时效性对单桩极限承载力的影响分析

目前，盐城地区正广泛采用打入式预制桩和泥浆护壁成孔灌注桩。从这两种桩的成桩工艺，结合地基条件，对盐城地区饱和软粘土层中这两种桩成桩后休止时间对单桩极限承载力的影响规律进行了分析研究，并对载荷试验的间歇时间的确定问题作一些有益的探讨。     

髓母细胞瘤中P53、bcl-2及Ki-67的表达及其意义

用免疫组化S P法检测 2 5例髓母细胞瘤中Ki 6 7、P53 及bcl 2基因的表达。结果表明 ,在 2 5例髓母细胞瘤中 ,bcl 2和P53 蛋白的阳性表达率分别为 72 % (18/ 2 5 )和 16 % (4/ 2 5 )。Ki 6 7阳性率平均为 (33.34± 4 .98) % ,其表达与组织学分型有关。说明在髓母细胞瘤中bcl 2蛋白与P53 蛋白可能参与调控细胞的凋亡     

我国北方沙尘暴灾害及防治对策

沙尘暴是与风沙活动、土地沙漠化过程密切相关的一种发生在沙漠及其邻近地区的灾害性天气现象 ,它是高速运行气流即大风与干燥裸露地表相互作用所形成的 ,是干旱与沙漠化气候环境的产物。我国的沙尘暴主要发生在西北、华北和东北西部 ,尤以西北地区的沙尘暴发生频繁、危害严重、影响范围广泛。它的发生、发展除与大气环流、下垫面状况等自然因素有关外 ,人类大量开垦农田、放牧、樵采、过渡利用地表和地下水资源以及进行各种工矿、交通建设等活动 ,破坏了地表植被和土壤层 ,使表土裸露直接遭受风力侵蚀作用 ,既加速了沙漠化土地的扩展 ,也扩大了沙尘源 ,使沙尘暴发生的频率和强度大为增加。为此 ,本文分析了我国沙尘暴的空间分布范围、运移路径、形成原因和危害表现 ,并提出了防治沙尘暴的对策建议     

开发平潭旅游业之我见

平潭素有“千礁岛县”的美誉 ,主岛海坛风景名胜区以优质海滨沙滩和奇特的海蚀地貌被专家誉为海蚀地貌博物馆 ,于 1 994年被国务院确定为国家重点风景名胜区。但几年来平潭旅游在我省的旅游产业发展中却默默无闻 ,本文通过对平潭旅游业发展现状的换位思考 ,提出为适应新经济环境的变化 ,平潭旅游业应长远谋划来做心灵的生意     

栗斑腹鹀种群数量变化的分析

1999年至 2 0 0 1年每年 4～ 7月在吉林省西部地区对栗斑腹种群数量及繁殖情况进行了调查 ,发现三年来栗斑腹种群数量连续下降 .其原因是 :人为干扰导致栗斑腹繁殖成功率及繁殖成活率降低 ,从而导致栗斑腹种群数量下降 ;研究地区内近几年连续高温干旱的天气也导致了栗斑腹种群数量的下降 ,气温升高 (R2 =0 9964 )、降雨量减少 (R2 =0 84 98)对栗斑腹种群数量下降的影响很大 .     

反应精馏过程设计研究

介绍连续反应精馏过程设计的两种研究方法：静态分析法和有限元正交搭配OEFE法，静态分析法是对反应精馏图进行热力学和拓扑学分析，鉴定反应精馏过程的基本可能性，此方法不需要依靠确定的对象的特性，要求最少最反应混合物的物理化学特性，有限元正交配技术应用了把整级评估模型转变成连续的模型。OCFE能精确地吻俣逐板模型的优化设计，而只是使用一套较小的模型公式和避免使用与塔级数有关的总决策变量，用静态分析寻找一个最大转化率稳定态，用OCFE确定反应精馏塔的级数（塔级数）及进行精级（塔板）位置。     

低成本人体步态在线检测系统

研究了一种由 CCD摄像机、三维测力台及表面肌电信号检测装置组成的人体步态在线检测系统。在该系统中图像、力和表面肌电信号都由一台计算机实时采集。采用普通监控用图像设备和边缘检测、模板匹配等方法识别运动图像中的标志点 ,降低了系统硬件成本和对测试背景的要求。初步应用结果表明 :系统同步性能好 ,空间分辨率小于0 .2 %。该系统不仅适合于临床进行步态分析 ,而且也可用作其他与人体运动姿态有关研究的检测平台。     

试论现代教学条件下的班级规模

班级规模是影响教学质量的重要因素。本讨论班级规模与教学质量的关系，班级规模变动的原因，以及在现代教学条件下班级规模扩大所产生的利与弊及其应对办法。     

Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of northern Xinjiang

Eolian loess is widely distributed on the various geomorphic surfaces between 700–2400 m a.s.l. on the northern slope of the Tian Shan. It is formed in a synchronous manner with dust transported from the Gurbantunggut Desert in the Junggar Basin. The thickest section of loess was found in the Shawan and Shihezi regions. Paleomagnetic and climatic proxy analyses of over 71 m of a loess-paleosol sequence on the highest terrace of the Qingshui He (River) in the Shawan show that the paleomagnetic Bruhues/Matuyama (B/M) boundary lies at the bottom of paleosol S8, at a depth of 69.5 m, and the bottom of the sequence was estimated to be ∼0.8 Ma. This implies that the extremely dry climatic conditions in the Junggar Basin and the initial Gurbantunggut Desert were present at least by 0.8 Ma. High-resolution grain size series demonstrate that this area and desert expansion experienced two dramatic periods of desert expansions that occurred at ∼0.65 Ma and 0.5 Ma, respectively; and the subsequent continuous enhancement led to the environment presently observed. This tremendous environmental effect, caused by large-scale expansion of the desert and arid region of inner Asia, might be an important driving force for the global temperature drop that occurred in the mid-Pleistocene.     

Nanometer properties of oceanic polymetallic nodules and cobalt-rich crusts

An ammonia leaching process was utilized to extract Co, Ni and Cu from oceanic polymetallic nodules, whereas an acid leaching process was utilized to extract Co, Ni, Cu, Zn and Mn from cobalt-rich crusts. Both processes produced nanometer materials—ammonia leaching residue and acid leaching residue. A systematic study was conducted on the phase, composition and physicochemistry properties of these residues. The result shows that both residues contain a large amount of nanometer minerals. Ammonia l eaching residue mainly consists of rhodochrosite, with the average grain diameter of 17.9 nm; whereas the acid leaching residue mainly consists of well-developed bassanite, with the average grain deameter of 9.5 nm. The bassanite also has a microporous structure, the volume of the pore space is 1.23 × 10⁻² mL/g. Both the ammonia and acid leaching residues have a large specific surface area, and they display a strong adsorption capacity to saturate sodium chloride vapour, N₂ and SO₂. Both residues have high contents of rare earth elements, and most of these elements exist in the state of ionic adsorption. The content of σ FeO is high. The P₂O₅ enrichment is observable in acid leaching residues. The unique composition and nanometer solid properties of the leaching residues displayed their potential value and promised a bright future for their application in the field of environmental protection and materials.