuclear Materials Authority Cairo Egypt Desert Research Center Cairo Egypt Chemistry Department Faculty of Science Aswan University Aswan Egypt

The potentiality of the alkali breakdown of the poly mineralized ore material south gabal El-A’urf area, central Eastern Desert, Egypt is investigated. It includes the multiple oxide mineral tanteuxenite, monazite, bastnasite, anatase, as well as zircon. This ore material assaying lanthanides (RE2O3 1.9%), niobium (Nb2O5 1.25%) as well as titanium and zirconium (TiO2 and ZrO2 1.23% and 1.12%) respectively besides tantalum (Ta2O5 0.13%), were used for the present work. This sample has thus been subjected to two alkali breakdown techniques using potash;namely agitation leaching and fusion. The latter technique was found to be preferred as it gives higher leaching efficiency. The optimum leaching conditions are weight ratio of the ore/potassium hydroxide 1/2 at 400°C for 1 h. The realized leaching efficiencies attained 95.0% and 93.7% for Nb and Ta respectively as well as 96% for lanthanides and 75% for Ti while that for Zr did not exceed 10%.

关键词： Lkali Fusion Agitation Leaching Niobium-Tantalum-Lanthanides Ores Polymineralized Ore Material

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