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1.
Banach空间中一类广义集值拟变分包含的迭代解 总被引：2，自引：1，他引：2
张云艳 《洛阳师范学院学报》2005,24(2):7-14
本文引入Banach空间中一类广义集值拟变分包含问题,利用集值预解的技巧,建立起Banach空间一类广义集值拟变分包含问题与预解方程及不动点问题间的等价关系,并给出了其解的存在性及其迭代逼近问题.这些结果改进、推广、统一了文[1-15,17-24,27-33]的相应结果. 相似文献
2.
陈晓光 《四川职业技术学院学报》2005,15(4):96-97
人的体液保持着一定的H＋浓度,即保持着一定的pH值,才能维持正常的生理和代谢功能.由于人体在代谢过程中会产生一定量的酸性物质或碱性物质,使体液中H＋浓度经常发生波动,但血液的pH值会在狭窄的7.35-7.45范围内变动,主要是人体能经过体液的缓冲系统,肺的呼吸和肾的调节等来平衡酸碱度. 相似文献
3.
Gizem Hülür Oliver Wilhelm Stefan Schipolowski 《Learning and individual differences》2011,21(6):742-746
We investigated the usefulness of the Over-Claiming Questionnaire (OCQ) as a measure of cognitive abilities. In OCQs respondents are asked to rate their familiarity with items of academic or everyday knowledge (Paulhus, Harms, Bruce, & Lysy, 2003). Some items exist in reality (reals), and others do not (foils). We developed four OCQs, each consisting of 40 reals and 8 foils from the domains of Science, Humanities and Civics. The OCQs were administered in a longitudinal rotation design to 112 participants who attended the 9th school grade at the beginning of the study. In latent variable regression analyses 53% of variation in the reals could be explained by fluid and crystallized intelligence and over-claiming as indicated by responses to foils. Further variation in responses to reals and foils was explained by intellectual engagement. Our results show that self-reported knowledge, although positively related to measures of ability, to a large extent reflects over-claiming. 相似文献
4.
额尔古纳成矿带是中国东北重要的银、铅、锌、铜、钼多金属成矿带，它位于蒙古-鄂霍茨克造山带的东南缘。最近，额尔古纳成矿带西北部发现了砂宝斯、老沟、小伊诺盖沟等金矿床和一些金矿点。这些金矿受洛古河-二根河韧性剪切带和额尔古纳河韧性剪切带控制，矿体常赋存于韧性剪切带的次级张扭性断裂构造中。矿石中硫化物含量一般不超过3％，且硫化物以黄铁矿为主。流体包裹体有气液两相、含CO2三相和纯CO2包裹体3种类型。气相成分以H2O、CO2和N2为主，含少量H，S、CH4为特征。流体包裹体的盐度低，介于2.06～8、54％NaCleqv之间。老沟金矿流体包裹体均一温度介于171℃～452℃之间，平均295℃，小伊诺盖淘金矿包裹体均一温度为169℃～493℃，平均亦为295℃，均属中温热液矿床。老淘金矿成矿压力为61～122MPa，平均82MPa；小伊诺盖沟金矿成矿压力为38～172MPa，平均93MPa。前者成矿深度介于6～9km，平均7km；后者成矿深度为4～11km，平均8km。上述金矿床的地质-地球化学特征与世界造山型金矿类似，形成于蒙古-中朝板块与西伯利亚板块之间的陆-陆碰撞造山作用。 相似文献
5.
第17、18届世界杯足球赛决赛阶段进球特征的量化分析 总被引：1，自引：0，他引：1
运用文献资料法、录像观察法、数理统计法和对比分析法,对2006年世界杯64场比赛147个进球特征进行统计分析,并与2002年世界杯64场比赛161个进球进行对比,揭示在当今高水平足球比赛中进球的规律和特征以及发展的趋势,并据此提出有针对性的建议。 相似文献
6.
运用新的不等式技巧和Bohnenblust-Karlin不动点定理研究了一类具Hybrid边值条件的分数阶微分包含解的存在性,获得了该包含解存在的一个新的充分条件.我们的结果实质性的改进和推广了相关文献的结果,并举例说明了我们的结果优于文[7]的定理. 相似文献
7.
山东招平断裂带大磨曲家金矿床流体包裹体初步研究 总被引：1，自引：0，他引：1
The Damoqujia gold deposit, discovered recently and located in the north of Zhaoping fault zone, is a large altered rock type deposit. In this paper, we report the preliminary research results of the fluid inclusions and discuss its metallogenic implications. The homogenization temperatures of fluid inclusions fall into four ranges： 310 ～350℃, 230 ～270℃, 160 ～ 200℃ and 110 ～ 150℃ ; corresponding to the four stages of hydrothermal ore～forming processes ： coarse grain pyrite～milk white quartz stage （ I ）, smoky gray Au～bearing quartz～fine grain pyrite stage （ 11 ） , Au～bearing polymetallic sulfide～quartz stage （ III ） , and quartz～carbonate stage （ IV ）. Ore～forming fluid is with low salinity and low density, ranging from 1.4 WtNacl% to 13.6 WtN～cl% and from 0.48g/cm～ to 1.03g/cm～ respectively. The inclusions are dominated by H20 and CO2 in gaseous compositions, and Na ＋ and K ～ in positive ions, SO～～ and CI ～ in negative ions of liquid compositions. Au～S complex is the major form for transportation of gold. The pressure varied from 260MPa to 340MPa during the formation of CO2～bearing inclusions at the early mineralization; the fluids are rich in SO～～ and Na ＂. The pressure is 26 ～49 ～ 105 Pa during the formation of the aqueous salt inclusions in late mineralization, the inclusions are rich in CI～ （ F～ ）, Na～. ～$18Oqu～,zis 10. 64 ～ 12.68%0, and the corresponding ～518 OH2o and ～＆D is -5.44 ～ 6.47%0 and -95.52 ～ 106.48%o respectively. Based on the studies about compositions and hydrogen and oxygen isotopes of inclusions, it is evidenced that ore-forming fluid is magmatic hydrothermal fluid in early period, but affected by meteoric water in late. 相似文献
8.
IrinaA.Andreeva Vyacheslav I.Kovalenko Vladimir B.Naumov 《中国科技期刊研究》2007,23(1):73-82
Crystalline and melt inclusions were studied in garnet, diopside, potassium feldspar, and sphene from the garnet syenite porphyry of the carbonatite-bearing complex Mushugai-Khuduk, southern Mongolia. Phlogopite, clinopyroxene, albite, potassium feldspar, sphene, wollastonite, magnetite, Ca and Sr sulfates, fluorite, and apatite were identified among the crystalline inclusions. The melt inclusions were homogenized at 1010℃～1080℃ and analyzed on an electron microprobe. Silicate, salt, and combined silicate-salt melt inclusions were found. Silicate melts show considerable variations in SiO2 concentration （56 to 66wt% ）, high Na2O ＋ K20 （up to 17wt% ）, and elevated Zr, F, and Cl contents. In terms of bulk rock chemistry, the silicate melts are alkali syenites. During thermometric experiments, salt melt inclusions quenched into homogeneous glasses of predominantly sulfate compositions containing no more than 1.3wt% SiO2. These melts are enriched in alkalis, Ba, Sr, P, F, and Cl. The investigation of the silicate and salt melt inclusions in minerals of the garnet syenite porphyries indicate that these rocks were formed under influence of the processes of crystallization differentiation and magma separation into immiscible silicate and salt （sulfate）liquids. 相似文献
9.
本文利用VB6.0和Access数据库技术,开发了热工基础考试系统,并简要介绍了该系统的设计思想、主要功能及实现方法,并给出了部分程序代码。 相似文献
10.
基于ABAQUS有限元分析方法,对两种热处理工艺下的16 Mn钢中MnS夹杂物在同一拉伸载荷作用下的应力和应变分布进行了研究。结果表明,两种晶粒尺寸的材料在长条形MnS夹杂物附近存在着垂直于加载方向的X形状的Mi-ses应力和PEEQ集中区。但细晶的16Mn钢中MnS引起的应力和应变集中程度要明显大于粗晶的16Mn钢中MnS引起的应力和应变集中,其原因与细晶强化有关。 相似文献