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91.
介绍了银河系中各种化学元素丰度随金属丰度的变化规律。结合恒星核合成理论,可以了解银河系的形成和演化过程。另外,某些化学元素丰度存在的弥散可能是恒星形成时银河系环境的不均匀性造成的。 相似文献
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Resulting from the rising levels of atmospheric carbon, ocean acidification has become a global problem. It has significant impacts on the development, survival, growth and physiology of marine organisms. Therefore, a highprecision sensor is urgently needed to measure the pH of sea-water. Iridium wire with a diameter of 0.25 mm is used as the substrate, and an Ir/Ir(OH)_x pH electrode is prepared by a one-step electrochemical method in a Li OH solution at the room temperature. A scanning electron microscope(SEM) observation reveals that it is coated with nanoscale particles. In laboratory tests, the electrode exhibits a very promising pH response, with an ideal Nernst slope(56.14–59.52), fast response, good stability and long life-span in tested pH buffer solutions. For a sea trial,four pH electrodes and one Ag/Ag Cl reference electrode are integrated with a self-made chemical sensor, and a profile detection of nearly 70 m is implemented near Newport Harbor, California on August 3, 2015. The results reflect that the pH value measured by the sensor is very close to the data given by Sea-Bird 911 plus CTD, with a difference value ranging from 0.000 075 to 0.064 719. And the sensor shows a better data matching degree in 0–40m water depth. In addition, the high precision and accuracy of the sensor make it possible to use in the ocean observation field. 相似文献
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Jingeng Sha Masaki Matsukawa Huawei Cai Baoyu Jiang Makoto Ito Chengquan He Zhiwei Gu 《Cretaceous Research》2003,24(6):715-728
In eastern Heilongjiang, the Upper Jurassic is marine and restricted to the Suibin and Dong’an areas, where it is characterized faunally by Callovian–Volgian (Tithonian) bivalves and florally by dinoflagellates. The Lower Cretaceous is widely distributed in eastern Heilongjiang, and characterized faunally by Berriasian–Valanginian bivalves, Barremian–Albian ammonites and Aucellina, and florally by dinoflagellates. To the west, the marine facies grade into non-marine beds. Thus, in the east, for example in the Dong’an and Dajiashan areas, near the northwestern Palaeo-Pacific, the Lower Cretaceous is marine; westward, in the Yunshan, Longzhaogou, Peide, and Zhushan areas, marine and non-marine deposits alternate, whereas further west still, e.g. in the Jixi Basin, non-marine facies are intercalated with marine beds. This regional distribution is indicative of a large, shallow embayment opening eastwards to the Palaeo-Pacific; during the Early Cretaceous successive transgressive-regressive events influenced the climate and biota of eastern Heilongjiang and northeastern China. Many of the Lower Cretaceous sections contain abundant coals, demonstrating that in this region the Early Cretaceous was an important coal-forming period. Some non-marine bivalve species are common to the Lower Cretaceous Jixi Group of eastern Heilongjiang, the Jehol Group of western Liaoning and the Transbaikalian Group of Siberia, suggesting that these groups are of comparable Early Cretaceous age. 相似文献
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燕山地区中生代花岗岩类侵入体中发育煌斑岩,呈脉状产于冀北寿王坟—五凤楼一带,岩石类型主要为云煌岩。岩石化学属基性,富钠,富碱,高Mg#,高钛,属高钛、钠质钙碱性煌斑岩。岩石中富集LREE、Ba等大离子亲石元素和P,亏损HREE和Nb、Zr、Ta等高场强元素,基本无Eu异常。其LA ICP MS锆石U Pb年龄为(1352±13) Ma, 侵位于早白垩世,与寿王坟杂岩体是同一时期岩浆活动的产物。五凤楼煌斑岩锆石εHf(t)值为-193~-133,模式年龄远老于其成岩年龄,表明岩浆起源于富集地幔。较高的Ba/Th值(12309~43634)和Sr值(9154×10-6~1 257×10-6),暗示源区在一定程度上受到了俯冲带流体的改造;较低的Rb/Sr值(002~011)及较高的Ba/Rb值(108~809)证明其源区含有角闪石。岩石地球化学特征显示,五凤楼煌斑岩由俯冲的古太平洋壳富钠流体交代形成的石榴石角闪二辉橄榄岩富集地幔的低程度(05%~15%)部分熔融上侵而成,起源深度为75~100 km。 相似文献
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通常情况下,随着地层压力降低,储层渗透率及流体性质的变化会导致气井产能方程随之发生变化。对于低渗透产水气藏,由于应力敏感、紊流效应、滑脱效应等非线性渗流效应及后期产水的影响,气井产能急剧降低。为了定量评价以上因素对气井产能的影响,基于常规二项式产能方程,建立了综合考虑地层压力变化、非线性渗流效应及产水对气井产能影响的产能方程。通过实例计算表明,由于应力敏感、紊流效应、滑脱效应等非线性渗流效应的综合影响,二项式系数A随地层压力的降低而减小,而系数B随地层压力的降低而增大;此外,由于后期产水影响,含水饱和度不断上升,气相相对渗透率随水气比的上升而减小,使二项式系数A、B均随水气比的上升而增大;因此,气井的产能下降幅度随地层压力下降呈线性升高趋势,随水气比下降呈对数降低趋势。该研究成果对于低渗透产水气井的产能预测及分析具有指导作用。 相似文献