大厂凹陷MIS3阶段以来沉积物地球化学特征分析

深海氧同位素3-1阶段是指深海沉积物有孔虫氧同位素记录的第四纪末次冰期至冰后期的一个时期,期间气候表现为间冰阶、极端寒冷、多次千年尺度气候事件至最后转暖多个变化特征,相关气候变化沉积响应及影响因素等科学问题一直以来备受关注。然而,该时期相关千年尺度气候事件的记录及讨论在华北平原地区仍有争议,为探讨华北平原西北地区在该阶段的气候特征,本研究在大厂凹陷区天然剖面进行高密度碳14断代样品测试,并开展常量和微量元素地球化学含量分析,获得地球化学数据变化趋势特征,结果表明,该剖面年代从32.5ka至8.2 ka,处于深海氧同位素3阶段末期至深海氧同位素1阶段早期。在该时段,主量元素氧化物TFe2O3、Al2O3、SiO2、MgO、CaO、Na2O与K2O与微量元素Sr、V、Ni、Co、Ga、Cu、Ba、Cr和Zn均呈现一致的变化趋势;在MIS2末次冰盛期和MIS1早期中的B?lling-Aller?d暖期和新仙女木冷期,K/Na、Al/Na、化学蚀变指数 、化学风化指数 和古温度等指标与东亚季风区气候呈现一致的变化,同时与全球尺度的事件具有同步性,因此认为晚更新世晚期华北平原的气候变化可归因于全球气候系统下东亚季风区的演化。     

内蒙古前进场岩体岩石学与锆石U-Pb年代学研究

前进场黑云母花岗岩岩体位于内蒙古东南部,华北板块与西伯利亚板块碰撞的缝合部位。岩体北西边缘与林西组地层的接触带发育道伦达坝中型铜–钨–锡多金属岩浆热液矿床。岩石地球化学研究表明,黑云母花岗岩为高钾钙碱性系列的过铝质花岗岩,Na2O+K2O含量为6.12%~9.31%,Al2O3含量为14.42%~15.59%,A/CNK值为1.09~1.22,δ均值为2.41,在花岗岩ACF图解中落入S型花岗岩区。全岩总稀土含量为102.65~237.92μg/g,低Sr(89.91~192.80μg/g)高Yb(2.17~3.46μg/g),δEu值为0.46~0.81,亏损Ba,Sr,Eu,富集La,显示S型花岗岩特征,在Rb–(Y+Nb)图解中显示后碰撞岩浆地球化学性质。利用LA-ICP-MS锆石U-Pb年代学方法,确定岩体形成年代为(273±7.7)~(278±4.3)Ma,在早二叠世形成于华北板块和西伯利亚板块碰撞后拉张伸展的构造背景。     

新疆尉犁蛭石矿蛭石的化学成分研究

对尉犁蛭石矿床的11个蛭石样品和6个金云母样品进行标准X—射线荧光分析得到其化学组成.一般地,蛭石化学组成为:SiO_2>42.49(％),MgO>27.15,Al_2O_3<14.K_2O+Na_2O<8.25;金云母化学组成为:SiO_2<42.01,MgO<26.75,Al_2O_3>14.K_2O+Na_2O>10.07.根据其成分分析结果计算蛭石和金云母的结构式,同时对其主要化学组成之间的关系进行讨论.在由金云母向蛭石的转变过程中,很明显地存在着元素的再分配,Al_2O_3和K_2O含量降低,SiO_2和MgO富集.     

Si/Al、Na/Al和H2O/Na2O摩尔比对无机铝硅酸盐涂层甲醛阻隔性能的影响

Wood-based panels containing urea-formaldehyde resin result in the long-term release of formaldehyde and threaten human health. In this study, inorganic aluminosilicate coatings prepared by combining metakaolin, silica fume, NaOH, and H₂O were applied to the surfaces of wood-based panels to obstruct formaldehyde release. The Si/Al, Na/Al, and H₂O/Na₂O molar ratios of the coatings were regulated to investigate their effects on the structure and formaldehyde-resistant barrier properties of coatings. Results showed that the cracks in the coatings gradually disappeared and the formaldehyde resistance rates of the barrier increased as the Si/Al molar ratio was increased from 1.6 to 2.2. This value also increased as the Na/Al molar ratio was increased from 0.9 to 1.2 because of the improvement of the degree of polymerization. As the H₂O/Na₂O molar ratio was increased from 12 to 15, the thickness of the dry film decreased gradually and led to the reduction in the formaldehyde resistance rate. When the Si/Al, Na/Al, and H₂O/Na₂O molar ratios were 2.2, 1.2, and 12, respectively, the inorganic aluminosilicate coating showed good performance as a formaldehyde-resistant barrier and its formaldehyde resistance rate could reach up to 83.2%.     

鱼台优质稻生产基地土壤地球化学元素调查

对山东省优质稻生产基地鱼台包括pH、水分、有机碳及N、P、F、V、Zn、Co、Mo、Mn、Se、B、Cr、Cd、Cu、Pb、Sb、Hg、As等在内的28种地球化学元素的含量及分布特征进行研究。研究结果表明,鱼台优质稻产区土壤中N、P、K、B、Mo、Mn、Se、Fe等有益元素富集,但As、Cd、Hg、Pb等重金属元素也有明显富集趋势。鱼台地区潮土与淹育水稻土的28种地球化学元素t-检验结果显示,As,B,Co,Cr,F,Mn,V,S,Al2O3,TFe2O3,MgO,CaO含量明显高于潮土,但是SiO2和Na2O的含量却明显低于潮土。淹育水稻土C(org)、水分含量也明显高于潮土。淹育水稻土有酸化现象。     

珠江口表层沉积物常量元素特征及其地球化学意义

 对珠江口348个站位表层沉积物中常量元素的地球化学特征进行了分析,探讨了其地球化学意义。结果表明,沉积物主要化学组成是SiO₂和Al₂ O₃,平均含量分别为60.1%和15.1%,且自河口向海方向SiO₂含量增大,Al₂ O₃含量减少。元素相关性及因子分析表明,沉积物主要由陆源和生物源碎屑沉积组成,包括SiO₂、Al₂O₃、P₂O₅、Fe₂O₃、MnO、TiO₂、K₂O 和CaO,是控制研究区沉积物化学成分的最主要因素;海源碎屑沉积包括Na₂O、MgO和K₂O,且K₂O具有陆源和海源碎屑双重特征.     

Effects of Si/Al,Na/Al and H_2O/Na_2O molar ratios on formaldehyde barrier properties of inorganic aluminosilicate coatings

Wood-based panels containing urea-formaldehyde resin result in the long-term release of formaldehyde and threaten human health.In this study, inorganic aluminosilicate coatings prepared by combining metakaolin, silica fume, NaOH, and H_2O were applied to the surfaces of wood-based panels to obstruct formaldehyde release. The Si/Al, Na/Al, and H_2O/Na_2O molar ratios of the coatings were regulated to investigate their effects on the structure and formaldehyde-resistant barrier properties of coatings. Results showed that the cracks in the coatings gradually disappeared and the formaldehyde resistance rates of the barrier increased as the Si/Al molar ratio was increased from 1.6 to 2.2. This value also increased as the Na/Al molar ratio was increased from 0.9 to 1.2 because of the improvement of the degree of polymerization. As the H_2O/Na_2O molar ratio was increased from 12 to 15, the thickness of the dry film decreased gradually and led to the reduction in the formaldehyde resistance rate. When the Si/Al, Na/Al, and H_2O/Na_2O molar ratios were 2.2, 1.2, and 12, respectively, the inorganic aluminosilicate coating showed good performance as a formaldehyde-resistant barrier and its formaldehyde resistance rate could reach up to 83.2%.     

2015—2021年采暖季华北平原污染过程气象条件分析

华北平原是中国三大平原之一，特殊的地理位置、较多的重工业企业及采暖季相对更高的污染排放，导致采暖季极易出现大范围、长时间的污染过程，PM_2.5浓度明显高于周边区域。为了更好地了解天气系统及气象要素对采暖季华北平原城市空气质量的影响，以北纬32°—40°、东经114°—120°华北平原地区50个城市为研究对象，分析2015—2021年采暖季(11月至次年3月)气象条件对华北平原采暖季大范围重污染过程的影响。研究表明，华北平原发生重污染时，高空500 hPa环流曲率减小，环流相对更加平直，垂直方向逆温出现概率增大，水平及垂直方向更加静稳，污染物扩散能力减弱，近地面山东中南部、河南异常偏南风导致区域升温、增湿，有利于颗粒物吸湿增长及二次转化，河北中西部异常偏东至东北风，导致污染物受太行山山脉影响，在太行山东侧堆积，易在山前形成大范围污染过程，且与山东中南部、河南的异常偏南风形成区域风场辐合，污染物扩散条件不利。分析2021年1月20日至28日一次污染过程发现，污染发生期间华北平原高空大气环流相对平直，地面以均压场控制为主，多静风辐合，湿度持续较大，整体污染扩散条件不利，...     

翡翠中绿辉石的矿物学特征

本文对翡翠中主要组成矿物绿辉石的矿物学特征进行了探讨。研究表明绿辉石的主要化学成份为ＳｉＯ２、Ａｌ２Ｏ３、Ｎａ２Ｏ,含有少量ＴＦｅＯ、ＭｇＯ、ＣａＯ、Ｃｒ２Ｏ３、ＭｎＯ、ＴｉＯ２、Ｋ２Ｏ。其绿辉石的化学成份介于硬玉与透辉石的二元混溶系列的中间态,具有Ｐ２或Ｐ２／ｎ型结构绿辉石的特征,这也得到了绿辉石的Ｘ射线粉晶衍射分析的证实。     

高铁铝土矿还原过程中的碱耗机理

采用化学分析,XRD,SEM和EDS等方法研究Na2O在产物中的分布及赋存状态,分析影响碱耗的因素和机理,有助于制定合理的工艺条件,降低成本和保护环境。从Na2CO3晶体的结构和能量变化角度研究熔融促进Na2O扩散的机理。研究结果表明:扩散损失的Na2O占总损失的87.76%,其中,43.60%属于固相扩散,56.40%属气相扩散。固相扩散量随物料与容器间的Na2O质量分数差的增加而显著提高,而气相扩散则不受到影响。还原性气氛增强、还原时间延长、温度升高以及物料含Fe2O3和Al2O3会导致Na2O扩散量增加。     

CaO-SiO_2-Na_2O-CaF_2-Al_2O_3-MgO渣系的粘度和结晶温度

采用CaOSiO2Na2OCaF2Al2O3MgO渣系,用差热分析仪测定熔渣的结晶温度,用粘度测定仪测定熔渣的粘度,研究结晶温度和粘度与碱度、w(Na2CO3)、w(CaF2)、w(Al2O3)和w(MgO)之间的关系,并得到相应的回归方程·利用这两个回归方程,可以预测连铸保护渣的结晶性能和粘性特征·化学成分通过改变粘度,来影响晶核形成速度和晶体成长速度,从而决定了熔渣的结晶性能·结晶温度随着粘度的减小而升高·渣系中只有MgO可以在减小粘度的同时降低结晶温度     

新疆柯柯亚一带晚石炭世硅质岩成因分析

新疆柯柯亚一带晚石炭世硅质岩分布极为广泛,通过野外地质填图及矿产调查过程中的详细观察和硅质岩岩石学特征分析,并根据硅质岩具有低SiO2、K2O、P2O5及HREE;高Al2O5、FeO、MgO、K2O＋Na2O、TiO2、∑EEE;SiO2／Al2O3、SiO2／（Na2O＋K2O）值分别为11～25和37～74;Fe／Ti值小于20、（Fe＋Mn）／Ti值小于15、Si／（Si＋Al＋Fe）值小于0．9等特征,认为这些硅质岩为火山成因。而且Th／Sc、Th／U和δCe等值及稀土配分曲线和TiO2-Al2O3图解也明确指示了硅质岩属火山成因类型。     

冀北崇礼红旗营子黑云斜长片麻岩的地质地球化学特征

基于当代红旗营子群是否应该解体这一观点,研究了崇礼红旗营子群中黑云斜长片麻岩的地质地球化学特征。研究表明原岩为泥质沉积岩,其特点为SiO2〉56％,Al2O3〉MgO,Na2O〉K2O,Na2O／（Na2O＋K2O）〉0．5,且其他氧化物与SiO2含量呈现出有规律的变化,随着岩石中SiO：含量的增加,TiO2,AL2O3,FeO,Fe2O3,MgO,CaO,Na2O和K2O呈明显下降趋势。稀土元素总量较低;轻重稀土分离程度较高,LREE／HREE的值为5．16～7．98,La。／Yb。的值为4．28～8．62,轻稀土富集,重稀土平坦分布,稀土配分曲线表现出中等程度的负Eu异常,δEu的值为0．73～0．83。稀土元素Ce基本无异常或略显负异常,表明其形成环境可能为一浅海相或边缘海或被陆地封闭海。     

历史时期华北平原的植被变迁

全新世中期由于全球处于冰后期的气候温暖期，所以我国华北平原北部分布着含有亚热带植物种属的暖温带落叶阔叶林，而该平原中南部则分布着北亚热带落叶阔叶与常绿阔叶混交林．到全新世晚期，即我国自西周以来的近三千年时期中，由于全球气候变得较前干冷，整个华北平原均变为暖温带落叶阔叶林区；随着人为活动的不断增强，人工栽培植被分布范围几经扩缩后，终于成为这一平原植被的主体，自然植被则几近消失．     

CuO-ZnO-CrOX-Al2O3催化剂前驱体组成及分解的热分析研究

采用热分析方法对CuO-ZnO-Al2O3和CuO-ZnO-CrOx-Al2O3催化剂的前驱体进行了研究，结果表明，当铬元素以硝酸铬引入时，Cr(NO3)3与碳酸钠反应生成Cr(OH)3沉淀，沉淀物的热分解产物为Cr2O3。当Cr元素采用Na2CrO4引入时，沉淀物的热分解产物为CrO3和CuO3。     

含SrO连铸保护渣熔点及粘度的研究

测试了ＳｒＯ－ＳｉＯ２－ＣａＯ－Ａｌ２Ｏ３（５％）－Ｎａ２Ｏ（１０％）－ＣａＦ２（１０％）六元渣系的熔点及粘度,绘制了等熔点曲线图及等粘度曲线图,得出了熔点及粘度与保护渣化学组成的数学关系式。通过对曲线图的分析,提出了含ＳｒＯ连铸保护渣的最佳组成范围。     

Comparative analysis of temperature and CO_2 fluxes for winter wheat in Tibetan Plain and North China Plain using the EMD method

Comparative study of spectral properties of temperature and CO2 fluxes measured by eddy covariance method at Yucheng (36°57'N, 116°36'E, 28 m a.s.l., in the North China Plain) and at Lhasa (29°41'N, 91°20'E, 3688 m a.s. 1., on the Tibetan Plateau) is described using the empirical mode decomposition (EMD) method. The main results are: (1) The intrinsic oscillation modes or intrinsic mode functions (IMFs) were extracted from data of temperature ( T) and CO2 fluxes (F) measured at Yucheng ( T1 and F1) and Lhasa ( T2 and F2) . (2) Hilbert transform was applied to these IMF components, then the Hubert-Huang spectra and the marginal spectra of these data were obtained. (3) Comparison of temperature and CO2 fluxes in North China Plain and on Tibetan Plain illustrated that the characteristic frequencies corresponding to T1, F1, T2 and F2 are 0.05 Hz, 0.03 Hz, 0.014 Hz and 0.005 Hz, respectively.     

碱性矿物质对煤灰熔融特性影响的研究

将K20和Na20添加剂按不同比例分别掺人两种煤灰中制成混合灰样，对混合灰样的熔融特性进行实验研究，采用X衍射图谱得到混合灰样不同温度的矿物组成，并利用三元系统相图进行分析．结果表明，在还原性气氛下，混合灰样灰熔点特性曲线与K2O-Al2O3-SiO2和Na2O-Al2O3-Sio2三元系统相图液相线温度曲线相似；在高温下混合灰样的矿物组成与三元系统相图的矿物组成基本一致．     

一种多次分相乳浊釉及其乳浊机理

研制了一种具有相当遮盖力和白度的新型分相乳浊釉，其主要成分为ＳｉＯ２，Ｂ２Ｏ３，Ａｌ２Ｏ３，ＣａＯ，ＭｇＯ，ＺｎＯ，Ｋ２Ｏ和Ｎａ２Ｏ通过电子显微镜观察，证实这种釉是分相乳浊釉，引用玻璃分相理论进行分析，探讨其产生分相现象的原因和其光学乳浊原理。     

Electrical conductivity optimization of the Na3AlF6-Al2O3-Sm2O3 molten salts system for Al-Sm intermediate binary ahoy production

Metal Sm has been widely used in making Al-Sm magnet alloy materials.Conventional distillation technology to produce Sm has the disadvantages of low productivity,high costs,and pollution generation.The objective of this study was to develop a molten salt electrolyte system to produce Al-Sm alloy directly,with focus on the electrical conductivity and optimal operating conditions to minimize the energy consumption.The continuously varying cell constant (CVCC) technique was used to measure the conductivity for the Na3AlF6-AlF3-LiF-MgF2-Al2O3-Sm2O3 electrolysis medium in the temperature range from 905 to 1055℃.The temperature (t) and the addition of Al2O3 (W(Al2O3)),Sm2O3 (W(Sm2O3)),and a combination of Al2O3 and Sm2O3 into the basic fluoride system were examined with respect to their effects on the conductivity (κ) and activation energy.The experimental results showed that the molten electrolyte conductivity increases with increasing temperature (t) and decreases with the addition of Al2O3 or Sm2O3 or both.We concluded that the optimal operation conditions for Al-Sm intermediate alloy production in the Na3AlF6-AlF3-LiF-MgF2-Al2O3-Sm2O3 system are W(Al2O3) + W(Sm2O3) =3wt％,W(Al2O3)∶ W(Sm2O3) =7∶3,and a temperature of 965 to 995℃,which results in satisfactory conductivity,low fluoride evaporation losses,and low energy consumption.