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Boron Enrichment in Salinized Lacustrine Organic-Rich Shale of the Paleogene Biyang Depression, East China: Occurrence and Geological Controlling Factors 中国东部古近纪毕阳凹陷盐渍化湖相富有机质页岩中硼的富集:发生与地质控制因素
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-09-03 DOI: 10.3390/min14090904
Yu Song, Paerzhana Paerhati, Shilin Xu, Bo Gao, Shu Jiang, Shuifu Li, Yuchen Wang, Hecun Lv
Although boron (B) is widely applied as a paleosalinity indicator for ancient lakes, the occurrence and geological controls of B enrichment in salinized lacustrine organic-rich shale (SLORS) are poorly understood. This study addresses this issue by comparing the mineral and element compositions of high-boron shale (HBS) and low-boron shale (LBS) from the Paleogene Biyang Depression, using integrated XRD, XRF, and ICP-MS analyses. The mineral composition of HBS is dominated by illite, whereas LBS primarily consists of albite; both are of detrital origin. Compared to the element composition of UCC, HBS is extremely enriched in Mo and W, whereas LBS is extremely enriched in W and U. Boron is positively correlated with Al2O3 and negatively correlated with Na2O, suggesting that B primarily occurs in illite. An enhanced extent of chemical weathering prevailed during the deposition of HBS, providing a greater supply of illite to the basin. Higher pH levels and greater reduction during HBS deposition encouraged illite absorption of B, ultimately leading to B enrichment in shale. Our findings suggest that pH and redox conditions, as well as the mineral compositions of shale, should be fully considered during the application of B and related ratios as paleosalinity indicators.
尽管硼(B)被广泛用作古湖泊的古盐度指标,但人们对盐渍化湖沼富含有机质页岩(SLORS)中硼富集的发生和地质控制却知之甚少。针对这一问题,本研究采用 XRD、XRF 和 ICP-MS 综合分析方法,比较了古近纪毕阳凹陷中高硼页岩(HBS)和低硼页岩(LBS)的矿物和元素组成。HBS 的矿物组成以伊利石为主,而 LBS 则主要由白云石组成,两者均为碎屑岩。硼与 Al2O3 呈正相关,与 Na2O 呈负相关,表明硼主要存在于伊利石中。在 HBS 沉积过程中,化学风化程度加剧,为盆地提供了更多的伊利石。在 HBS 沉积过程中,较高的 pH 值和较强的还原性促进了伊利石对硼的吸收,最终导致页岩中硼的富集。我们的研究结果表明,在应用硼和相关比率作为古盐度指标时,应充分考虑页岩的 pH 值和氧化还原条件以及矿物成分。
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引用次数: 0
Flotation Tailings from Cu-Au Mining (Bor, Serbia) as a Potential Secondary Raw Material for Valuable Metals Recovery 将铜金矿浮选尾矿(塞尔维亚博尔)作为有价金属回收的潜在二次原材料
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-09-03 DOI: 10.3390/min14090905
Vanja Trifunović, Ljiljana Avramović, Dragana Božić, Marija Jonović, Dragan Šabaz, Dejan Bugarin
The increased exploitation of ores leads to the generation of mining waste, which has a negative impact on the environment and human health. For this reason, it is necessary to take care of it in an adequate way by applying some of the possible treatments. In addition to protecting the environment by applying appropriate treatment, there is also the possibility of making a profit by valorizing useful elements from mining waste. In order to choose the most adequate treatment, it is necessary to perform the characterization of mining waste. This paper contains a detailed characterization of the flotation tailings deposited at the Old Flotation Tailings in eastern Serbia, originating from copper ore processing. Characterization includes physico-chemical analysis, polarizing microscope analysis, X-ray Diffraction analysis (XRD) and Scanning Electron Microscopy with Energy Dispersive Spectroscopy (SEM-EDS) analysis analysis. The obtained results indicate that the investigated flotation tailings can be used as a secondary raw material for metal recovery, in this case primarily copper (whose content is about 0.24%), gold (with a content of about 0.43 ppm) and silver (with a content of about 1.7 ppm). Considering that the content of valuable elements is quite low, it is suggested to apply hydrometallurgical treatment for their recovery.
矿石开采量的增加导致采矿废物的产生,对环境和人类健康造成负面影响。因此,有必要通过一些可能的处理方法对其进行适当的处理。除了通过适当的处理方法保护环境之外,还可以通过对采矿废料中的有用成分进行估值来获得利润。为了选择最适当的处理方法,有必要对采矿废料进行特征描述。本文详细描述了沉积在塞尔维亚东部老浮选尾矿的浮选尾矿的特征,这些尾矿源自铜矿加工。特性分析包括物理化学分析、偏光显微镜分析、X 射线衍射分析 (XRD) 和扫描电子显微镜与能量色散光谱分析 (SEM-EDS)。所得结果表明,所调查的浮选尾矿可用作金属回收的二次原料,在这种情况下,主要是铜(含量约为 0.24%)、金(含量约为 0.43 ppm)和银(含量约为 1.7 ppm)。考虑到有价元素的含量很低,建议采用湿法冶金处理来回收这些元素。
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引用次数: 0
A New Mineral Calcioveatchite, SrCaB11O16(OH)5·H2O, and the Veatchite–Calcioveatchite Isomorphous Series 一种新矿物钙钛矿、SrCaB11O16(OH)5-H2O 和 Veatchite-Calcioveatchite 同构系列
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-09-02 DOI: 10.3390/min14090901
Igor V. Pekov, Natalia V. Zubkova, Vladimir N. Apollonov, Vasiliy O. Yapaskupt, Sergey N. Britvin, Dmitry Yu. Pushcharovsky
The new mineral calcioveatchite, ideally SrCaB11O16(OH)5·H2O, is a Ca-Sr-ordered analogue of veatchite. It was found at the Nepskoe potassium salt deposit, Irkutsk Oblast, Siberia, Russia in halite-sylvite and sylvite-carnallite rocks, with boracite, hilgardite, kurgantaite, hydroboracite, volkovskite, veatchite, anhydrite, magnesite, and quartz. Calcioveatchite forms prismatic or tabular crystals up to 1 × 1.5 × 3 mm3 and crystal clusters up to 3 mm across. It is transparent and colourless with vitreous lustre. Calcioveatchite is brittle, cleavage is perfect on {010}, the Mohs’ hardness is ca 2, Dmeas is 2.58(1), and Dcalc is 2.567 g cm−3. Calcioveatchite is optically biaxial (+), α = 1.543(2), β = 1.550(5), γ = 1.626(2), 2Vmeas = 30(10)°, and 2Vcalc = 35°. The average chemical composition (wt.%, electron microprobe, H2O calculated by stoichiometry) is: CaO 7.05, SrO 20.70, B2O3 61.96, H2O 10.22, and total 99.93. The empirical formula, calculated based on 22 O apfu = O16(OH)5(H2O) pfu, is Sr1.23Ca0.78B10.99O16(OH)5·H2O. Calcioveatchite is monoclinic, space group P21, a = 6.7030(3), b = 20.6438(9), c = 6.6056(3) Å, β = 119.153(7)°, V = 798.26(8) Å3, and Z = 2. Polytype: 1M. The strongest reflections of the powder XRD pattern [d,Å(I,%)(hkl)] are: 10.35(100)(020), 5.633(12)(110), 5.092(10)(120), 3.447(14)(060), 3.362(13)(101, 051), 3.309(38)(–102), 2.862(10)(012), and 2.585(19)(080). The crystal structure was solved based on single-crystal XRD data, R1 = 0.0420. Calcioveatchite (calcioveatchite-1M) is an isostructural analogue of veatchite-1M with the 11-fold cation polyhedron occupied mainly by Sr [Sr0.902(8)Ca0.098(8)] whereas the 10-fold polyhedron is Ca dominant [Ca0.686(7)Sr0.314(7)]. The chemical composition of veatchite from five localities in Russia (Nepskoe), Kazakhstan (Shoktybay and Chelkar in the North Caspian Region), and the USA (Tick Canyon and Billie Mine in California) was studied, and it is shown to exist in nature as a continuous, almost complete isomorphous series which extends from Ca-free veatchite, Sr2B11O16(OH)5·H2O, to calcioveatchite with the composition Sr1.14Ca0.87B10.99O16(OH)5·H2O.
新矿物钙钛矿(理想状态下为 SrCaB11O16(OH)5-H2O)是一种钙-锶有序的钒钛矿类似物。它是在俄罗斯西伯利亚伊尔库茨克州的 Nepskoe 钾盐矿床发现的,矿床位于光卤石-钠长石和钠长石-钙长石岩石中,并与硼酸盐岩、蛭石、库尔干沸石、氢硼酸盐岩、volkovskite、钒钛铁矿、无水石膏、菱镁矿和石英一起存在。钙钒铁矿形成棱柱形或片状晶体,大小可达 1 × 1.5 × 3 立方毫米,晶体簇直径可达 3 毫米。它透明无色,具有玻璃光泽。钙橄榄石较脆,{010}上的裂隙完美,莫氏硬度约为 2,Dmeas 为 2.58(1),Dcalc 为 2.567 g cm-3。钙钛矿具有光学双轴性 (+),α = 1.543(2),β = 1.550(5),γ = 1.626(2),2Vmeas = 30(10)°,2Vcalc = 35°。平均化学成分(重量百分比,电子显微探针,按化学计量学计算的 H2O)为CaO 7.05,SrO 20.70,B2O3 61.96,H2O 10.22,总计 99.93。根据 22 O apfu = O16(OH)5(H2O) pfu 计算得出的经验公式为:Sr1.23Ca0.78B10.99O16(OH)5-H2O。钙钛矿为单斜晶系,空间群为 P21,a = 6.7030(3),b = 20.6438(9),c = 6.6056(3)埃,β = 119.153(7)°,V = 798.26(8)埃3,Z = 2。聚类:1M.粉末 X 射线衍射图[d,Å(I,%)(hkl)]的最强反射是10.35(100)(020)、5.633(12)(110)、5.092(10)(120)、3.447(14)(060)、3.362(13)(101, 051)、3.309(38)(-102)、2.862(10)(012) 和 2.585(19)(080)。晶体结构是根据单晶 XRD 数据 R1 = 0.0420 解得的。钙钒钛铁矿(calcioveatchite-1M)是钒钛铁矿-1M 的等结构类似物,其 11 倍阳离子多面体主要由锶占据[Sr0.902(8)Ca0.098(8)],而 10 倍阳离子多面体则以钙为主[Ca0.686(7)Sr0.314(7)]。研究了来自俄罗斯(Nepskoe)、哈萨克斯坦(北里海地区的 Shoktybay 和 Chelkar)和美国(加利福尼亚州的 Tick Canyon 和 Billie 矿)五个地方的钒钛铁矿的化学成分,结果表明其在自然界中以连续、几乎完整的同构系列存在,从无钙钒钛铁矿(Sr2B11O16(OH)5-H2O)延伸到钙钒钛铁矿(Sr1.14Ca0.87B10.99O16(OH)5·H2O.
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引用次数: 0
Open-Circuit Technology of Zinc Oxide Ore Flotation with Ternary Collector and Its Adsorption Characteristics on Smithsonite Surface 三元捕收剂浮选氧化锌矿石的开路技术及其在史密松岩表面的吸附特性
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-09-02 DOI: 10.3390/min14090902
Zhiwei Li, Qicheng Feng, Qian Zhang, Shuming Wen
The sulfidization-amine flotation method is commonly used for the beneficiation of zinc oxide ores. Lanping zinc oxide ores contains 8.40% zinc, with the main mineral being smithsonite; additionally, they have a high mud content. Conventional sulfidization–ammonium flotation presents a low flotation index and unsatisfactory flotation froth. A new open-circuit technology is employed to treat Lanping zinc oxide ores, where Na2S, KG-248, and dodecyl amine + sodium isoamyl xanthate + ammonium dibutyl dithiophosphate are used as the regulator, depressant, and ternary collector, respectively. Consequently, the flotation indices for the zinc grade and recovery are 28.71% and 86.24%, respectively, and the flotation froth becomes more stable. Subsequently, the flotation behavior and adsorption mechanism of smithsonite with a ternary collector are investigated. The flotation recovery of smithsonite increases to 94.40% after treatment with the ternary collector. Surface-analysis results indicate that the ternary collector can synergistically adsorb onto the sulfidized smithsonite surface to enhance its hydrophobicity, thus increasing the floatability of smithsonite. Meanwhile, the total consumption of the collector in the ternary-collector system is lower than that in the binary- or unitary-collector system.
硫化-胺浮选法常用于氧化锌矿石的选矿。兰坪氧化锌矿石含锌量为 8.40%,主要矿物为铁闪锌矿,含泥量较高。传统的硫化-铵浮选法浮选指数低,浮选泡沫不理想。在处理兰坪氧化锌矿石时,采用了一种新的开路技术,分别使用 Na2S、KG-248 和十二烷基胺 + 异戊基黄原酸钠 + 二丁基二硫代磷酸铵作为调节剂、抑制剂和三元捕收剂。结果,锌品位和回收率的浮选指数分别为 28.71% 和 86.24%,浮选泡沫变得更加稳定。随后,研究了三元捕收剂对铁闪锌矿的浮选行为和吸附机理。经三元捕收剂处理后,铁石棉的浮选回收率提高到 94.40%。表面分析结果表明,三元捕收剂能协同吸附在硫化的铁石棉表面,增强其疏水性,从而提高铁石棉的可浮性。同时,三元收集器系统中收集器的总消耗量低于二元或单元收集器系统。
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引用次数: 0
Dissolution Mechanisms and Surface Charge of Clay Mineral Nanoparticles: Insights from Kinetic Monte Carlo Simulations 粘土矿物纳米颗粒的溶解机制和表面电荷:蒙特卡洛动力学模拟的启示
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-09-02 DOI: 10.3390/min14090900
Inna Kurganskaya
The widespread use of clay minerals and clays in environmental engineering, industry, medicine, and cosmetics largely stems from their adsorption properties and surface charge, as well as their ability to react with water. The dissolution and growth of minerals as a function of pH are closely related to acid–base reactions at their surface sites and their surface charge. The vivid tapestry of different types of surface sites across different types of clay minerals generates difficulties in experimental studies of structure–property relationships. The aim of this paper is to demonstrate how a mesoscale stochastic kinetic Monte Carlo (kMC) approach altogether with atomistic acid-base models and empirical data can be used for understanding the mechanisms of dissolution and surface charge behavior of clay minerals. The surface charge is modeled based on equilibrium equations for de/protonated site populations, which are defined by the pH and site-specific acidity constants (pKas). Lowered activation energy barriers for these sites in de/protonated states introduce pH-dependent effects into the dissolution kinetics. The V-shaped curve observed in laboratory experiments is reproduced with the new kMC model. A generic rate law for clay mineral dissolution as a function of pH is derived from this study. Thus, the kMC approach can be used as a hypothesis-testing tool for the verification of acid–base models for clay and other minerals and their influence on the kinetics of mineral dissolution and growth.
粘土矿物和粘土在环境工程、工业、医药和化妆品中的广泛应用主要源于它们的吸附特性和表面电荷,以及与水发生反应的能力。矿物的溶解和生长随 pH 值的变化而变化,这与其表面部位的酸碱反应和表面电荷密切相关。不同类型的粘土矿物具有不同类型的表面位点,这给结构-性质关系的实验研究带来了困难。本文旨在展示如何利用中尺度随机动力学蒙特卡洛(kMC)方法,结合原子论酸碱模型和经验数据来理解粘土矿物的溶解机制和表面电荷行为。表面电荷的建模基于去质子化/质子化位点群的平衡方程,这些位点群由 pH 值和特定位点酸度常数(pKas)定义。在脱/质子化状态下,这些位点的活化能垒降低,从而在溶解动力学中引入了与 pH 值相关的效应。新的 kMC 模型再现了实验室实验中观察到的 V 型曲线。这项研究得出了粘土矿物溶解随 pH 值变化的通用速率定律。因此,kMC 方法可作为一种假设检验工具,用于验证粘土和其他矿物的酸碱模型及其对矿物溶解和生长动力学的影响。
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引用次数: 0
Sandstone Porosity Evolution and Reservoir Formation Models of the Paleogene Huagang Formation in Yuquan Structure of West Lake Sag, East China Sea Basin 东海盆地西湖相玉泉构造古近系华岗地层砂岩孔隙度演化及储层形成模型
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-08-31 DOI: 10.3390/min14090899
Yonghuang Cai, Zhengxiang Lv, Yuanhua Qing, Cheng Xie, Bingjie Cheng, Zheyuan Liao, Bing Xu
The West Lake Sag is abundant in oil and gas reserves, primarily in the Huagang Formation reservoir which serves as the primary source of production. The level of exploration is rather high, but there are still some unresolved issues, such as an unclear understanding of pore evolution features and reservoir growth mode. To tackle the aforementioned problems, this study employs optical microscopic examination, scanning electron microscope analysis, inclusion analysis, isotope analysis, X-ray diffraction analysis, and other techniques to elucidate the primary factors governing reservoir development and establish an analytical model regarding the cause of the sandstone reservoir. The results are as follows: (1) The sandstone reservoirs of the Huagang Formation of the Yuquan (abbreviated to YQ) Structure are now in the mesomorphic A stage as a whole, and minerals such as 4-phase authigenic quartz, 2-phase illite, 2-phase chlorite, 1-phase kaolinite, 1-phase ammonite mixing layer and 2-phase carbonate were formed during the diagenesis. (2) Feldspar and carbonate solution pores make up the majority of the reservoir space. About 10% of the porosity is made up of carbonate solution pores, which are the most prevalent reservoir space. Carbonate solution pores are primarily made up of metasomatic carbonate solution pores and cemented carbonate solution pores. Feldspar solution pores come next, contributing roughly 6.2% of the porosity. At 1.8%, residual intergranular holes are the least common. (3) The four main processes listed below are responsible for the creation of pores in the sandstone of the Huagang creation. The early carbonate cements resist the destruction of mechanical compaction and effectively preserve intergranular volume. The high content of feldspar provided a material basis for later dissolution. Early chlorite surrounding the edges of particles reduced the damage of authigenic minerals to porosity. The faults and cracks formed by the later structural inversion connected to the acidic water in the atmosphere, causing the dissolution of carbonate minerals and feldspar in the sandstone of the Huagang Formation. (4) Carbonate dissolution + feldspar dissolution type, carbonate dissolution type, and feldspar dissolution type are the three main types of reservoir formation in the Huagang Formation; the first two types mainly develop in the Upper Huagang Formation, while the latter mainly develops in the lower part of the Huagang Formation. The research results are conducive to the establishment of a geological prediction model for high-quality reservoirs of different geneses in the Huagang Formation and promote the exploration process of deep-seated hydrocarbons in the West Lake Sag.
西湖相思油气储量丰富,主要分布在华岗地层储层中,该储层是西湖相思的主要产地。虽然勘探水平较高,但仍存在一些尚未解决的问题,如对孔隙演化特征和储层生长模式的认识不清。针对上述问题,本研究采用光学显微镜检查、扫描电子显微镜分析、包裹体分析、同位素分析、X 射线衍射分析等技术,阐明了储层发育的主要因素,建立了砂岩储层成因分析模型。研究结果如下(1)玉泉(简称玉泉)构造华岗层砂岩储层目前整体处于中生A期,成岩过程中形成了4相自生石英、2相伊利石、2相绿泥石、1相高岭石、1相芒硝混合层和2相碳酸盐等矿物。(2)长石和碳酸盐溶液孔隙占储层空间的绝大部分。约10%的孔隙度由碳酸盐溶液孔隙构成,这是最普遍的储层空间。碳酸盐溶液孔隙主要由变质碳酸盐溶液孔隙和胶结碳酸盐溶液孔隙组成。其次是长石溶蚀孔隙,约占孔隙度的 6.2%。残余晶间孔最少,仅占 1.8%。(3)下面列出的四个主要过程是造成花岗岩砂岩孔隙形成的原因。早期的碳酸盐胶结物能抵抗机械压实的破坏,有效地保持晶间体积。长石的高含量为后来的溶解提供了物质基础。颗粒边缘环绕的早期绿泥石减少了自生矿物对孔隙度的破坏。后期构造反转形成的断层和裂隙与大气中的酸性水相连,导致华岗地层砂岩中碳酸盐矿物和长石的溶解。(4)碳酸盐溶解+长石溶解型、碳酸盐溶解型、长石溶解型是华岗地层储层形成的三种主要类型,前两种类型主要发育在华岗地层上部,后者主要发育在华岗地层下部。研究成果有利于建立花岗地层不同成因优质储层的地质预测模型,推动西湖相深层油气勘探进程。
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引用次数: 0
Research on Prediction of Ash Content in Flotation-Recovered Clean Coal Based on NRBO-CNN-LSTM 基于 NRBO-CNN-LSTM 的浮选回收洁净煤灰分预测研究
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-08-30 DOI: 10.3390/min14090894
Yujiao Li, Haizeng Liu, Fucheng Lu
Ash content is an important production indicator of flotation performance, reflecting the current operating conditions of the flotation system and the recovery rate of clean coal. It also holds significant importance for the intelligent control of flotation. In recent years, the development of machine vision and deep learning has made it possible to detect ash content in flotation-recovered clean coal. Therefore, a prediction method for ash content in flotation-recovered clean coal based on image processing of the surface characteristics of flotation froth is studied. A convolutional neural network –long short-term memory (CNN-LSTM) model optimized by Newton–Raphson is proposed for predicting the ash content of flotation froth. Initially, the collected flotation froth video is preprocessed to extract the feature dataset of flotation froth images. Subsequently, a hybrid CNN-LSTM network architecture is constructed. Convolutional neural networks are employed to extract image features, while long short-term memory networks capture time series information, enabling the prediction of ash content. Experimental results indicate that the prediction accuracy on the training set achieves an R value of 0.9958, mean squared error (MSE) of 0.0012, root mean square error (RMSE) of 0.0346, and mean absolute error (MAE) of 0.0251. On the test set, the prediction accuracy attains an R value of 0.9726, MSE of 0.0028, RMSE of 0.0530, and MAE of 0.0415. The proposed model effectively extracts flotation froth features and accurately predicts ash content. This study provides a new approach for the intelligent control of the flotation process and holds broad application prospects.
灰分是浮选性能的重要生产指标,反映了浮选系统当前的运行状况和精煤回收率。它对于浮选的智能控制也具有重要意义。近年来,机器视觉和深度学习的发展使得浮选回收精煤中灰分的检测成为可能。因此,本文研究了一种基于浮选泡沫表面特征图像处理的浮选回收精煤灰分预测方法。提出了一种经牛顿-拉斐逊优化的卷积神经网络-长短期记忆(CNN-LSTM)模型,用于预测浮选浮沫的灰分含量。首先,对采集的浮选泡沫视频进行预处理,提取浮选泡沫图像的特征数据集。随后,构建混合 CNN-LSTM 网络架构。卷积神经网络用于提取图像特征,而长短期记忆网络则用于捕捉时间序列信息,从而预测灰分含量。实验结果表明,训练集上的预测精度 R 值为 0.9958,均方误差 (MSE) 为 0.0012,均方根误差 (RMSE) 为 0.0346,平均绝对误差 (MAE) 为 0.0251。在测试集上,预测精度的 R 值为 0.9726,MSE 为 0.0028,RMSE 为 0.0530,MAE 为 0.0415。所提出的模型能有效提取浮选矿沫特征,准确预测灰分含量。这项研究为浮选过程的智能控制提供了一种新方法,具有广阔的应用前景。
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引用次数: 0
Assessing Mining Performance Indicators in Relation to the SDGs: Development of a Guided Methodology and Its Application in an Iron Ore Mine 评估与可持续发展目标相关的采矿绩效指标:开发指导方法及其在铁矿中的应用
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-08-30 DOI: 10.3390/min14090887
Rhaymá do Carmo Silva, Anna Luiza Marques Ayres da Silva
The concept of sustainability has gained significant recognition across all industrial sectors, particularly in response to the potential global environmental crisis. In mining, sustainability ensures responsible operations by addressing environmental, social, and economic aspects. Performance indicators, categorized into environmental, social, economic, and governance groups, are monitored to oversee these aspects. In 2015, the UN established 17 Sustainable Development Goals (SDGs) as a global agenda for achieving equitable economic and social development. This study presents a methodology to evaluate performance indicators in an iron ore mine in southeast Pará, Brazil, to understand whether and how these indicators guide the mine’s operations toward fulfilling the SDGs. This study was based on the application of a methodology specifically developed for this purpose, where a seven-step application was defined, with each step involving an activity to be carried out to verify the correlation performance indicators with the SDGs. By applying the proposed methodology, the assessment of 286 performance indicators was conducted, revealing that 55.24% aligned the mine’s operation with the SDGs. Furthermore, the developed methodology may be applied to other mining enterprises, supporting their sustainability reports and compliance with the sector’s regulatory standards and mine closure plan requirements.
可持续发展的概念在所有工业领域都得到了广泛认可,尤其是在应对潜在的全球环境危机方面。在采矿业,可持续发展通过解决环境、社会和经济方面的问题来确保负责任的运营。绩效指标分为环境、社会、经济和治理四个组别,对这些方面进行监督。2015 年,联合国制定了 17 项可持续发展目标 (SDG),作为实现公平经济和社会发展的全球议程。本研究介绍了一种评估巴西帕拉州东南部一座铁矿的绩效指标的方法,以了解这些指标是否以及如何指导铁矿的运营实现可持续发展目标。本研究基于为此目的专门开发的方法论的应用,其中定义了七步应用,每一步都涉及要开展的活动,以验证绩效指标与可持续发展目标的相关性。通过应用所提出的方法,对 286 项绩效指标进行了评估,结果显示 55.24% 的矿山运营符合可持续发展目标。此外,所开发的方法还可应用于其他矿业企业,为其可持续发展报告以及遵守行业监管标准和矿山关闭计划要求提供支持。
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引用次数: 0
NaClO3 Crystal Growth and Dissolution by Temperature Cycling in a Sessile Droplet 通过温度循环在无水液滴中生长和溶解 NaClO3 晶体
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-08-30 DOI: 10.3390/min14090898
Alexis Leborgne, Woo-Sik Kim, Bum Jun Park, Morgane Sanselme, Gérard Coquerel
Abstract: Sodium chlorate is the most popular compound used to study spontaneous symmetry breaking by means of crystallization. Therefore, it is important to know the behavior of the solid particles. NaClO3 crystal growth and dissolution are investigated in an aqueous sessile droplet subjected to numerous temperature cycles. On cooling, in addition to the classical formation of repeated elongated fluid inclusions, there is a reproducible appearance of prismatic fluid inclusions (PFIs) at the corners of single crystals. The underlying mechanism involves the complete termination of the (110) face growth and the propagation of the {100} faces, which can close the PFIs. This study reports that on heating, transient donut-like single crystals formed, which could lead to their segmentation, even without stirring the suspension. The systematic addition of other sodium salts with chlorine atoms at different oxidation states did not change these observations.
摘要:氯酸钠是最常用于研究通过结晶自发破坏对称性的化合物。因此,了解固体颗粒的行为非常重要。本文研究了在水性无柄液滴中,NaClO3 晶体生长和溶解过程中的多次温度循环。冷却时,除了重复拉长的流体包裹体的典型形成外,在单晶体的边角处还会重复出现棱柱形流体包裹体 (PFI)。其基本机理涉及 (110) 面生长的完全终止和 {100} 面的传播,后者可以封闭 PFIs。本研究报告指出,加热时会形成瞬时甜甜圈状单晶体,即使不搅拌悬浮液也会导致单晶体分割。系统地添加其他具有不同氧化态氯原子的钠盐并没有改变这些观察结果。
{"title":"NaClO3 Crystal Growth and Dissolution by Temperature Cycling in a Sessile Droplet","authors":"Alexis Leborgne, Woo-Sik Kim, Bum Jun Park, Morgane Sanselme, Gérard Coquerel","doi":"10.3390/min14090898","DOIUrl":"https://doi.org/10.3390/min14090898","url":null,"abstract":"Abstract: Sodium chlorate is the most popular compound used to study spontaneous symmetry breaking by means of crystallization. Therefore, it is important to know the behavior of the solid particles. NaClO3 crystal growth and dissolution are investigated in an aqueous sessile droplet subjected to numerous temperature cycles. On cooling, in addition to the classical formation of repeated elongated fluid inclusions, there is a reproducible appearance of prismatic fluid inclusions (PFIs) at the corners of single crystals. The underlying mechanism involves the complete termination of the (110) face growth and the propagation of the {100} faces, which can close the PFIs. This study reports that on heating, transient donut-like single crystals formed, which could lead to their segmentation, even without stirring the suspension. The systematic addition of other sodium salts with chlorine atoms at different oxidation states did not change these observations.","PeriodicalId":18601,"journal":{"name":"Minerals","volume":"7 1","pages":""},"PeriodicalIF":2.5,"publicationDate":"2024-08-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215223","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Correction: Leeman et al. U-Pb LA-ICP-MS Zircon Dating of Crustal Xenoliths: Evidence of the Archean Lithosphere Beneath the Snake River Plain. Minerals 2024, 14, 578 更正:Leeman et al. U-Pb LA-ICP-MS Zircon Dating of Crustal Xenoliths:Evidence of the Archean Lithosphere Beneath the Snake River Plain.矿物 2024,14,578
IF 2.5 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-08-30 DOI: 10.3390/min14090886
William P. Leeman, Jeffrey D. Vervoort, S. Andrew DuFrane
There were three errors in the original publication [...]
原始出版物中有三处错误 [...]
{"title":"Correction: Leeman et al. U-Pb LA-ICP-MS Zircon Dating of Crustal Xenoliths: Evidence of the Archean Lithosphere Beneath the Snake River Plain. Minerals 2024, 14, 578","authors":"William P. Leeman, Jeffrey D. Vervoort, S. Andrew DuFrane","doi":"10.3390/min14090886","DOIUrl":"https://doi.org/10.3390/min14090886","url":null,"abstract":"There were three errors in the original publication [...]","PeriodicalId":18601,"journal":{"name":"Minerals","volume":"7 1","pages":""},"PeriodicalIF":2.5,"publicationDate":"2024-08-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215180","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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Minerals
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