马脾铁蛋白铁核表层磷铁组成稳定性

马脾铁蛋白络合Ｆｅ２＋的能力与它的铁核表层磷酸盐和Ｆｅ３＋组成含量有关．ＯＨ－参与铁核表层组成，并迫使铁蛋白释放Ｆｅ３＋．用强还原剂还原铁核表层时，铁蛋白只能释放磷酸盐．在Ｆｅ２＋、磷酸盐和氧化剂存在下，铁蛋白能贮存原铁核总磷酸盐量的６０％的磷．     

STUDY ON THE PERMEABILITY OF MICROCAPSULES

In the present study,microcapsules with disperse dye solutions and a direct dye solution ascore materials were prepared by the complex coaeervation method and the interfacialpolycondensation method respectively.Experiments and theoretical analysis showed that there wasan exponential relationship between the diffusion time and the release rate of the core material intothe surrounding medium.A concise equation to calculate the permeability constant was derivedand verified by the experimental results.By means of duplex focus on the inner and outer diametersof a microcapsule,the average wall thickness of microcapsules was measured.     

室内实验规模的出砂数学模拟

为了研究疏松砂岩的出砂特征,根据连续性孔隙介质渗流、微粒释放和微粒运移理论,建立了室内实验规模的出砂数学模型,并采用有限差分法对该模型进行了求解。结果表明,实验条件下数学模拟与物理实验模拟的结果吻合较好。用理论出砂模型模拟了胶体力、水动力导致的出砂和砂粒运移过程中滞留引起的渗透率变化。模拟结果表明,渗流速度高于临界流速才引起冲刷出砂;胶体力和冲刷力是出砂的诱发因素,砂微粒在运移过程中在孔隙表面再沉积和孔喉处被捕集将降低出砂程度;渗透率比值与注水孔隙体积倍数或渗流速度的关系曲线均呈"S"形;在运移过程中,砂微粒滞留导致渗透率比值随岩心长度的变化呈线性降低趋势。     

新疆若羌县赤石山变质核杂岩研究

新疆北山裂谷带西缘若羌县赤石山地区存在大型变质核杂岩构造。其下拆离盘为古元古界结晶基底杂岩 ,上拆离盘为中元古界白湖群变质岩系 ,滑脱拆离带为已变形的大型韧性正断层。核杂岩南、北侧发育上叠盆地 ,北侧形成“年轻”正断层及同构造期岩浆岩。变质核杂岩的形成与晚古生代北山陆内裂谷区域伸展有直接联系。该区变质核杂岩的首次厘定 ,对深化北山裂谷的研究具有重要意义     

抓"软"管理 提升核心竞争力

从更新观念,推动改革和创新;营造企业内外发展的良好氛围;构筑企业文化,提升企业核心竞争力3个方面阐述了抓“软”管理,对提升企业核心竞争力的重要作用。     

Recent temperature increase recorded in an ice core in the source region of Yangtze River

Interests on climate change in the source region of Yangtze River have been raised since it is a region with the greatest warming over the Tibetan Plateau (TP). A 70-year history of precipitation δ~(18)O has been recovered using an ice core record retrieved in a plat portion of the firn area in the Guoqu Glacier (33°34′37.8″N, 91°10′35.3″E, 5720 m a.s.l.), Mt. Geladaindong (the source region of Yangtze River), in November, 2005. By using a significant positive relationship between ice core δ~(18)O record and summer air temperature (July to September) from the nearby meteorological stations, a history of summer air temperature has been reconstructed for the last 70 years. Summer temperature was relatively low in 1940s and high in 1950s to the middle of 1960s. The lowest temperature occurred in the middle of 1970s. Temperature was low in 1980s and dramatically increased since 1990s, keeping the trend to the begin-ning of the 21st century. The warming rate recorded in the ice core with 0.5℃/10 a since 1970s is much higher that that in the central TP and the Northern Hemisphere (NH), and it becomes 1.1℃/10 a since 1990s which is also higher than these from the central TP and the NH, reflecting an accelerated warm-ing and a more sensitive response to global warming in the high elevation region.     

核心价值观的缺失与大学生价值观教育

大学生的失败并不都是由核心价值观的缺失引起的,但是核心价值观的缺失必然引起大学生理想信念的淡漠,价值取向的偏离和人生航向的迷失.这就是对大学生有效进行核心价值观教育的紧迫性、必要性和重要性.     

简论软件保护产品核心库开发

主要依据测试驱动开发技术的两个核心思想,首先通过测试用例来分析现有软件保护产品的缺陷,然后依据产品缺陷列表重构产品核心库;并在重构的产品核心库安全模型中引用了安全通道的概念,提升了核心库的反破解能力;对核心库中关键代码加入了互斥操作,提高了核心库的系统稳定性.这样设计既保证软件保护产品的质量,又缩短了核心库的开发周期.     

子洲地区山西组及盒8段有利砂体成因探讨

目的为了查明鄂尔多斯盆地东部子洲地区山西组及盒8段有利砂体的特征及成因,进而寻找有利砂体及高产天然气聚集区。方法采用野外观察与室内研究相结合的方法。结果大量的砂岩样品统计显示,山西组砂岩类型以岩屑砂岩、石英砂岩为主,其次为岩屑石英砂岩,盒8段砂岩主要为岩屑砂岩、岩屑石英砂岩;不同类型的砂岩物性不同,石英砂岩物性最好,其次是岩屑石英砂岩,岩屑砂岩物性最差;沉积相分析认为,子洲地区山西组主要为三角洲前缘,盒8段发育辫状河三角洲前缘,探明了重点气层组山23及盒82沉积微相的平面展布。结论有利的天然气储集体主要形成于水下分流河道微相,由于山西组和盒8段形成时古地理条件的不同,其砂体类型及储集性能也有一定的差异。     

腰英台地区裂缝分布规律与油气运聚的关系

目的研究腰英台地区裂缝分布规律与油气运聚之间的关系。方法在岩心、分析测试等一性资料对裂缝标定的基础上,提取裂缝测井响应特征,进而对全区裂缝进行全面系统的测井解释,然后结合钻井、压裂等后期动态资料对测井解释的裂缝作核实验证。结果裂缝的发育程度与岩性、层厚和构造因素有关,而断层作用尤为明显。结论腰英台地区裂缝性储层发育段是该区的主力含油层,从储盖配置关系来看,裂缝在油气疏导方面起主要作用。