吉林省磐石市小红石砬子铅锌块状硫化物矿床的特征及意义

磐石市小红石砬子银铅锌多金属矿区处在磐石—永吉—双阳海西期花岗岩与石炭系碳酸岩建造的外接触带,产在中生代北西向线性火山断陷盆地内,位于海西晚期近圆形的火山穹隆构造南东部,属于块状硫化物型银铅锌多金属矿床;通过对该矿床地质特征的描述,区域分布规律及其成矿机理的探讨,为吉中地区寻找类似矿床打开了思路。     

2,5-二(4-氨基苯基)-1,3,4-噁二唑合成方法的优化

建立了一种2,5-二(4-氨基苯基)-1,3,4-噁二唑的最佳合成方法。以对硝基苯甲酸和盐酸氨基脲为原料,多聚磷酸为脱水剂,150~160℃的条件下反应2h,高收率(89%)制得中间体2,5-二(4-硝基苯基)-1,3,4-噁二唑;然后在DMF溶剂中以Na2S为还原剂,于100℃的条件下反应4h,中间体还原得到目标产物2,5-二(4-氨基苯基)-1,3,4噁二唑。此反应具有时间短、收率高且后处理简单、产物容易提纯等优点。     

粉煤灰脱硅液FeSx-CuS共沉淀法深度除铁实验

粉煤灰碱法提取氧化铝中间产物——粉煤灰脱硅液中含有较高含量的Fe元素,严重制约了脱硅液在超白玻璃生产等对Fe含量有严格限制的领域的应用。研究采用FeS_x-CuS共沉淀法对粉煤灰脱硅液进行了深度除铁处理。以硫化钠为絮凝剂、以硫酸铜为助凝剂,通过实验研究了二者用量及配方比对Fe离子的沉降、脱除效果。实验结果显示,粉煤灰脱硅液投加硫化钠于65~70℃下絮凝反应5 min,后降温至45℃,加入五水硫酸铜保温反应30 min助凝,最后静置24 h,可将脱硅液中Fe元素进行有效脱除。硫化钠添加量为Fe_2O_3摩尔质量的300倍;且硫化钠与硫酸铜的最佳摩尔质量配比为3∶2时,粉煤灰脱硅液中Fe_2O_3含量被降至最低检出限以下,同时Cu离子残留亦最低,有利于超白玻璃等生产。     

Effect of H2S concentration on the corrosion behavior of pipeline steel under the coexistence of H2S and CO2

The effect of H2S concentration on H2S/CO2 corrosion of API-X60 steel was studied by scanning electron microscopy, a weight-loss method, potentiodynamic polarization tests, and the electrochemical impedance spectroscopy technique. It is found that the cor-rosion process of the steel in an environment where H2S and CO2 coexist at different H2S concentrations is related to the morphological structure and stability of the corrosion product film. With the addition of a small amount of H2S, the size of the anode reaction region is de-creased due to constant adsorption and separation of more FeS sediment or more FeHS＋ions on the surface of the steel. Meanwhile, the dou-ble-layer capacitance is diminished with increasing anion adsorption capacity. Therefore, the corrosion process is inhibited. The general cor-rosion rate of the steel rapidly decreases after the addition of a small amount of H2S under the coexistence of H2S and CO2. With a further increase in H2S concentration, certain parts of the corrosion product film become loose and even fall off. Thus, the protection provided by the corrosion product film worsens, and the corrosion rate tends to increase.     

洱海水硫化物及六价铬含量的检测分析

目的:了解洱海水硫化物及六价铬含量。方法:采集洱海20个点的水样对硫化物及六价铬的含量进行检测,分别采用亚甲蓝分光光度法,二苯碳酰二肼分光光度法进行测定。结果按照《地表水环境质量标准进行评价》。结果:硫化物、六价铬合格率为100%。结论:硫化物、六价铬均达到GB 3838-2002《地表水环境质量标准》的一类水质。     

厌氧条件下硫酸盐废水中硫化物生成的影响因素

采用实验室模拟废水进行实验,研究了硫酸盐转化为硫化物的条件,包括厌氧环境中有菌和无菌情况下硫酸盐（SO42-）的浓度,反应时间,pH和温度对转化结果的影响,以出水硫化物的生成量为测定指标.得出结论：废水中硫酸盐含量为1 500 mg·L-1,时间36 h,pH介于6.8～7.0,温度在30～35℃之间,硫酸盐还原菌（Sulfate reducing bacteria,SRB）的生长活性较高,硫化物的生成量最大,为14.6 mg·L-1.     

青海祁连郭米寺-尕大坂铜多金属矿成矿地质特征和成矿模式探讨

青海祁连郭米寺-尕大坂铜多金属矿位于北祁连成矿带走廊南山成矿亚带.矿区主要出露中寒武统,其次为上石炭统及白垩系.含矿蚀变带长2500m,宽20~150m,最宽155m,向北西逐渐尖灭,向南东被白垩系巨厚红层和石炭系煤系层掩盖,已发现长800m,宽20~155m的含矿带.矿床成矿类型为典型的与海相中酸性火山活动有关的块状硫化物矿床(白银厂式矿床).     

Electrochemical and spectroscopic study of interfacial interactions between chalcopyrite and typical flotation process reagents

Comparative voltammetry and differential double-layer capacitance studies were performed to evaluate interfacial interactions between chalcopyrite (CuFeS₂) and n-isopropyl xanthate (X) in the presence of ammonium bisulfite/39wt% SO₂ and caustic starch at different pH values. Raman spectroscopy, Fourier transform infrared (FTIR) spectroscopy, contact angle measurements, and microflotation tests were used to establish the type and extent of xanthate adsorption as well as the species involved under different mineral surface conditions in this study. The results demonstrate that the species that favor a greater hydrophobicity of chalcopyrite are primarily CuX and S0, whereas oxides and hydroxides of Cu and Fe as well as an excess of starch decrease the hydrophobicity. A conditioning of the mineral surface with ammonium bisulfite/39wt% SO₂ at pH 6 promotes the activation of surface and enhances the xanthate adsorption. However, this effect is diminished at pH ≥ 8, when an excess of starch is added during the preconditioning step.     

聚苯硫醚交联反应机理的量子化学计算研究

用量子化学从头计算方法,利用静态理论对聚苯硫醚（ＰＰＳ）的交联机理进行了研究,通过对ＰＰＳ分子模型和可能产生的自由基模型的量子化学计算,探讨了ＰＰＳ的热交联反应趋势和交联结构,证实了氧在交联中所起的重要作用。     

大牛地奥陶系马五段硫化氢腐蚀机理与影响因素

为了解决大牛地气田硫化氢腐蚀严重问题,分析了硫化氢腐蚀机理以及影响腐蚀程度的因素。结合大牛地奥陶系马家沟组马五段地质条件以及硫化氢赋存条件确定该区域硫化氢形成的机理,为硫酸盐热化学还原反应;且该区域存在的大量石膏层为含硫化氢气体提供了良好的圈闭条件。硫化氢腐蚀模拟试验模拟了马五段地层水环境对N80钢和P110钢的腐蚀程度,P110钢的腐蚀程度较N80钢轻微,两者均属于极严重腐蚀。结合腐蚀表面微观形貌观测与腐蚀产物能谱分析得出:大牛地奥陶系马家沟组马五段硫化氢腐蚀机理为高温高压下CO2/H2S电化学腐蚀为主;并伴随有高Cl-破坏腐蚀产物膜加速腐蚀。硫化氢腐蚀影响因素分析得出温度和CO2含量增加会加速硫化氢腐蚀。