Surface area of papermaking woodpulps used by the British paper industry

The surface area was determined for various papermaking woodpulps: bleached eucalyptus globulus sulphate pulp; bleached eucalyptus grandis sulphate pulp; bleached betula verrucosa sulphate pulp; bleached pine/spruce sulphate pulp; bleached pine/spruce sulphate pulp fines. The method of negative adsorption was used which gives an effective wet surface area. By looking at negative adsorption data more closely, some inference can be made about the morphology of the substrate.Glossary of symbols B (e²/2kT)^1/2 - ¯C concentration of fibre per unit volume of pulp - 1 - ¯¯c - h angle between pore and the axis of the bed in a permeable material - K permeability coefficient - k Boltzmann constant - k ₀ shape factor for pores in a permeable material - n _i concentration of co-ion in the bulk solution - n _i experimentally observed increase in concentration of co-ion in the bulk solution - S surface area - S _t wS - S ₀ surface area per unit volume of permeable material - V _t total volume of solution - V excluded volume - V _s excluded volume accessible to water but not to ions - V _obs experimentally observed excluded volume - w weight of dry fibre - ¯ effective volume of fibres in a permeable pad - surface potential at outer Helmholtz plane     

浅谈开放教育与图书馆服务

广播电视大学图书馆是电大的文献信息中心,随着开放教育这一新的教育模式的出现,图书馆也应在整体上做出相应的改革,树立“以人为主体”的服务理念。未来图书馆事业发展的核心是信息增值服务和人本服务。     

中国小冰期区域气候演化研究

在我国不同地区通过不同代用资料如冰芯、树轮、孢粉、湖泊沉积物、历史文献记录等恢复的小冰期气候的基础上, 分析总结了小冰期我国气候演化的区域分异特征,并探讨其原因机制,力图为未来气候变化提供参考。     

浅论新型师生关系的建构

随着素质教育的不断推进和深化，建立新型的师生关系在教学改革中显得尤为重要。通过师生相互沟通使学生参与教学决策，通过了解学生需求以融合师生感情并增强学生的主体意识，从而在更高的层次上激发学生参与教学活动和教学管理的积极性、主动性，使学生能够开放思维的空间，激发创新灵感，并真正成为学习的主人。     

长江流域棉花种植面积变化遥感监测--以安庆市和池州市为例

决定棉花产量的关键因素之一是棉花的种植面积,适时准确地掌握棉花的种植面积对于科学指导棉花生产具有十分重要的意义.文章以安庆市、池州市为例,系统地介绍了在棉花种植面积遥感监测过程中,通过土地利用背景数据库建设,以及基于背景数据的棉花种植面积遥感解译,准确地监测了棉花种植面积及其变化率.结果显示长江流域棉花主要集中分布于沿江的洲圩区,其次分布于沿江的岗地和丘陵;在2001～2002年度,棉花种植面积变化主要是减少,在2002～2003年度,棉花种植面积变化主要是增加.究其变化的原因,主要受棉花市场价格和气候条件的影响.     

陕西省人均粮食与人均耕地变化研究

对陕西省人均粮食及人均耕地变化进行了时空差异分析,结果表明:(1)近50余年的绝大多数年份为人均粮食占有量的递增期,且不同时段的增幅不同;粮食增长率大于人口增长率的时期,对应人均粮食的增长时期;(2)1978—1998年绝大多数地、市人均粮食递增,且地域差异明显;(3)近50多年来全省耕地面积总体逐年递减,近10年来减少之势加剧;同期人口数量的持续增长,造成人均耕地面积急剧减少.相关回归分析显示:各地、市人均粮食绝对增量与其相对增量之间呈正相关,人均粮食增加量占粮食增量的份额整体偏低;提高粮食生产水平及控制人口是增加全省人均粮食占有量的重要途径.     

利用空间大地测量技术研究地球动力学最新进展

空间大地测量以高精度，高时空分辨率测定地球整体（地球自转）和各圈层（特别是大气，海洋与地壳）的运动，使地球动态变化的监测，研究及应用呈现了崭新的面貌，本文介绍了近年来国际地球动力学最新发展概况，内容包括地壳运动，地球自转，重力场时间变化等。     

论FDI对西部制度变迁的影响及对策

本文首先对我国西部地区利用FDI的现状进行了描述 ,然后运用回归分析的方法分析了FDI和制度变迁的关系 ,指出FDI是影响区域制度变迁的重要因素 ,FDI在区域分布上的不均衡严重制约着西部地区制度变迁的进程。西部地区应该加快体制改革的步伐 ,改善投资环境 ,吸引FDI ,进而通过FDI带动西部地区制度变迁的进程 ,最终形成FDI和制度变迁相互推动、相互促进的良性循环。     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.