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681.
不同虾种间肌肉组织蛋白质的比较 总被引:2,自引:0,他引:2
采用薄层等电聚焦凝胶电泳方法对罗氏沼虾(Macrobrachium rosenbergii)、绿须虾(Aristeus virilis)、长毛对虾(Penaeus penicillatus)、日本对(P.japonicus)、斑节对虾(P.monodon)和周氏新对虾(Metapenaeus joyneri)的肌肉组织蛋白质进行分离,检测各蛋白质组份及其等电点。根据蛋白质区带的共享度计算共相互间的遗传距离指数,然后用聚类方法处理数据,构建系统树,分析其间的差异程度,最后确定6种虾的亲缘关系。结果表明,每种虾可获得6-11条 蛋白质区带,等电点范围在4-6.95之间。虾类肌肉组织蛋白质组份及其电泳行为,可为虾类在分类学上的定位提供生化依据。 相似文献
682.
熊凤兰 《中国海洋大学学报(自然科学版)》1990,(2)
本文定义了从X到Y的模糊变换σ_(g·f)和从Y到X的模糊变换σ_(g·f)~(-1)。当g(λ)=λ时这种变换便是查德提出的变换,即扩展原理。此外,还讨论了此变换的性质;指出其在代数系的同态,尤其是群同态方面的应用。并给出有关变换的唯一确定性定理。 相似文献
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It is necessary for undergraduates majoring in geography to learn the history of geographic thought. Although there are different cultural and educational backgrounds between China and the West, teaching methods such as text teaching, students’ presentations and group learning are suitable for most of teachers and students even from different countries and regions. The blended method is helpful to popularize history of geographic thought and improve the level of teaching and learning. Owing to lack of the class on the history of geographic thought in countries like China, the authors try to explore a blended method for the first-year geography undergraduates and to assess the effects of this teaching based on some questionnaires. The students have different benefits and responses to this class. A special group consisting of one teacher and several undergraduates does the research and coauthors the paper through making questionnaire, interviewing and analyzing materials from 67 freshmen majoring in human geography and geography science (teacher-training) in China. For the undergraduates especially from the countries like China, it is well worth making the history of geographic thought become a necessary and interesting class. 相似文献
687.
昝立博 《南京气象学院学报》2016,8(5):479-480
环称为唯一强clean是指每一个元素都可唯一的表示为可交换的幂等元与单位元的和.主要讨论唯一强clean群环的结构,证明了如果群G是局部有限群,则群环RG是唯一强clean环当且仅当环R是唯一强clean环,群G是2-群. 相似文献
688.
《Chemie der Erde / Geochemistry》2016,76(4):621-641
This publication provides a literature review on experimental studies of dissolution kinetics of mainly carbonates and feldspar group minerals, i.e. most common minerals at potential CO2-injection and/or storage sites. Geochemical interaction processes between injected CO2 and coexisting phases, namely reservoir and cap rock minerals and formation fluids close to the CO2-injection site can be simulated by flow-through or mixed flow reactors, while processes far from the injection site and long-term processes after termination actual CO2-injection can be mimicked by batch reactors. At sufficient small stirring rates or fluid flow rates as well as low solute concentrations flow-through reactors are also able to simulate processes far from the injection site. The experimental parameter temperature not only intensifies the dissolution process, the dominant dissolution mechanisms are also influenced by temperature. The dissolution mechanisms change from incongruent and surface controlled mechanisms at lower temperatures to congruent and transport controlled mechanisms at higher temperatures. The CO2 partial pressure has only a second order influence on dissolution behavior compared to the influence of pH-value and ionic strength of the CO2-bearing brine. Minerals exposed to CO2-bearing brines at elevated temperatures and pressures are subject of alteration, leading to severe changes of reactive surfaces and potential precipitation of secondary minerals.Computational simulations of mineral reactions at potential CO2 storage sites have therefore to include not only the time-resolved changes of dissolution behavior and hence kinetics of mineral dissolution, but also the influence of secondary minerals on the interaction of the minerals with CO2-enriched brines. 相似文献
689.
寻乌岩组变沉积岩发育在江西南部新元古代—早古生代南城—寻乌盆地内,时代为震旦—寒武纪。寻乌岩组的Si O2含量变化较大,除1个含量较低的样品外,平均为63.01%,具有相对较高的K2O、Al2O3及(TFe O+Mg O)值,较低的Na2O、Ca O。相容元素含量与后太古代澳大利亚页岩(PAAS)十分接近,高于中国东部上地壳,与其较高的(TFe O+Mg O)特征相吻合,说明源区具有一定数量的中基性组分。稀土元素总量高于上地壳及PAAS,但其球粒陨石标准化配分模式与典型的上地壳及PAAS相似,表现为明显向右倾斜,轻稀土富集,重稀土平坦,铕负异常显著,铈负异常不明显。岩石地球化学特征显示其原岩属于一种中等成熟度的陆源碎屑岩,物源主要为被改造的上地壳长英质和花岗质物源区,少部分物源为中基性火山岩。高场强元素及稀土元素等不活动元素地球化学特征表明其沉积环境为浅海—半深海,其构造环境属于发育有裂谷系的被动大陆边缘,该认识从沉积岩地球化学方面为华南早古生代构造属性提供了新资料。 相似文献
690.
Integrating ground heat exchanger elements into concrete piles is now considered as an efficient energy solution for heating/cooling of buildings. In addition to the static load of buildings, the concrete piles also undergo a cycle of thermal deformation. In the case of single energy pile, calculation methods already exist and permit to perform a proper geotechnical design. In the case of energy pile group, the thermo‐mechanical interactions within the group are more complex. Very few experimental results on the energy pile group are available so that numerical analysis can be an interesting way to provide complementary results about their behavior. This paper deals with a numerical analysis including a comparison between a single energy pile and an energy pile group with different boundary conditions at the pile head. In order to take into account the stress reversal induced by the thermal expansions and contractions, a cyclic elastoplastic constitutive model is introduced at the soil–pile interface. The analysis aims to give some insights about the long‐term cyclic interaction mechanisms in the energy pile group. Based on this qualitative study, some guidance can be brought for the design of energy piles in the case where group effects should be considered. Copyright © 2015 John Wiley & Sons, Ltd. 相似文献