全球气候变化与塔里木盆地古城绿洲演变关系

我国西部地区地形复杂,气候的地域差异性大.特别是青藏高原的突起给塔里木盆地的环境带来了巨大的变化,导致盆地气温降水的突变.从而使塔里木盆地水流分布状态发生改变,导致盆地中原有的古绿洲的蜕变,进而直接影响到整个人类的发展历史.历史研究表明,塔里木盆地气候服从于全球气候变化,并且与某些人文事件,特别是古城绿洲兴盛与消亡有着十分一致的耦合关系.所以,全球环境变化对古城绿洲发展影响重大.     

凡勃伦与马克思制度经济学思想比较

从理论来源、分析方法等方面比较了凡勃伦与马克思制度经济思想，指出二者虽然在理论来源、分析方法等方面有较大的区别，但也有一些相互融通的地方，同时，马克思经济思想给早期的制度经济学的发展开辟了更广的出路与领域。     

分子间作用力对制备含有机废弃之水泥浆体影响研究

研究以水泥处理固体有机物时，有机物对水泥水化的影响。以膜流模式说明水份在水泥浆体内传输的现象。水膜存在半干之水泥浆体，其厚度小于100nm，膜流由离分压所驱动，而离分压来自分子间作用力。膜拟结果发现，水泥浆体内局部位置可用以进行水化之水量为Q=-Aslv／6vπ。当有机物添加在水泥浆体内时，会影响Hamaker常数，Aslv因此可能使膜流不稳定或完全抑制膜流，因而使水泥浆体内局部缺水，影响水化进行，造成成品强度降低，影响品质。     

Evolutionary and ecological implications of cardenolide sequestration in the monarch butterfly

Summary Monarch butterflies sequester cardenolides from their larval host plants in the milkweed genusAsclepias for use in defense against predation. Of 108Asclepias species in North America, monarchs are known to feed as larvae on 27. Research on 11 of these has shown that monarchs sequester cardenolides most effectively, to an asymptote of approximately 350 g/0.1 g dry butterfly, from plants with intermediate cardenolide contents rather than from those with very high or very low cardenolide contents. SinceAsclepias host plant species are distributed widely in space and time across the continent, monarchs exploit them by migration between breeding and overwintering areas. After overwintering in central Mexico, spring migrants east of the Rocky Mountains exploit three predominantAsclepias species in the southern USA that have moderately high cardenolide contents. Monarchs sequester cardenolides very effectively from these species. First generation butterflies are thus well protected against predators and continue the migration north. Across the northern USA and southern Canada most summer breeding occurs on a fourthAsclepias species and in autumn most of these monarchs migrate back to Mexican overwintering sites. The ecological implications of this cycle of cardenolide sequestration for the evolution of monarch migration are discussed.     

真蓝甲藻(Gymnodinium eucyanochroum Tseng Sp.nov.)的亚微结构、色素性质及其在藻类进化中的意义

本文报告了在南京发现的蓝色裸甲藻,测定了它的藻胆色素。证明蓝色藻胆蛋白不是山“胞内蓝藻”(Cyanellen)所提供。电子显微镜的扫描表明细胞表面有众多的突起,不是光滑的;横沟内的鞭毛不是“带状”而是由细纤维丝膜状物拉着的螺旋形。透视电子显微镜观察表明,该藻有两个类型的细胞核,即“甲藻核结构”(Dinocaryotic structure)和“真核结构”,(Eucaryotic Structure),真核与叶绿体有一个共同的膜的包被,有一个与原生动物相近似的伸缩泡系统。叶绿体是分枝状,在细胞的边缘位,但也有其它形态。有淀粉颗粒而无“造粉核”或称”“蛋白核”(Pyrenoid),多数位于叶绿体外或之间,类囊体与一般甲藻不同,不是三个排成一条“带”而是两个排列成“带”。有发达的线粒体,和高尔基体;鞭毛不论纵沟内的或横沟内的,其横切面,均为9+2的形式,其纵切面是由纤维丝成束的结构。蓝色色素提取物,可见光最大吸收峰为456nm,与隐藻藻胆色素十分相似。从细胞亚微结构及其色素性质,作者认为它是藻类演化过程中的一个中间类型的甲藻共生体。     

Misuses of biology in the context of the paranormal

Summary Public suspicion of science stems from science's challenging of perceptions and myths about reality, and a public fear of new technology. The result is a susceptibility to pseudoscience. In claiming that creation science is as valid as evolution the creationists misquote scientists and seek to spread their own scientific myths concerning a young age for the earth, an act of creation based on a particular literalist interpretation of the Christian Bible and a single worldwide flood. They use methods of debate and politics, rather than scientific research. A selection of their arguments is examined and the nature of the evidence for evolution is discussed. Problems with the creation science model are noted. In the myth of the hundredth monkey phenomenon, original research is misquoted to denigrate scientific research and support sentimental ideas of paranormal events. The misuse of science is seen as damaging to society because it reduces the effective gathering and application of scientific information. However, pseudoscience provides a valuable guide to gaps in public scientific education.     

酶与有机溶剂

本文阐述了酶在有机溶剂中存在的两种形式:通过表面活性剂聚集体在有机溶剂中的溶解和直接以固态酶的形式悬浮于有机溶剂中.讨论了反胶团(或w/o微乳浊液)系统在酶促反应、选择性提取蛋白质等领域的应用和固态酶悬浮于有机溶剂中的性质和特点,并展望了这些系统的发展前景.     

西秦岭南带中志留统的岩石学特征与沉积环境

详细研究了西秦岭南带中志留统岩石学特征,对遭受重结晶作用的碳酸盐岩进行了结构成因分类。分析了该区中志留世的沉积环境及变化特征。在该区发现的层孔虫生物礁及其它“浅水”标志,表明志留纪时,为若尔盖微古陆北侧的边缘浅海环境。西部为局限陆棚环境,可分为:局限内陆棚、海湾、礁滩-泻湖-潮坪(孤立台地)等亚环境;东部为开阔陆棚环境,可分为浅海砂滩、内陆棚、外陆棚等亚环境。     

溶剂萃取法制备碳酸盐的热力学讨论

向金属氯化物(Ⅰ)的水溶液中通入CO_2气体,以期制备相应的碳酸盐和酸式碳酸盐,在常温常压下,体系的△G>0,反应几乎是不可能的。向反应体系中加入有机溶剂(S),使生成的HCl即被萃取,可促进Ⅰ的继续转化。分析计算表明,S对HCl必须有很强的萃取能力,其K_萃须在10~5以上。研究了加入有机溶剂N_(235)前后,体系的热力学状态、函数及其变化。加入N_(235)后,K_萃值增大了5个数量级。考察了温度、时间和通气次数对系统热力学性质的影响。根据反应的耦合原理和热力学分析,提出萃取剂选择的原则。结合实验数据的估算说明:溶剂萃取法由Ⅰ和CO_2制备碳酸盐的工艺路线是可行的。     

外源有机酸协同生物炭对土壤微量元素的影响

为未来改善生物炭和有机酸共存的土壤营养状况提供参考依据,有必要探究生物炭和有机酸共存对土壤中微量元素的影响。以玉米秸秆为原材料制备生物炭,采集不同深度的黄棕壤,选择柠檬酸和苹果酸这2种酸进行试验,除对照外共设置8个不同处理方式,分别是不施加或施加生物炭的表土加柠檬酸处理、不施加或施加生物炭的表土加苹果酸处理、不施加或施加生物炭的底土加柠檬酸处理和不施加或施加生物炭的底土加苹果酸处理。结果表明：（1）与对照组相比,施加2种有机酸增加了土壤中的铁和锰的溶出,且柠檬酸处理的土壤溶液中的铁和锰含量高于苹果酸处理;（2）由于底土和表土存在理化性质的差异,影响了铁和锰的溶出量,底土溶液锰的溶出量高达0.34 mmol/L,而表土溶液铁的溶出量高达0.7 mmol/L;3）2%的生物炭没有完全阻碍两种有机酸对微量元素的溶出。结论 有机酸可以活化土壤中的铁和锰,其活化效果与有机酸种类、浓度、金属、土壤酸碱度有关,且生物炭的施加对阻碍有机酸活化土壤中微量元素的能力有限。