Raw mix designing, clinkerization and manufacturing of high-strength Portland cement from the limestone and clay of Darukhula Nizampur, Nowshera District, North-West Frontier Province （N.W.F.P.）, Pakistan

This paper covers the detailed version of the potential raw material deposits at Darukhula and the adjacent areas of Nizampur, the manufacturing of high-strength Portland cement samples from the same material and comparison of the physical and chemical parameters for resulting cement with British and Pakistan standard specifications, which include compressive strength, setting time, consistency, lechatelier expansion, Blaine and insoluble residue. It was found that the raw material available in the study area meets the standard specifications and the area is feasible for the cement plant installation. The area can provide raw material which is quite sufficient for the running of a cement plant.     

CCD星点提取方法研究

电荷耦合器件CCD星敏感器的关键问题是星图识别,星图识别就是从星敏感器获得的原始星图中获取星的位置和星等信息。在介绍星敏感器工作原理的基础上,初步探讨了电荷藉合器件（CCD）天文定位的应用和优点,重点分析了Moravec算子、Frstner算子、Harris算子等几种点特征提取算子的原理和其适用性。     

克孜尔水库跨断层形变变化速率的非均匀性特征分析

对克孜尔水库跨断层垂直形变近40年的资料和水平形变近32年的资料进行了分析。研究发现,①跨断层形变的变化速率具有明显的不均匀性,根据数据序列走势,变化速率的不同可分为6个阶段;②水库施工对跨断层形变有一定的影响,水库蓄水对跨断层形变有显著的影响;③水库蓄水达到正常库容量后的新平衡状态下,跨断层形变速率变化几乎是无干扰背景下变化速率的2倍;④区域应力场的增强对跨断层形变趋势性转折有显著性影响。     

西氏鲍与皱纹盘鲍及其正反杂交F_1代样本的营养成分的组成和含量比较

对西氏鲍、皱纹盘鲍及其正反杂交F1代样本的含肉率、基本营养成分的组成和含量、矿物质含量及氨基酸和脂肪酸的组成和含量分别进行测定,并对它们的营养价值进行综合评价.结果表明,正反杂交F1代样本和皱纹盘鲍的含肉率均显著高于西氏鲍（p〈0.05）;西氏鲍的粗蛋白质含量最高（63.65%）,粗脂肪含量最低（3.37%）,2种杂交F1代样本的肌肉蛋白质含量都高于皱纹盘鲍;亲本及其正反杂交F1代样本内脏中的Fe、Mn、K、Ca、Zn、P、Cd、Pb、Cr含量均高于其足部肌肉,但4种鲍足部肌肉的各种元素含量差别不大.实验测定皱纹盘鲍♀×西氏鲍♂杂交的F1代样本的不饱和脂肪酸相对总量和牛磺酸含量高于其他3种鲍;西氏鲍♀×皱纹盘鲍♂杂交的F1代样本的氨基酸总量（56.50%）、必需氨基酸含量（17.26%）、必需氨基酸指数（93.47）及鲜味氨基酸总量（24.51%）均高于其他三者.以上实验数据说明,通过种间杂交,亲本某些遗传性状缺陷在子代中得以改良,并且获得的正反杂交F1代样本都有部分性状优于双亲.     

松辽盆地F油层高岭石、伊利石对储层物性、敏感性影响的实验研究

松辽盆地F油层砂泥岩互层发育,高岭石、伊利石为其主要粘土矿物,对研究储层物性及该油层的有效开发具有重要意义。本文通过对F油层90块天然岩心的室内研究发现,F油层渗透率、孔隙度随着高岭石相对含量的增加而增加,随着伊利石相对含量的增加而减小。砂岩层渗透性较好,高岭石相对含量较高,次生石英很少就地沉积,大量长石溶蚀孔隙得以保存;泥岩层渗透性差,伊利石相对含量较高。而且伊利石纤维状赋存和高岭石书页状赋存使砂岩层孔渗性更好,而使泥岩层孔渗性更差。该层开发过程中,高岭石、伊利石对储层物性的影响由室内岩心流动实验可知,F油层为中等强度偏弱速敏、中等强度偏强碱敏,速敏指数随着高岭石、伊利石绝对含量的增加而增加;储层的碱敏指数随高岭石绝对含量的增加而增加,而与伊利石含量无关。由于在所有粘土矿物中,高岭石相对含量接近一半,所以在F油层的开发过程要注重防范高岭石的碱敏、速敏损害。     

汞离子对细基江蓠孢子萌发和生长的影响

研究了4种Hg2+浓度对细基江蓠果孢子和四分孢子附着、萌发和生长的影响。结果表明:与对照组相比,Hg2+抑制了果孢子附着却促进了四分孢子的附着,但0.0025 mg/L浓度与对照组的差异不显著(P>0.05),各浓度间差异显著(P<0.05);Hg2+在实验浓度范围内(0.0025、0.0050、0.0075、0.0100 mg/L)影响了孢子的正常萌发,使孢子不能正常分裂和生长,刺激了孢子脱落,并且使盘状体的形态发生变异;`Hg2+不同浓度之间也存在显著差异(P<0.05),并且Hg2+浓度越高对孢子的萌发和生长影响越大。     

辽西义县组基性、中基性火山岩内沉凝灰岩层的发现及其意义

义县组岩性以基性、中基性火山岩、火山碎屑岩为主，局部发育有富含“热河生物群”化石的沉积层。在这些沉积层之下、义县组复成分底砾岩之上，发现有 4个沉凝灰岩层，与基性、中基性火山岩呈互层状产出，其岩性以沉凝灰岩或含砾凝灰质粉砂岩为主。这些凝灰岩层厚度虽小，但分布较广泛，走向延伸稳定。根据辽西地区中生代火山岩活动的基本规律，沉凝灰岩层与基性、中基性火山岩的空间展布特征及野外地质综合研究将义县组早期火山活动划分出 5个火山作用旋回，并确认四合屯、黄半吉沟、尖山沟、以及上园、大康堡、河夹心等地富含“热河生物群”化石的沉积层均属于同一火山旋回（第五旋回）的产物。这一发现极大地丰富了辽西地区中生代陆相盆地火山—沉积作用的研究内容，并将促进火山活动与生物灭绝事件方面的研究工作。     

DNA and morphological identification of an invasive swimming crab,Charybdis japonica,in New Zealand waters

Mitochondrial DNA sequences were used to identify an invasive swimming crab found in Waitemata Harbour, New Zealand. A 457 base sequence of the cytochrome oxidase 1 gene was compared in New Zealand specimens and nine species of Charybdis from Australia and Asia. The New Zealand specimens aligned with C. japonica. The diagnostic morphological characters of C. japonica were also checked in 54 specimens of the species collected in Waitemata Harbour, and concur with the mtDNA result. This is the first record of C. japonica establishing populations outside its native range. C. japonica, along with C. hellerii and the Lessepsian migrant C. longicollis, are the only known invasive species of Charybdis. C. japonica and C. hellerii are two of the few Charybdis species that inhabit the intertidal zone, and it is likely that the intertidal characteristics of these species contribute to their success as invasive species.     

Geoid from geopotential model in the Taiwan area

The geoid undulation on GRS80 in the Taiwan area at half‐degree grid points has been calculated using the reduced 30’ × 30’ block mean gravity anomalies and the OSU91A geopotential coefficient set up to degree and order 360. The OSU91A results have been used to compare with WGS84, CEM10C, and OSU86F geoid undulations determined in 18 first‐order triangulation stations of the Taiwan Geodetic Datum 1980 (TGD80). Comparisons have also been made between these free‐air anomalies determined from OSU91A, and terrestrial gravity anomalies. It has been found that the average difference between the OSU91A model‐derived, and 243 actual point free‐air anomalies is 16.8 ± 48.0 mgal. It has also been found that more reliable and dense terrestrial gravity data are needed, both for terrestrial observations and for the OSU91A model, to achieve the very high‐precision geoid on GRS80 in the area of study.