贫赤铁矿高压辊磨产品湿式预选研究

采用柱状磁介质研究了介质棒间隙、直径及背景磁场强度对贫赤铁矿高压辊磨产品湿式强磁预选效果的影响,并对磁场中不同直径的单矿物颗粒进行了受力分析.研究表明:减小介质棒间隙、增加介质棒直径和提高背景磁场强度均能降低预选尾矿的品位和产率,提高回收率.在同一背景磁场强度下,随着直径的增加,介质棒对粗颗粒的捕收磁力增加,对细颗粒的捕收磁力减小;对于实际连生体矿粒,考虑到矿粒重力和黏滞阻力的影响,增大介质棒直径在有利于粗矿粒捕收的同时并不影响细矿粒的捕收;减小介质棒直径有利于细矿粒的捕收,但对粗贫连生体矿粒的捕收能力下降.     

Magnetism parameters characteristics of drilling deposits in Jianghan Plain and indication for forming of the Yangtze River Three Gorges

The forming time of the Yangtze River Three Gorges is considered as one of keys in the research on the Yangtze River, also is one of the most disputed hotspots. In order to solve the difficult problem, the authors adopt the internationally recognized thoughts and methods of substance tracing from source to sink. The lithologic characteristics, magnetic parameters and magnetic mineral characteristics of deposits in 2 bores are analyzed, which are both sampled from the sedimentary center of the Jianghan Plain. The results are as follows： At about 110 m depth of the core, the contents of coarse materials and stable magnetic mineral both increase significantly. Meanwhile, the magnetic susceptibility of sediment, saturation isothermal remanent magnetization and magnetic susceptibility values of anhysteretic remanent magnetism increase suddenly, which all reflect that at about 110 m depth, the important adjustment has appeared in water system of the Jianghan Plain, and the sedimentary environment and material composition have changed greatly. And it may be the horizon where the Yangtze River Three Gorges formed, its forming time reflected by the paleomagnetic dating is between 1.17 and 1.12Ma B.P.     

矿山重金属污染土壤的磁化率特征及其意义——以广东大宝山多金属矿床为例

以广东省大宝山多金属矿区作为重金属污染土壤磁化率监测指标的探索研究。选择两个尾矿库、尾矿废水汇入河流的上游土壤、中游土壤以及未污染土壤分别进行磁化率测试。发现在尾矿库中,细粒沉积物中磁化率值高于粗粒,重金属污染土壤的磁化率显著高于未污染土壤。在污染河流沉积物和土壤剖面,随沉积物从土壤向底部粗砂过渡,下部粗粒沉积物的磁化率大于上部土壤,这一变化特征说明大宝山地区的原生污染可能更为严重。研究证明磁化率可以作为土壤重金属污染监测的替代性指标。     

Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting

Terrigenous components were separated from the bulk sediment of Core A7 from the Okinawa Trough and Core A37 from the Ryukru Trench and grain-size distributions of these sub-samples were analyzed.Based upon and analysis of the grain-size data of the two sedimentary sequences,grain-size populations are identified to be sensitive to sedimentary environmental changes.The modal values and size ranges of the two main grain-size populations in Core A7 are evidently different from those of Core A37,indicating the spatial variability of sediment sources and transport processes between the two places.The downcore variations in the content of the environmentally sensitive sgrain-size populations reveal that during the accumulation of sedimentary material the environment remained relatively stable at the site where Core A7 was collected,except for the apparent events for the formation of two turbidite layers and a volcanic ash layer.However,the sedimentary sequence of Core A37 shows six sedimentary cycles,indicating a highly variable sedimentary environment at this location.     

Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting

Grain-size data have been widely used to determine sediment transport patterns and to reconstruct the sedi-mentary environment. Because the natural occurring sediments deposited in the geologic periods and modern times are mostly mixtures of materials transported from multi-sources or/and by different sedimentary processes, the grain size of bulk samples is an incomplete, approxi-mate index for sedimentary environment changes[1,2]. Thus, further studies on the quantitative reconstruction of th…     

一种难选铁矿石磁选精矿直接反浮选的分散特征

介绍了一种处理难选铁矿石磁选精矿的直接反浮选工艺.采用XRD,SEM和EDS等手段对原矿、精矿和尾矿的形貌及矿物组成进行了表征,重点探讨了分离过程中矿物的分散特征,为含碳酸盐难选铁矿石磁选精矿的直接反浮选技术提供理论基础.研究结果表明,采用添加分散剂直接反浮选技术可以获得合格铁精矿;有用铁矿物和脉石矿物细颗粒无选择性粘附在有用铁矿物和脉石粗颗粒表面,是造成铁矿石分离困难的主要原因;分散剂的加入有利于颗粒分散,从而实现了有用铁矿物与脉石矿物的选择性分离.     

磁性参数的环境指示意义

介绍了岩石磁学研究中常用的能够指示环境变迁和气候变化的几种磁性参数及其组合。研究表明：磁化率是气候变化的代用指标之一，其值的高低反映气候的暖冷和沉积颗粒的细粗，用参数HSIRM，Bcr,HSIRM/k可以识别磁性矿物类型，较多磁铁矿的存在指示暖湿的沉积环境，反映沉积物颗粒细；而较多赤铁矿的存在则指示干冷的沉积环境，反映沉积物颗粒粗。HARM，Ber,HSIRM/k，S比(HSIRM-100mT/HSIRM)在环境监测中有重要的意义。     

Relationship between magnetic fabric parameters and dynamic characteristics of deposits in different environments

Comparison of magnetic fabric parameters of deposits in different modern sedimentary environments indicates that values ofP, F andL of eolian deposits are lower obviously than those of hydrogenic ones respectively. On relationship diagrams of magnetic fabric parameters, data points of eolian samples concentrated in limited area near origin of coordinates indicate that dynamic intensity is lower with less variation; while those of hydrogenic ones depart from origin of coordinates suggest higher intensity of sedimentary dynamics. Analyses of dynamic characteristics of different sedimentary environments indicate that values of magnetic fabric parameters of deposits are determined by dynamic types and characteristics of depositional processes. Magnetic fabric analyses of deposits are effective in determination of sedimentary environments.     

Magnetic separation studies on ferruginous chromite fine to enhance Cr:Fe ratio

The Cr:Fe ratio (chromium-to-iron mass ratio) of chromite affects the production of chrome-based ferroalloys. Although the literature contains numerous reports related to the magnetic separation of different minerals, limited work concerning the application of magnetic separation to fine chromite from the Sukinda region of India to enhance its Cr:Fe ratio has been reported. In the present investigation, magnetic separation and mineralogical characterization studies of chromite fines were conducted to enhance the Cr:Fe ratio. Characterization studies included particle size and chemical analyses, X-ray diffraction analysis, automated mineral analysis, sink-and-float studies, and magnetic susceptibility measurements, whereas magnetic separation was investigated using a rare earth drum magnetic separator, a rare earth roll magnetic separator, an induced roll magnetic separator, and a wet high-intensity magnetic separator. The fine chromite was observed to be upgraded to a Cr:Fe ratio of 2.2 with a yield of 55.7% through the use of an induced roll magnetic separator and a feed material with a Cr:Fe ratio of 1.6.     

福州盆地不同土地利用方式下土壤磁化率特征

福州盆地不同土地利用方式下的土壤磁化率研究表明,福州城市土壤表层土的磁化率平均值为230×10-8m3/kg,频率磁化率均值仅为0.74%,表现出磁化率高,频率磁化率低的特征,表明土壤中有较多人类活动产生的粗粒磁性矿物颗粒物输入.工业区、商业区、生活文化区和城市风景区的磁化率平均含量分别为326×10-8,297×10-8,156×10-8,113×10-8m3/kg,表现出工业区>商业区≥生活文化区>城市风景区的特征,土壤磁化率影响因素呈现多元性特征.城郊农业用地的磁化率相对城市用地的磁化率低,表层土壤的平均值为106×10-8m3/kg,与20cm以下的磁背景值较为接近,并且随深度变化不大,表明农业用地化肥和农药的过量使用并不严重,重金属未在土壤中大量累积,不同用地类型的磁化率特征规律为果园土>林地土>菜园土>水稻土.     

硫化矿浮选混合精矿振动高梯度磁选的研究

本文阐述硫化矿浮选混合精矿振动高梯度磁分离的研究,其要点是:a.为消除非磁性矿粒的机械夹杂,采用磁介质振动的振动高梯度磁选法;b.为了消除微细异质矿粒凝聚,矿浆入选前进行脱药和充分分散。     

Thermally unstable maghaemite and its palaeoclimatic significance in Chinese loess

Magnetite and maghaemite are the two main contributors to magnetic susceptibility in the Chinese loess/palaeosol sequence. Due to the close similarity in physical properties, early investigators treated them together as "magnetite". Utilising the property of thermally instability of maghaemite, we have been able to separate it from magnetite in loess and palaeosol samples from the upper parts of the Xifeng and Luochuan sections on the central Chinese Loess Plateau and compare its variation with depth and horizon. Our results indicate that thermally unstable maghaemite is relatively enriched in both 1) weakly weathered loess units and 2) towards the west, the direction of dust supply, suggesting that maghaemite is at least partially (coarse grains) of detrital aeolian origin while some pedogenic maghaemite (extra fine grains) occurs in the palaeosols. The physical meaning of magnetic susceptibility, therefore, needs to be reconsidered as a synthetic indicator reflecting the palaeoenvironment for both source area and deposition area. Thermally unstable goethite is a minor magnetic component of palaeosol samples, but it may play a significant role in determining characteristic magnetic remanence of weakly weathered loess samples, especially when one applies alternating-field cleaning.     

河北三河上更新统——全新统磁化率变化旋回分析

为了获取河北三河地区上更新统-全新统古气候和古环境变化,在该区实测一地层剖面,采集磁化率样品进行测试,以磁化率变化为沉积环境代用指标,在前人研究确立的地质年代框架下,运用频谱分析、演化谱分析等方法对地层垂向磁化率变化进行旋回分析。结果表明研究区冲积沉积中存在23ka的岁差尺度旋回,由于剖面较短未识别出更长周期的斜率和偏心率旋回。根据分析结果计算出剖面沉积时限为4-45ka,属于晚更新世晚期至全新世早期河流砂坝和泛滥平原沉积,平均沉积速率为24cm/ka。磁化率的变化与粒度变化具有正相关性,粗粒沉积磁化率较高、细粒沉积磁化率较低;磁化率的变化受岁差驱动气候变化影响,岁差高值时大气降水对河流补给增多,陆源碎屑增多提高了沉积物中磁性矿物的含量,反之,则磁性矿物少,磁化率低。岁差驱动气候变化在河流冲积物中的发现,为河流冲积沉积天文驱动气候变化研究提供参考依据,为第四纪冲积沉积和地质事件研究提供新的年龄约束手段。     

海砂矿球磨微观解离与细粒级磁选受力分析

为拓宽铁矿石来源,提高海砂品位以应用于长流程炼铁系统,对一种印尼海砂矿进行了球磨磁选实验,并利用X射线衍射(XRD)、扫描电镜(SEM)以及激光粒度分析(LPSA)等方法,研究了其在不同球磨阶段的微观解离特点、粒度与磁感应强度对精矿品位与回收率的影响以及细粒级下磁选过程中的受力机理.结果表明:球磨至一定阶段后,矿石粒度已较小,连生体基本以包裹体形式存在,很难继续解离,故此时继续降低矿石粒度对精矿品位的提升意义不大;另外,当矿石较细时,水阻力将成为磁选过程中的主要作用力,细粒级矿粒将不能到达磁鼓表面,故此时精矿回收率较低.     

The characteristics and significance of magnetic fabrics of muddy tidal flat

Conclusions The magnetic fabric parameterK of the tidal flat with the same material sources in the wide coastal zone is a high-resolution indicator for the recognization of sedimentary dynamically active zones of tidal flat, which indicates that the magnetic fabric method could be widely applied to the study of sedimentology, comparative sedimentology and sedimentary dynamics. The high and low values of magnetic fabric parametersq, F andL occur alternately, which indicates the presence of microbedding structures, such as small-scale sequences consisting of a single muddy layer and a sandy layer and small-scale sequence series. This indicates that the magnetic fabric analysis could be a new effective method for the study of sedimentary microstructure sequence series of tidal flats. The statistical results of parametersK, L, F andq have revealed that correlations between the variations of magnetic fabric parameters of sediments and the sedimentary dynamic environments are a new way for the studies of tidal flat types and sedimentation.     

利用FEMLAB模拟微电磁石的磁场区域

利用FEMLAB软件模拟出在2D和3D的情况下微电磁石的电磁感应对磁场强度的影响.因为在3D界面下不能完全将实际模型重建,采用缩小实体的方法,将缩小后的模型在2D环境下模拟,可以显示出与大空间范围构造相似的仿真结果.3D仿真结果显示的大体结构及空间范围的情况与2D仿真结果大致相同,且3D仿真结果的误差在正常情况下至少为10%,因此3D与2D仿真环境下的磁体结构是可以比较的.     

洛阳二里头遗址南沉积剖面的粒度和磁化率分析

洛阳盆地内二里头遗址南沉积剖面位于遗址所在二级阶地的前缘,属于河流堆积。对剖面的沉积物样品做了光释光测年及磁化率、粒度分析。结果表明:剖面沉积年代大致在2000~5000 aBP之间。剖面下部(113~123 cm)沉积物粒度较细,磁化率偏高,粒度曲线反映水流较弱的泛滥平原沉积环境,属河漫滩堆积;中部(90~113 cm)粒度较粗,磁化率较低,粒度曲线反映水动力较强的边滩–漫滩沉积环境,属河床边滩堆积;上部(0~90 cm)粒度变细,磁化率升高,粒度曲线反映水动力条件较弱的泛滥平原沉积环境,属河漫滩堆积。其中沿水平方向可见剖面中部的河床边滩堆积直接覆盖在二级阶地顶面的龙山时期灰坑之上,由此可以确认剖面中部地层记录了一场漫上了河流阶地的特大洪水事件,这一记录与孢粉分析得到的气候变化过程具有明显的相关性。4000 aBP前后异常洪水的出现和大洪水前后河流过程的变化,可能是对4200 aBP全球性气候异常事件的区域响应,对我国最早的都邑——二里头城址的选址有重要的影响。     

级配离析沥青混合料性能的试验研究

通过室内试验，分析混合料级配离析状态和离析程度对沥青混合料体积参数、路用性能和力学性能的影响．结果表明，在不同离析程度下，粗集料离析对沥青混合料性能的影响大于细集料离析的影响．在粗集料集中区域，由于空隙率过大，吸水性和渗水性增大，对沥青混合料的水稳定性极为不利，还将大幅度降低沥青混合料的疲劳寿命和强度．在细集料集中区域，压实空隙率过小，虽然对沥青混合料的水稳定性和抗疲劳性能无不利影响，但将使沥青混合料的抗车辙能力和抗滑性显著降低．     

用磁选柱精选齐大山选矿厂磁选中矿的试验研究

介绍了用磁选柱选别齐大山选矿厂磁选中矿的实验室研究。试验证明：磁选柱可有效地将磁铁矿连生体颗粒从磁铁矿精矿中分选出来,从而获得高品位的铁精矿。     

雨季广州大气中的硝酸盐粒子

对雨季广州大气中的硝酸盐粒子进行了两年的观察 .粒子被分为两部分 :粗大粒子 (r >1.0 μm )和微小粒子 (r≤ 1.0 μm ) .用离子色谱对粒子总量进行了总体分析 ,用复合薄膜法和X_射线分析法对单个粒子进行了分析 .总体分析结果表明 ,粗大粒子中的NO- 3、Ca2 +和Na+含量比微小粒子中的高 .对单个粒子的分析发现 ,硝酸盐粒子不仅存在于粗大粒子中 ,而且也存在于微小粒子中 ,证明硝酸能凝结在海盐上形成粗大硝酸盐粒子 ,粗大硝酸盐粒子有可能起着最终消除广州大气中硝酸的作用 .