Monodisperse chloromethyl-functionalized macroporous polymer particles by seeded polymerization in aqueous media

This study presents a method to produce monodisperse chloromethyl-functionalized macroporous poly(styrene-co-divinylbenzene) polymer particles by seeded polymerization in aqueous media. We observed that the molecular structure of polystyrene seed particles, the composition of the secondary monomer mixtures, and the type of solvents were very important factors that determine the morphology and porosity of the final particles. This study proposes that the molecular chemistry of polystyrene seed polymers, increasing molecular weight or crosslinking, is another factor that can control the porosity of the final particles. Also, the selection of a poor solvent was effective in forming the larger surface area. In this study, it was confirmed that the chloromethyl groups introduced on the surface of porous particles were quantified chemically and their effective incorporation had a close relationship with the surface area.     

Biotechnological storage and utilization of entrapped solar energy

Our laboratory has recently developed a device employing immobilized F₀F₁ adenosine triphosphatase (ATPase) that allows synthesis of adenosine triphosphate (ATP) from adenosine 5′-diphosphate and inorganic phosphate using solar energy. We present estimates of total solar energy received by Earth’s land area and demonstrate that its efficient capture may allow conversion of solar energy and storage into bonds of biochemicals using devices harboring either immobilized ATPase or NADH dehydrogenase. Capture and storage of solar energy into biochemicals may also enable fixation of CO₂ emanating from polluting units. The cofactors ATP and NADH synthesized using solar energy could be used for regeneration of acceptor d-ribulose-1,5-bisphosphate from 3-phosphoglycerate formed during CO₂ fixation.     

Effect of Inorganic Ions on Oleate Adsorption at a Nigerian Hematite–Water Interface

Using “pure” natural hematite selected from a high silica Nigerian hematitic ore, oleate adsorption densities at the hematite–water interface were determined in the presence of various inorganic ions (anions and cations) of different charges and at varying concentrations. Adsorption density was determined using electrical conductivity measurements. The specific surface area of the hematite particles was determined using the method of adsorption of paranitrophenol in aqueous solution. Inorganic ions in solution depressed oleate adsorption at the aqueous hematite surface. The charge of the ion proved to be the dominant factor determining the depression of oleate adsorption. Ionic strength also was an influence, up to a limiting value at which monolayer oleate coverage of the hematite surface occurred. The inorganic ions in solution are considered to function through nonspecific adsorption in the diffuse region of the electric double layer.     

碱性水蒸气处理的ZSM-5沸石酸性质及孔结构的影响

 采用XRD，NH3－TPD，比表面积和孔结构测定等研究了在不同温度下用含10％NH3的水蒸气处理时HZSM－5沸石n（Si）／n（Al）＝25）酸性质及孔结构的变化规律．结果表明，随着处理温度的提高，HZSM－5的结构未发生明显的变化；样品的总酸量下降很快，但弱酸分布量相对提高，而强酸分布量相对下降；提高处理温度，样品的比表面积和微孔体积减小，二次孔或中孔体积及外表面积有增大的趋势．     

高比表面积窄孔分布氧化铝的制备研究 Ⅰ.沉淀条件的影响

 以硫酸铝液为原料，以氨水、氢氧化钠和铝酸钠为碱沉淀剂，采用pH摆动法制备了高比表面积、大孔径、窄孔分布、大孔体积氧化铝，考察了沉淀剂、沉淀温度及沉淀时酸侧pH值对氧化铝物性的影响，并对pH摆动法与等pH沉淀法的结果进行了比较．结果表明，通过改变制备参数可以获得高比表面积、大孔体积的氧化铝，当沉淀温度为70℃，pH摆动3或4次时，氧化铝的孔体积可高达1．0ml／g，比表面积仍大于300m2／g．用pH摆动法制得的样品比用等pH沉淀法制得的样品容易酸溶，对挤压成型有利．不同样品在酸溶液中的分散性表明，用氨水沉淀剂可获得相对较小的沉淀粒子．改变沉淀时酸侧的pH值，可导致沉淀粒子的结构发生变化．     

云南两高辐合背景下低涡强降水过程对比分析

基于气象观测和欧洲中期天气预报中心第五代大气再分析资料（ERA5）,选取2018—2020年发生在云南的3次两高压辐合区（以下简称两高辐合）背景下低涡连续性强降水过程进行对比分析,探究其环流形势、动热力因子及水汽辐合的相似性和差异性.结果显示：(1)夏半年西太平洋副热带高压（以下简称西太副高）西伸时,云南常受两高辐合影响,当辐合区中有低涡生成,易发生连续性强降水,且强降水落区并不完全分布在整个狭长的两高辐合区内.(2)两高辐合区低涡降水具有相似的雨带分布和移动特征,但雨带的集中程度、分布范围、小时雨强和总雨量存在差异.强降水开始时,落区偏东,随着西太副高西伸及东北引导气流的引导,低涡向南向西移动,强降水落区也随之向南向西移动.低涡在某一地区徘徊导致降水集中在该区域,且西太副高西伸较强时,两高辐合形势更强,低涡降水大雨及以上量级雨带也更窄.(3)低涡造成的降水主要分布在低涡中心及低涡切变附近,且降水发生在低层暖湿的环境中,低层及中高层有冷空气侵入时,小时雨强的极端性更强,降水落区也相对偏北.两高辐合区低涡降水落区与水汽辐合区对应较好,水汽辐合强度较弱时,对应的总降水量较小.     

人工干预压采条件下东风湖泉域地下水环境响应研究

为掌握我国北方典型岩溶泉域在人工干预条件下地下水的动态响应规律,以涉县东风湖泉域为研究对象,结合区内地质、水文地质、2011-2021年地下水位动态监测和地下水压采资料,在分析该地区地下水动态变化特征的基础上,运用GMS软件构建了在人工压采干预作用下的地下水流数值模拟模型,对地下水位变化趋势进行了预测。结果表明：①研究区地下水动态变化明显,具有周期性、滞后性,具体表现为4个变化阶段;②研究区内岩溶地下水整体呈现回升的状态,但是空间分布特征不同,上升区主要分布于下游地区;;③地下水类型为降水入渗-开采型,低水位期基本在5-6月,高水位期在1-2月;④在干预条件下,区内地下水位有着不同程度的回升,南部(下游)浅层水位响应特征值超过15m,中游地下水位响应特征值达到了5-10m,北部(上游)地下水位响应特征值为3-5m;上游和中游地下水位影响整体小于下游,下游水位响应尤为突出。该研究对于泉域内泉的保护以及地下水开发利用和保护具有重要的理论和实际意义。     

海口分层流中的泥沙输运计算

本文展示了一个计算泥沙输运过程的三维数值模型,此模型的特点在于较准确地计入凝絮及河床侵蚀对于泥沙沉淀过程的影响,关于凝絮及侵蚀的定量计算模型已为大量实验所验证,且是首次被结合运用于三维输运计算。文中对于海湾区域的泥沙输运进行了数值研究,第一闪通过定量计算评实了所谓最大浑浊区的存在,并研究了影响其形成及强度的几个因素,这些计算结果不仅评实了数值模型的有效性,而且显示了其在泥沙输运研究方面的作用与潜力     

局域网的规划与INTERNET的连接技术

介绍了NETWARE局域网的规划方法、实施步骤,并简述了其与INTERNET实现连接的几种方法。     

贵州省粮食储藏地理区划初步研究

通过对贵州省气象特征的分析,尤其是对影响粮食安全储藏的主要环境因素温度和相对湿度的分析,得出贵州省粮食储藏可划分为四个地理区域。依据各区域的储藏气候条件和主要粮食的储藏特点,提出相应的储藏技术措施。