138 resultados para 616.865
Resumo:
The species composition and abundance of microzooplankton at 10 marine and five coastal stations (Hongdao, Daguhe, Haibohe, Huangdao and Hangxiao) in the Jiaozhou Bay (Qingdao, China) were studied in 2001. The microzooplankton community was found to be dominated by Tintinnopsis beroidea, Tintinnopsis urnula, Tintinnopsis brevicollis and Cvdonellopsis sp. The average abundance of microzooplankton was highly variable among stations. Specifically, the abundance of microzooplankton was higher at inshore stations and lower in the center of the bay (St. 5), bay mouth (St. 9) and outside the bay (St. 10). The highest average annual densities (346 ind./L) was observed at St. 3, while the lowest (55 ind./L) was at St. 10. Two abundance peaks were recorded in May (324 ind./L) and February (300 ind./L). The distribution of microzooplankton in three sampling layers at the 10 stations was relatively homogenous and the abundance decreased slightly as the water depth increased. At coastal stations, the highest average annual density was recorded at Hongdao Station (677 ind./L), followed by Daguhe Station (616 ind./L), Haibohe Station (400 ind./L), Huangdao Station (275 ind./L) and Hangxiao Station (73 ind./L). Furthermore, a 24-h sampling analysis conducted at Hangxiao Station revealed that the microzooplankton assemblages were characterized by a bimodal diel vertical migration pattern, with the highest densities occurring at dusk (154 ind./L), followed by dawn (146 ind./L), noon (93 ind./L) and midnight (77 ind./L). The density of microzooplankton in the Jiaozhou Bay was in the middle range of the densities of temperate coastal waters worldwide.
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Quantum chemical calculations based on DFT method were performed on three polydentate Schiff base compounds (PSCs) used as corrosion inhibitors for iron in acid media to determine the relationship between the molecular structure of PSC and inhibition efficiency. The structural parameters, such as the frontier molecular orbital energy HOMO (highest occupied molecular orbital) and LUMO (lowest unoccupied molecular orbital), the charge distribution of the studied inhibitors, the absolute electronegativity (chi) values, and the fraction of electrons (Delta N) transfer from inhibitors to iron, were also calculated and correlated with inhibition efficiencies. The results showed that the inhibition efficiency of PSCs increased with the increase in E-HOMO and decrease in E-LUMO-E-HOMO; and the areas containing N atoms are most possible sites for bonding the metal iron surface by donating electrons to the metal. (C) 2007 Elsevier Ltd. All rights reserved.
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The application of hot-dipped zinc and zinc-aluminum alloy coatings were introduced. Exposure tests of the steels with these coatings were conducted in the offshore atmosphere in Qingdao and Xiamen for 12 years separately. Effects of the coating thickness, alloy composition and atmospheric environment on the corrosion performance were studied. Results of the onsite exposure tests were compared with the results of a previous indoor salt spray accelerated corrosion tests. The study supports that zinc-aluminum alloy coatings are useful in providing better corrosion resistance and can be further developed for future applications.
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Six compounds were isolated from the 75% ethanol extract of Nitraria tangutorum seed.On the basis of spectroscopic methods including 1H NMR,13C NMR and ESI-MS and comparison with literature,their structures were elucidated as daucosterol(1),4-hydroxypipecolic acid(2),quercetin(3),allantoin(4),1,2,3,4-tetrahydro-1-methyl-β-carboline-3-carboxylic acid(5) and L-tyrosine(6).Compounds 1,2,3,5 and 6 were isolated from Nitraria tangtorum for the first time.
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本文对珠芽蓼果实的营养成分进行了分析.结果表明,珠芽蓼果实含有丰富的蛋白质、总糖、氨基酸和矿质元素,是一种值得有效开发的野生植物资源.
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根据天然草地退化程度的差异,采用松耙+补播+施肥+封育(退化较严重的草地)、封育+施肥(轻度退化草地)等措施,植物群落物种组成、多样性等特征值及其植被盖度发生明显变化.研究第2年结果表明,物种数封育+施肥处理最高(32种),对照居中(26种),补播+施肥处理最低(13种);多样性指数大小依次为封育+施肥(3.126)、对照(2.819)、补播+施肥(1.494);均匀度指数大小依次为封育+施肥(0.902)、对照(0.865)、补播+施肥(0.582);群落总盖度大小依次为封育+施肥(85.9%)、补播+施肥(79.7%)、对照(72.9%);补播+施肥+封育处理后地上生物量最大(460.65 g/m2),原生植被+封育+施肥处理居中(310.14 g/m2),对照最低(178.96 g/m2);地下生物量大小依次为封育+施肥(6 920.37 g/m2)、补播+施肥(1 458.96 g/m2)、对照(828.91 g/m2);补播+施肥+封育处理优良牧草较对照提高近50倍,杂草类减少82.81%,封育+施肥处理较对照良牧草比例提高48倍,杂草类比例减少80.46%.半人工草地通过灭除杂草和施肥相结合的示范试验表明:单纯进行灭杂,地上生物量减少,灭杂和施肥相结合不仅可提高地上生物量,而且可提高优良牧草的比例;不同处理区土壤养分含量各不相同,其中封育+施肥处理全氮、全碳、有机碳最高,对照居中,补播+施肥较低.
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研究细穗香薷(Elsholtzia ianthina)的挥发油成分.采用水蒸气蒸馏法提取,用气相色谱质谱联用技术进行分析,用面积归一法计算出有关的相对含量,鉴定出45个化合物,主要的挥发油化学成分为三环[4.3.1.13,8]十一烷-1-醇,2,3,5,6-四甲基酚,共占挥发油总量的56.29%.
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系统报道了中藏药款冬大小孢子的发生、雌雄配子体发育和胚胎的发育过程。药壁发育双子叶型; 绒毡层发育接近菊科中的“The Com os bip innatus”型; 成熟花粉为3 细胞型; 单珠被, 薄珠心, 倒生胚珠;具发达的珠被绒毡层;胚囊发育4 孢子型, 接近五福花(A d ox a)型胚囊。受精作用属于有丝分裂前配子体融合类型。胚乳发育为核型。胚胎发育为紫菀型千里光变型。讨论了该种胚胎学特征的生态学及系统学意义。
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利用动力学通量箱法与高时间分辨率大气测汞仪的联用技术, 在瑞典西南的Kristineberg海洋观测站(KMRS)和Knobesholm的Hovgårdsån河分别测定了夏季海水和河水表面与大气间汞的交换通量. 在夏季, 河水和海水都是大气汞的源. 河水和海水表面与大气间汞的交换通量在夏季具有一致的昼夜变化规律, 白天由水体向大气排汞且在正午达到最大值; 夜间排汞量相对较小且有时会出现大气汞向水体沉降. 河水与大气间汞的交换通量与光照强度呈线性正相关关系, 与大气相对湿度呈线性负相关性, 同时还与水体温度存在指数相关性. 海水与大气间汞交换通量只与光照强度存在良好的线性正相关关系. 水体中溶解态气汞的过饱和是水体汞向大气释放的驱动力.
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白云鄂博Fe-Nb-REE矿床是世界上最大的REE矿床,前人已做过大量的研究工作.该矿床成因一直是中外地质学家争论的焦点,曾先后出现过多种成因观点,而赋矿白云岩(H6~H8)的成因则是争论的核心问题,水成/火成、同生/后生的争论.
Resumo:
秦岭造山带是华北与扬子两大古板块的接合带,在空间上,自北而南,秦岭造山带可分为华北板块南缘(华熊地块)、北秦岭造山带、南秦岭造山带和扬子板块北缘等4个构造单元。小秦岭金矿田位于华熊地块北缘,是国内外学者共识的造山型金矿田,河南灵宝大湖金-钼矿床位于小秦岭金矿田,属断控脉状矿床。大湖金-钼矿床最先正是以金矿床进行勘查的,其黄金储量28t,平均品位8.7g/t。随着开采深度的加大,部分含金石英脉向深部转变为辉钼矿-石英脉,目前探明钼资源量已达中型规模。 本论文主要从区域地质背景、矿床地质特征、元素地球化学、同位素地球化学、流体包裹体地球化学、矿床年代学及成矿机理等角度对大湖金-钼矿床进行了较为系统的研究,主要获得如下认识: 成矿过程经历3个阶段:早阶段为黄铁矿-石英脉,遭受变形、破碎,应形成于挤压或压剪过程;中阶段为细粒的辉钼矿-黄铁矿-石英网脉,贯入到早阶段黄铁矿或石英矿物的裂隙(可呈共轭状),应形成于剪切环境;晚阶段石英-碳酸盐细脉具梳状构造,充填于张性或张扭性裂隙。 大湖金-钼矿床的金属硫化物ISr=0.70470-0.71312,平均0.70854;(143Nd/144Nd)i=0.51143-0.51215,平均0.51162;(206Pb/204Pb)i=17.033-17.285,(207Pb/204Pb)i=15.358-15.438,(208Pb/204Pb)i = 37.307-37.582。其围岩太华群样品平均值ISr=0.72294,(143Nd/144Nd)i=0.51107,(206Pb/204Pb)i=17.127-18.392,(207Pb/204Pb)i =15.416-15.604,(208Pb/204Pb)i=37.498-37.814,它们的平均值分别是17.547,15.470,37.616。通过金属硫化物及围岩太华群的对比,可以看出,成矿物质具有太华群和深部地幔混合的特征。 通过对不同阶段的含矿石英脉中的流体包裹体特征研究表明,早阶段只发育CO2-H2O型流体包裹体;中阶段流体包裹体类型复杂,有纯CO2型、CO2-H2O型、H2O-NaCl型和含子晶包裹体,指示流体沸腾作用强烈;而晚阶段只发育水溶液包裹体。早、中、晚3个阶段的流体包裹体均一温度分别集中在400-500℃、290-470℃、220-260℃;估计的早、中阶段流体的最低捕获压力分别为138-331MPa和78-237MPa,对应于成矿深度分别为13.8-11.0km和7.8-8.0km。早、中阶段的压力反应出静岩压力到静水压力的转变。成矿温度和压力明显高于浅部含金石英脉的成矿温度120-310℃,成矿压力100-150MPa。与野外观察到的“上金下钼”的空间关系一致。 大湖金-钼矿床辉钼矿-石英脉Re-Os同位素模式年龄较集中,介于215.4±5.4-255.6±9.6Ma,Re-0s等时线年龄为218±41Ma(MSWD=38,2σ误差),表明大湖金-钼矿的辉矿化形成于印支期。 三叠纪末,随着古秦岭洋的逐渐封闭,处在弧后转换带的深部岩石在挤压作用下发生变质脱水而形成初始成矿流体,成矿流体沿断裂带(韧性剪切带)向上迁移而引起大湖钼矿床成矿系统的发育。随着区域构造环境由挤压转为伸展,区域的变质脱水更强,形成大量成矿流体,变质流体上侵为浅层流体循环提供了的热能,而浅层构造也因减压扩容而为流体循环提供了通道,这无疑有利于浅层流体循环和混入成矿系统。同时,增温和减压也有利于成矿流体发生沸腾。因此,充足的流体、热以及强烈的流体沸腾等,势必导致发生最为强烈的成矿物质快速沉淀作用。随着挤压作用的减弱,伸展作用的增强,区域热异常消失,地壳深部组分发生亏损,流体以浅源大气降水占主导,成矿作用迅速衰竭,形成石英-碳酸盐网脉,对成矿作用贡献减弱。总之,通过对大湖金钼矿床研究表明,大湖金钼矿床形成于由挤压转向伸展的构造背景,这与矿床地质的特征一致。
Resumo:
A novel mode of capillary electrochromatography (CEC), called dynamically modified strong cation-exchange CEC (DMSCX-CEC), is described in this paper. A column packed with a strong cation-exchange (SCX) packing material was dynamically modified with a long-chain quaternary ammonium salt, cetyltrimethylammonium bromide (CTAB), which was added to the mobile phase. CTAB ions were adsorbed onto the surface of the SCX packing material, and the resulting hydrophobic layer on this packing was used as the stationary phase. Using the dynamically modified SCX column, neutral solutes were separated with the CEC mode. The highest number of theoretical plates obtained was about 190 000/m, and the relative standard deviations (RSD's) for migration times and capacity factors of alkylbenzenes were less than 1.0% and 2.0% for five consecutive runs, respectively. The effects of CTAB and methanol concentrations and the pH value of the mobile phase on the electroosmotic flow and the separation mechanism were investigated. Excellent simultaneous separation of the basic and neutral solutes in DMSCX-CEC with a high-pH mobile phase was obtained, A mixture containing the acidic, basic, and neutral compounds was well separated in this mode with a low-pH mobile phase; however, peak tailing for basic compounds was observed in this mobile phase.