Prediction of nonregular secondary structures of proteins based on wavelet analysis

The secondary structures of proteins fall into two classes: regular structure and nonregular structure. Helices and sheets are termed "regular" structures because their residues have repeating main-chain torsion angles, and their backbone N-H and C-O groups are arranged in a periodic pattern of hydrogen bonding. In contrast, the remaining structures with nonrepeating backbone torsion angles are called nonregular secondary structures. In this note, we performed an extensive sequence analysis of nonregular secondary structures and showed that these nonregular parts could be effectively predicted by continuous wavelet transform.     

Timing and history of marine hydrocarbon accumulation in Tarim craton

<正> Based on the analyses of hydrocarbon inclu-sions, K-Ar dating of authigenic illites and oil/gas-watercontact retrospection as well as other methods, the marineprimary reservoirs in the cratonic region of the Tarim Basinare found to have been formed in the late Caledonian toearly Hercynian, late Hercynian, and Himalayan, and oil andgas adjusted and redistributed in the Yanshanian (Jurassic toCretaceous) and Himalayan (Tertiary). The analyses alsoshow that the remaining primary oil accumulations aremostly formed in the late Hercynian, and the secondary oilreservoirs resulted from the adjustment and redistribution ofthe earlier accumulations during the Yanshanian and Hima-layan (especially late Himalayan), of which the Himalayan isalso the major stage of gas accumulation. The primary oilreservoirs formed in the late Hercynian mostly occur withinthe Paleozoic formation, whereas the secondary reservoirsformed in the Himalayan in the Mesozoic. The late adjust-ment and redistribution of reservoirs in the craton region ofthe Tarim Basin is ubiquitous because of the intensified tec-tonic movements since the Mesozoic, especially Cenozoic andintrusion of the high- to over-mature gas. Furthermore, thelower amplitude of reservoirs in the craton region also makesthem easier to be adjusted and redistributed. Therefore, theremaining paleo-uplift and palaeo-slope developed in rela-tively stable tectonic regions are the main potential areas forthe middle-large marine reservoirs in the Tarim Basin.     

蛋白质结构型预测的研究

以 nα、nβ、nβαβ、n4α、n4β等五个二级结构参数为基础 ,用离散增量研究了蛋白质的聚类和蛋白质的结构型预测 .α型 ,β型和 αβ型可以很好地分别聚在三个大支中 .蛋白质结构型预测总体预测正确率为 82 % ,用 Self-consistency和 Jake-knife这两种方法测试的结果没有明显的差别 .从结果可以看出利用蛋白质的二级结构参数能较好地体现出各种结构型蛋白质的特点 .     

精细地质研究在大庆萨中南一区丙块挖潜中的应用

根据现代细分沉积相理论 ,对南一区丙块萨 +葡 II油层进行细分单元砂体沉积相带图研究 ,第一次确立了该区块油层各单砂体三角洲沉积模式 ,并对各沉积单元的沉积特征及平面非均质性进行了描述和分析 ,进而预测和确定了该地区各类砂体中不同类型剩余油富集区 ,对二次加密调整井布井及射孔方案的编制具有指导作用 .     

北京猿人洞穴堆积气候地层的再研究(英文)

周口店第一地点洞穴40余米厚的堆积层自下而上共分17层，新近测量的年代推前了近20万年，对堆支所含哺乳动物化石和孢粉资料进行聚类统计和因子分析，结合风化系数和微量元素含量等古气候代用指标，重新定量地描绘它所记录的古气候波动旋回，根据第2层TIMS测年为41万年BP，第14层上部是磁性地层测量的B／A界线，可以将该洞穴堆积层1－4层对比于深海岩芯δ^18O气候曲线的11－19段或中国黄土－－古土壤序列S4－S7，并且古气候旋回内的次级波动也可进行一定程序的对比。     

粉螨污染空气的研究

为探讨粉螨污染空气的情况 ,采用空气粉尘采样器和自制空气悬浮螨采样器 ,进行工作场所内悬浮螨的分离 ,并将获得的粉螨制片、鉴定。结果在中药厂、面粉厂、纺织厂、粮库的工作场所内和本校教学楼的工作环境内发现粉螨 8种 ,即粗脚粉螨 ( A.siro) ,小粗脚粉螨 ( A.farris) ,腐食酪螨 ( T.putrescentiae) ,椭圆食粉螨 ( A.ovatus) ,纳氏皱皮螨 ( S.nesbitti) ,害嗜鳞螨 ( L .destructor) ,粉尘螨 ( D.farinae)和屋尘螨 ( D.pteronyssinus) ,隶属于 3科 6属。由此可见 ,空气中粉螨的污染严重 ,应引起注意     

Diels—Alder反应中的区域选择性与次级轨道效应

本文介绍了含有次级作用项的分子轨道的微扰方程,从而运用前线轨道能量和系数分析了次级效应即不直接成键原子间的相互作用对 Diels-Alder 反应的区域选择性的控制作用。     

嫩江——齐齐哈尔江段水质污染状况的生物调查与评价

本文通过对嫩江——齐齐哈尔江段浮游植物与底栖动物指标的分析,为评价嫩江水质污染状况提供依据.     

模式识别方法预测蛋白质二级结构的研究

提出一种预测蛋白质二级结构的模式识别方法。该法首先对大量已知结构的蛋白质实验数据进行分析，找出鉴别蛋白质不同结构成分的有效信息，即设计分类器，然后实现对未知蛋白质二级结构的预测。用此方法对６４０个实验样本进行了研究，得到较高的预测精度，表明方法是有效的。还对实验结果进行了分析；讨论了有限样本对分类器性能的影响。     

用约束次弯矩法直接计算预应力砼超静定结构的次弯矩

本文首次提出用约束次弯矩法直接计算预应力砼超静定结构的次弯矩,具有物理意义明确,推导公式简捷,用于计算机程序设计使其更容易与普遍砼结构程序相容,用于手算更为便捷,此法也使预应力沿预应力筋变化时的公式统一,使其计算更简捷。