生物化学综合性实验的探索与评价

以河北科技师范学院2005级生物科学、生物技术专业学生为样本,通过对生物化学综合性实验效果的调查,说明综合性实验在突出学生主体地位、激发学生兴趣等方面起到了积极的作用,能够在培养学生团队合作精神、科研能力等多方面综合能力的提升。     

美国高校师资的国际流动:流入与流出

教师是教学理念的具体实行者,高等教育的国际化必须首先实现高校师资队伍的国际化。无论在丰富自身的知识体系和专业经验方面,还是在开阔视野和提高专业素养方面,有众多的原因决定了必须大力推动高校师资的国际流动。美国在高校师资的国际流动方面有着丰富的经验,一方面通过客座教授项目、访问学者项目和教授交换项目吸引了大批国外优秀师资,另一方面通过教师带队出国留学项目、富布赖学者项目和教师交换项目鼓励本国师资走出国门,改善师资质量。     

汉语不赞同言语行为的调节策略

不赞同言语行为是威胁面子行为,其调节策略可以缓和其语力.基于Muntigl & Tumbill(1998)的不赞同言语行为的调节策略模式,试图总结归纳汉语不赞同言语行为的调节模式,以期深刻理解汉文化背景下的不赞同言语行为.     

创新性教育的基本特征与生理基础

激发学生的求知欲望,增强学生的创新意识,培养学生科学的学习、观察、抽象、思维、想象、综合、研究、实验等各种创新能力,是创造新性教育的基本特征;形成大脑细胞的优势兴奋中心,延长优势兴奋中心的时间,反复多次地、多形式地、定向地反复刺激大脑建立条件反射,产生科学灵感,是创新教育的生理基础。     

浅谈微博在尿沉渣形态学教学改革中的作用

伴随医学检验专业改制(五年学制改为四年制),教学学时也相应缩减,在此形势下,如何保持教学质量尤其是尿沉渣形态学教学质量成为目前教改的焦点。利用微博建立尿沉渣形态学线上教学互动平台就可解决这一问题,教改实践证明:这样不仅保持了教学质量,学生对形态学的学习兴趣也提高了。     

黄梅戏文化视域下语文课程的阅读教学研究

黄梅戏是中华民族戏曲艺术中一颗璀璨的明珠,本文试图结合黄梅戏文化知识探讨语文课程中的阅读教学,把戏曲文化中的文本、造型等深厚的戏曲素养融入语文教学,分析总结语文课程教学行之有效的方法,使语文教学与戏曲知识完美融合,展示艺术魅力,创新语文课程教学。     

Paving the road toward the use of β-Fe2O3 in solar water splitting: Raman identification,phase transformation and strategies for phase stabilization

Although β-Fe₂O₃ has a high theoretical solar-to-hydrogen efficiency because of its narrow band gap, the study of β-Fe₂O₃ photoanodes for water splitting is elusive as a result of their metastable nature. Raman identification of β-Fe₂O₃ is theoretically and experimentally investigated in this study for the first time, thus clarifying the debate about its Raman spectrum in the literature. Phase transformation of β-Fe₂O₃ to α-Fe₂O₃ was found to potentially take place under laser and electron irradiation as well as annealing. Herein, phase transformation of β-Fe₂O₃ to α-Fe₂O₃ was inhibited by introduction of Zr doping, and β-Fe₂O₃ was found to withstand a higher annealing temperature without any phase transformation. The solar water splitting photocurrent of the Zr-doped β-Fe₂O₃ photoanode was increased by 500% compared to that of the pure β-Fe₂O₃ photoanode. Additionally, Zr-doped β-Fe₂O₃ exhibited very good stability during the process of solar water splitting. These results indicate that by improving its thermal stability, metastable β-Fe₂O₃ film is a promising photoanode for solar water splitting.     

Olivine-norite rock detected by the lunar rover Yutu-2 likely crystallized from the SPA-impact melt pool

Chang’E-4 landed in the South Pole-Aitken (SPA) basin, providing a unique chance to probe the composition of the lunar interior. Its landing site is located on ejecta strips in Von Kármán crater that possibly originate from the neighboring Finsen crater. A surface rock and the lunar regolith at 10 sites along the rover Yutu-2 track were measured by the onboard Visible and Near-Infrared Imaging Spectrometer in the first three lunar days of mission operations. In situ spectra of the regolith have peak band positions at 1 and 2 μm, similar to the spectral data of Finsen ejecta from the Moon Mineralogy Mapper, which confirms that the regolith''s composition of the landing area is mostly similar to that of Finsen ejecta. The rock spectrum shows similar band peak positions, but stronger absorptions, suggesting relatively fresh exposure. The rock may consist of 38.1 ± 5.4% low-Ca pyroxene, 13.9 ± 5.1% olivine and 48.0 ± 3.1% plagioclase, referred to as olivine-norite. The plagioclase-abundant and olivine-poor modal composition of the rock is inconsistent with the origin of the mantle, but representative of the lunar lower crust. Alternatively, the rock crystallized from the impact-derived melt pool formed by the SPA-impact event via mixing the lunar crust and mantle materials. This scenario is consistent with fast-cooling thermal conditions of a shallow melt pool, indicated by the fine to medium-sized texture (<3 mm) of the rock and the SPA-impact melting model [Icarus 2012; 220: 730–43].     

1936—2018年环北极典型流域气温与降水时空变化

降水是环北极地区水资源的主要来源。定量分析气温与降水时空变化是深入理解环北极地区陆地水循环过程的基础。本文选取鄂毕河、叶尼塞河、勒拿河流域为对象,利用167个俄罗斯国家气象站点1936—2018年的气温与降水观测数据,结合线性趋势分析和Mann-Kendall突变点检验,揭示环北极典型流域气温与降水的时空变化特征。结果表明：①鄂毕河、叶尼塞河和勒拿河流域多年平均气温为0.06 ℃、-2.98 ℃、-7.41 ℃,年均增温速率分别为0.27 ℃/10 a,0.22 ℃/10 a,0.15 ℃/10 a。年内极端最低温（TNn）上升尤为明显,约为年均增温速率的1.3倍,春、冬季增温速率大于夏、秋两季;②鄂毕河、叶尼塞河和勒拿河流域多年平均降水量为496 mm、428 mm、369 mm;年降水量显著增加,其中叶尼塞河流域增速较慢（3.36 mm/10 a）,而鄂毕河（13.02 mm/10 a）和勒拿河（9.59 mm/10 a）流域增速较快,降水增加集中在春、秋、冬三季;③在空间上,增温较快的区域集中在西伯利亚高原和山地,最大增温速率达0.60 ℃/10 a,而平原地区普遍偏低;降水的空间差异大,西伯利亚南部高海拔地区（>1100 m）年降水量达1000 mm左右,北部低海拔地区普遍为300~ 600 mm。上述观测数据指示,环北极流域正在变暖变湿,且空间差异大,可能与“北极放大”及流域下垫面条件有关。