纤维质燃料水平填充床反向阴燃传播特性研究

基于两步反应动力学机理(包括燃料热解和燃料的氧化),建立了二维非稳态燃料填充床阴燃的数学模型.该模型既考虑了固相和气相之间的热传递,也考虑到了气体在多孔介质内扩散系数的变化.辐射换热采用扩散近似方式予以表达.数值模拟结果表明:阴燃传播速度随着来流速度的增大而增大,但当来流速度超过0.35 cm/s时,阴燃速度增长幅度大大减小;来流速度对阴燃最高温度影响不大.同时还模拟了燃料阴燃过程中气体组分(O2、CO、CO2及H2O)和固体成分(燃料、焦炭)的变化以及温度分布情况.图8,表2,参12.     

超滤分离纯化麦胚蛋白酶解物的研究

采用超滤法从麦胚蛋白酶解物中初步分离纯化抗氧化活性肽,考察了操作压力、操作温度及料液浓度等工艺参数对超滤过程中膜通量的影响,并对超滤前后麦胚蛋白酶解物的相对分子质量分布、氨基酸组成及抗氧化活性进行了比较.结果表明:采用截留相对分子质量3000的聚砜膜对麦胚蛋白酶解物进行超滤分离的最适工艺条件为操作压力0.30 MPa、操作温度20 ℃、麦胚蛋白酶解物浓度35 g/L;超滤有效地除去了料液中相对分子质量较大的组分,麦胚蛋白酶解物中相对分子质量1 000～500及500～130的组分分别为23.81%、48.63%,其抗氧化活性得到提高,清除O2-·的IC50由超滤前的1.64 mg·mL-1降至超滤后的1.29 mg·mL-1.图5,表3,参13.     

鳟鱼海水网箱养成及相关技术的初步研究

在鳟鱼网箱养成及长途运输、海水驯化等专项研究的基础上,分别对鳟鱼海水养成及相关技术进行了研讨,提出了鳟鱼海水养成的关键技术和影响鳟鱼长途运输及海水驯化的主要因素,为开发鳟鱼海水驯养提供实用参考。     

南海北部大陆架海洋生态系统Ecopath模型的应用与分析

过度捕捞和环境恶化导致渔业资源和海洋生态系统逆向发展。采用EwE5.1软件,对南海北部大陆架建立Ecopath(生态通道模型)模型。通过各级流量、生物量、生产量、捕捞量、系统总流量以及生态位和混和营养效应等方面的分析,得出营养流通主要有2种途径,肉食鱼类间饵料竞争非常激烈,低值鱼类间具相似的捕食压力,顶级捕食者对大部分鱼类负效应不明显。系统受过度捕捞渔业影响很大,并存在营养级I利用效率低和渔业资源小型化、低值化等不稳定的幼态特征。     

养殖俄罗斯鲟性腺发育及人工繁殖

在繁殖季节通过肉眼观察和组织切片对池塘养殖7龄的俄罗斯鲟(Acipenser gueldenstaedti)性腺发育进行分析,发现雌性个体间性腺发育差异较大(n=500)。其中73%卵巢中可以看到白色卵粒,卵径小于1.0mm;有16%卵巢达到Ⅲ期,卵粒已经着色;有9%卵巢发育到IV期早期,卵径平均为2.6±0.2 mm;还有2%卵巢中肉眼看不到卵粒,组织学观察属于I期卵巢。雄性俄罗斯鲟全部达到性成熟,有部分成熟好的可以挤出精液。激素催产2尾八龄和6尾九龄的雌性俄罗斯鲟,其中7尾催产成功;剖腹手术收集游离卵7.2 kg,催产后的雄鱼全部排精。     

C语言函数调用过程中变量的同名问题的解决

通过C语言函数调用过程中参数传递问题的讨论,进而引出了变量的同名问题,并分别从实参与形参、存储空间分配、复合语句、外部变量与内部变量四个方面深入剖析了程序执行时,同名变量引用的规则和方法的全过程。     

小学数学教学培养学生创新思维的几条途径

在小学数学教学中培养学生的创新思维,可把握以下几条途径：一,营造和谐的教学氛围;二、强化熟练的操作能力;三、巧用知识的迁移原理;四、立足不同的解题视角。     

Benthic foraminiferal fauna turnover at 2.1 Ma in the northern South China Sea

Quantitative analysis of benthic foraminifera from ODP Site 1146 in the northern South China Sea (SCS) shows that abundance of Bulimina alazanensis, sometimes up to about 90%, decreased gradually since 3.2 Ma, especially at 2.1 Ma. Abundance of other benthic foraminiferal species, Globobulimina sub-globosa and Cibicidoides wuellerstorfi, increased after 2.1 Ma. Comparison with changes in oxygen and carbon isotopes of planktonic and benthic foraminifera shows that high abundance values of B. alazanensis corresponded with lower values of oxygen isotope, but for carbon isotope, high values of the species were consistent with heavier carbon isotope of benthic foraminifera and lighter carbon isotope of planktonic foraminifera, respectively, and vice versa. Considering factors such as uplift of Bashi Strait, expansion of the North Hemisphere Glaciation, strengthening of East Asian winter mon-soon and variations in oxygen and carbon isotope of foraminifera, changes of B. alazanensis in ODP Site 1146 suggest that the source of deep water masses of the northern South China Sea changed from the warm Pacific deep water with high oxygen content to Pacific Intermediate water with low oxygen content at 2.1 Ma. In addition, the strengthened East Asian winter monsoon resulted in increased pri-mary productivity, high nutrient and suboxic bottom water. Variations in species of B. alazanensis seemed to be unable to tolerate environmental stress induced by deep water masses and productivity changes.     

Clay minerals in surface sediments of the Pearl River drainage basin and their contribution to the South China Sea

Clay minerals have played a significant role in the study of the East Asian monsoon evolution in the South China Sea by being able to track oceanic current variations and to reveal contemporaneous paleoclimaUc changes prevailing in continental source areas. As one of the most important rivers inputting terrigenous matters to the northern South China Sea, the Pearl River was not previously paid attention to from the viewpoint of clay mineralogy. This paper presents a detailed study on clay minerals in surface sediments collected from the Pearl River drainage basin （including all three main channels, various branches, and the Lingdingyang in the estuary） by using the X-ray diffraction （XRD） method. The results indicate that the clay mineral assemblage consists dominantly of kaolinite （35%-65%）, lesser abundance of chlorite （20%-35%） and illite （12%-42%）, and very scare smectite occurrences （generally 〈5%）. Their respective distribution does not present any obvious difference throughout the Pearl River drainage basin. However, downstream the Pearl River to the northern South China Sea, the clay mineral assemblage varies significantly： kaolinite decreases gradually, smecUte and illite increase gradually. Additionally, illite chemistry index steps down and illite crystallinity steps up. These variations indicate the contribution of major kaolinite, lesser illite and chlorite, and very scarce smecUte to the northern South China Sea from the Pearl River drainage basin. The maximum contribution of clay minerals from the Pearl River is 72% to the northern margin and only 15% to the northern slope of the South China Sea. In both glacials and interglacials, kaolinite indicates that the ability of mechanical erosion occurred in the Pearl River drainage basin.     

Coupling and propagating of mesoscale sea level variability between the western Pacific and the South China Sea

The coupling and propagating features of mesoscale sea level variability between the western Pacific (WP) and the South China Sea (SCS) were studied based on time series analyses of satellite altimeter measured, along-track sea surface height anomalies (SSHA) along 21°N and the slope of the northern SCS. The analyses show that mesoscale sea level fluctuations in the WP have rather limited coherent effects on the SCS, and no statistically significant propagation of mesoscale variability through the Luzon Strait was observed except in the 45-day band. Evidence suggests that the 45-day fluctuation is very much likely a character of the Kuroshio originating from its low-latitude beginning. It is also sug- gested that the westward propagating Rossby waves will deform when they encounter the dynamical barrier of the Kuroshio. The Kuroshio will then acts on the SCS in its own way. The SCS is a relatively isolated system in the sense of coupling and propagating of oceanic mesoscale waves.