海拉尔盆地地层水特征与粘土矿物转化和赋存的关系

海拉尔盆地地质条件及其复杂,开发难度大,本文将油藏地球化学中地层水研究与粘土矿物成岩转化研究相结合,指出了地层水特征与空隙中粘土矿物及其他矿物成岩转化和赋存的某种相关性,对储集层地质学研究很有助益,对勘探开发一体化研究提供了该方面重要的科研依据。     

Molecular cloning and expression of interleukin Ibeta (IL-1β) from red seabream (Pagrus major)

The interleukin 1β (IL-1β) cDNA was cloned from the red seabream (Pagrus major) by homology cloning strategy. A cDNA fragment was amplified by PCR using two degenerated primers, which were designed according to the conserved regions of other known IL-1β sequences, and elongated by 3' ends and 5' ends RACE PCR to get the full length coding sequence of red seabream IL-1β (RS IL-1β). The sequence contained 1252 nucleotides that included a 5' untranslated region (UTR) of 84bp, a 3' UTR of 410 bp and an open reading frame (ORF) of 759 nucleotides which could be translated into a putative peptide of 253 amino acids with molecular weight of 28.6 kD and putative isoelectric point pI of 5.29. The deduced peptide contained two potential N-glycosylation sites and an identifiable IL1 family signature, but lacked the signal peptide and the clear ICE cut site, which were common in other nonmammalian IL-1β genes. The RS IL-1β had the highest homology with piscine IL-1β according to phylogenetic tree analysis.     

喀斯特粘土矿物的稀土元素实验研究

本文报道对喀斯特粘土矿物进行稀土元素水解实验、解析实验、人工吸附实验的研究结果，目的在于探讨粘土矿物对离子型稀土元素最佳吸附的ＰＨ值环境。     

亚硝基血红色素食品着色剂的研究

本文以健康的猪、牛、羊的新鲜牲血为原料，经化学提取、合成及酶解等简单步骤、研制成了亚硝基血红色素食品着色剂。该产品可替代具有毒性作用的亚硝酸盐而直接加入食品着色，是一种无毒副作用的理想的调味食品着色剂，同时也增强了食品的营成份。     

DNA与中性红相互作用电化学和光谱研究

利用电化学和光谱方法研究中性红和DNA的相互作用,根据其循环伏安曲线和紫外-可见光谱,在pH=7.05缓冲体系中中性红与DNA发生了嵌插作用.     

红曲色素生产中代谢调控的研究进展

红曲色素由红曲霉发酵而得,它的发酵质量直接影响红曲色素的产量和质量.文章对近几年红曲色素发酵中代谢调控的研究进展以及控制过程中建立的数学模型作一简单介绍.     

论红三角地区的协调发展

实现区域内部的协调发展对红三角地区有着重要的意义，但其内部经济的同构、经济水平低下和区域公共品的缺位则妨碍了其协调发展。要实现协调发展，红三角地区必须对未来的发展进行合理定位，整合资源，发展优势产业，并通过制度创新促进经济协调发展。     

急性力竭游泳后小鼠血液成分变化的动态观察

为了观察急性力竭游泳对小鼠血液成分的影响,分别于小鼠力竭游泳停止后0(即刻)、1、4、8和24 h时进行尾静脉取血,测定了其白细胞、红细胞、血小板和血红蛋白等指标.结果表明:白细胞的数量在小鼠力竭游泳后0 h为(8.46±3.20)×109/L,与对照组的(10.65±2.29)×109/L比较明显减少(P＜0.05);在4 h时为(17.67±3.41)×109/L,与对照组比较显著增多(P＜0.01);在8 h以后恢复正常.红细胞的数量在小鼠力竭游泳后4 h时为(9.99±0.95)×1012/L,与对照组的(10.87±0.79)×1012/L比较明显减少(P＜0.05);在8h以后恢复正常.血小板的数量在小鼠力竭游泳后1、4、8和24 h时分别为(856.5±129.0)×109、(859.5±67.9)×109、(874.1±96.5)×109和(875.7±124.8)×109/L,与对照组的(721.5±115.7)×109/L比较均明显增多(P＜0.05).说明急性力竭游泳对小鼠血液中不同成分的作用存在差异,在一定时间内导致红细胞数减少、血小板增多和白细胞数先降后升的现象.     

Do multiple cycles of aeolian deposit-pedogenesis exist in the reticulate red clay sections in southern China?

Since the Quaternary scientists successfully dis-closed the paleoclimatic significance of the loess-paleo- sol sequence in the Loess Plateau, Northwest China, the loess-paleosol sequence has become well-known terres-trial materials revealing the multiple cyclic changes of Quaternary climates. As a carrier of paleoenvironmental information, it could compare beauty with the deep ocean deposit[8]. In recent years, however, the researchers began to put their sights to southern China. They try t…     

Loess-soil sequences in southern Anhui Province： Magnetostratigraphy and paleoclimatic significance

Two parallel loess-soil sequences from Xuancheng and Fanchang in southern Anhui Provinces are dated using geomagnetic and luminescence methods.The Brunhes/Matuyama(B/M) reversal boundary is recognized within the lower part of the so-calles Vermiculated Red Soil (VRS) in the Xuancheng section while the entire Fanchang sequence is of Brunhes age.This indicated that the most recent VRS in southern China,a stratigraphic marker and an indication of extremely warm-humid conditions,was formed during the middle Pleistocene,chronologically correlative with the S4 and S5 soil units in northern China.Microscopic and sedimentologic in vestigations reveal that eolian deposition started in this region at about 0.85 MaBp,roughly synchronous with the well-known Mid-Pleistocene climate change of global significance.The strengthening of both summer and winter monsoon circulations and the consequent river hydrological changes at that time would have provided favorable conditions for sustained eolian deposition in the middle-lower reaches of the Yangtze River since 0.85 MaBP.