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World's largest coal-fired carbon capture demonstration project begins operation in Gansu Province, China 世界上最大的燃煤碳捕获示范项目在中国甘肃省开始运行
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.31035/cg2025151
Hui Guo , Li-qiong Jia , Xi-jie Chen , Zi-guo Hao
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引用次数: 0
Editorial Committee of China Geology 《中国地质》编辑委员会
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.1016/S2096-5192(25)00120-X
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引用次数: 0
Improved SE-UNet network-based semantic segmentation and extraction of hidden geological significance in geological maps 基于改进SE-UNet网络的地质图隐含地质意义语义分割与提取
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.31035/cg2023146
Kai Ma , Jun-jie Liu , Si-qi Lu , Ze-hua Huang , Miao Tian , Jun-yuan Deng , Zhong Xie , Qin-jun Qiu
Automatic segmentation and recognition of content and element information in color geological map are of great significance for researchers to analyze the distribution of mineral resources and predict disaster information. This article focuses on color planar raster geological map (geological maps include planar geological maps, columnar maps, and profiles). While existing deep learning approaches are often used to segment general images, their performance is limited due to complex elements, diverse regional features, and complicated backgrounds for color geological map in the domain of geoscience. To address the issue, a color geological map segmentation model is proposed that combines the Felz clustering algorithm and an improved SE-UNet deep learning network (named GeoMSeg). Firstly, a symmetrical encoder-decoder structure backbone network based on UNet is constructed, and the channel attention mechanism SENet has been incorporated to augment the network's capacity for feature representation, enabling the model to purposefully extract map information. The SE-UNet network is employed for feature extraction from the geological map and obtain coarse segmentation results. Secondly, the Felz clustering algorithm is used for super pixel pre-segmentation of geological maps. The coarse segmentation results are refined and modified based on the super pixel pre-segmentation results to obtain the final segmentation results. This study applies GeoMSeg to the constructed dataset, and the experimental results show that the algorithm proposed in this paper has superior performance compared to other mainstream map segmentation models, with an accuracy of 91.89% and a MIoU of 71.91%.
彩色地质图中内容和元素信息的自动分割与识别,对于矿产资源分布分析和灾害信息预测具有重要意义。本文主要介绍彩色平面栅格地质图(地质图包括平面地质图、柱状地质图和剖面图)。虽然现有的深度学习方法通常用于一般图像的分割,但由于地质科学领域彩色地质图的元素复杂、区域特征多样、背景复杂,其性能受到限制。为了解决这一问题,提出了一种结合Felz聚类算法和改进的SE-UNet深度学习网络(GeoMSeg)的彩色地质图分割模型。首先,构建基于UNet的对称编码器-解码器结构骨干网,并引入通道注意机制SENet增强网络的特征表示能力,使模型能够有针对性地提取地图信息;利用SE-UNet网络对地质图进行特征提取,得到粗分割结果。其次,利用Felz聚类算法对地质图进行超像素预分割;在超像素预分割结果的基础上对粗分割结果进行细化和修正,得到最终的分割结果。本研究将GeoMSeg应用于构建的数据集,实验结果表明,与其他主流地图分割模型相比,本文提出的算法具有优越的性能,准确率为91.89%,MIoU为71.91%。
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引用次数: 0
Cassiterite U-Pb geochronology of the Sareshenke Tin deposit in the East Junggar: Implications for the two stages of tin mineralization 准噶尔东部萨累申克锡矿锡石U-Pb年代学及其两期锡矿化意义
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.31035/cg2024153
Su-xia Peng , Kai Weng , Xiao-qin Quan , Bo Chen , Zhao-wei Zhang , Chao Sun
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引用次数: 0
Organic geochemistry and basin modeling of the Eocene Mangahewa source rock system in the Pohokura oilfield, Taranaki Basin (New Zealand) and their indication of oil and gas potential 新西兰Taranaki盆地Pohokura油田始新统Mangahewa烃源岩体系有机地球化学、盆地模拟及其油气潜力指示
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.31035/cg2023137
Talha S.M. Qadri , Mohammed Hail Hakimi , Mahdi Ali Lathbl , Aref Lashin , Mohammed Almobarky , Afikah Rahim
The importance of organic geochemistry and basin modeling is widely recognized and used to understand the source rock potential and hydrocarbon generation history of the Mangahewa Formation, and thereby given the foundational role in the petroleum exploration. This study utilized the total organic carbon (TOC) content and hydrogen index (HI) to investigate the dominant kerogen type and hydrogen richness for the significance of petroleum generative potential. The Mangahewa coals and carbonaceous shales exhibit an excellent source rocks, with high total organic content (TOC) of more than 22%. The coals and carbonaceous shales were also characterised by Type II–III kerogen with Type III kerogen, promising oiland gas-prones. The Mangahewa Formation reached the main oil generation, with vitrinite reflectances between 0.53% and 1.01%. Vitrinite reflectance was also used in developing themal models and reveal the transformation (TR) of 10–50% kerogen to oil during the Late Miocene. The models also showed that the Mangahewa source rock has a significant oil generation and little expulsion competency, with a TR of up to 54%. These findings support the substantial oil-generating potential in the Taranaki Basin's southern graben and can be used as a guide when developing strategies for an oil exploration program.
有机地球化学和盆地建模的重要性已被广泛认识,并用于了解Mangahewa组烃源岩潜力和生烃历史,从而为石油勘探提供基础作用。利用总有机碳(TOC)含量和氢指数(HI)研究优势干酪根类型和氢丰度,对油气生烃潜力具有重要意义。manggahewa煤和碳质页岩具有优良的烃源岩特征,总有机含量(TOC)大于22%。煤和碳质页岩以II-III型干酪根为特征,其中III型干酪根具有较好的油气潜力。Mangahewa组为主要生油层,镜质组反射率为0.53% ~ 1.01%。利用镜质体反射率建立热模拟,揭示了晚中新世10-50%干酪根向石油的转化(TR)。模型还表明,Mangahewa烃源岩生油能力强,排油能力弱,TR高达54%。这些发现支持了Taranaki盆地南部地堑的巨大产油潜力,并可作为制定石油勘探计划策略的指南。
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引用次数: 0
Late Jurassic tectono-volcanic evolution and sauropod radiation of eastern Jiangnan orogen: Evidence from Tunxi Formation, China 江南造山带东部晚侏罗世构造-火山演化与蜥脚类动物辐射:来自屯溪组的证据
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.31035/cg2023087
Xin-xin Ren , Xu-ri Wang , Yi-chuan Liu , Shu-bin Ju
A prevailing theory suggests that volcanic eruptions triggered environmental changes, which compelled dinosaurs to migrate in search of new habitats. Compelling evidence for this hypothesis has now been discovered in the Tunxi Basin of eastern China. During the Late Mesozoic, the subduction of the Pacific Plate beneath southeastern China led to multi-stage volcanic activity. The Tunxi Formation in the basin, the first reported Upper Jurassic volcanic unit in the eastern Jiangnan orogen. It overlies the stratum bearing the easternmost mamenchisaurids, which is the dominant Asian sauropod lineage. Geochemical analyses suggest its affinity with coeval magmatism in southeastern China, while new rhyolite zircon U-Pb dating yields an age of 151.6 ± 2.2 Ma, further indicating a transition from arc magmatism to back-arc extension driven by Paleo-Pacific subduction during the Late Jurassic. These studies also confirm that, as early as 156 Ma, the Tunxi Basin was already a key habitat for mamenchisaurids. The Late Jurassic subduction of the Paleo-Pacific Plate caused extensive magmatism across eastern China. This intense tectonic shift likely induced abrupt environmental changes in relative basins. Severe volcanic activity drastically reduced the habitat of mamenchisaurids, prompting a northwestward and southward radiation trend —presents a coherent scene of volcanic eruptions, environmental catastrophe, and dinosaurs migrating.
一种流行的理论认为,火山爆发引发了环境变化,迫使恐龙迁徙寻找新的栖息地。目前在中国东部屯溪盆地发现了支持这一假说的有力证据。晚中生代,太平洋板块在中国东南部的俯冲作用导致了多期火山活动。屯溪组是该盆地中首次报道的上侏罗统江南造山带东部的火山单元。它位于最东边的马门齐龙地层上,马门齐龙是亚洲主要的蜥脚类动物谱系。地球化学分析表明其与中国东南部同期岩浆活动密切相关,而新流纹岩锆石U-Pb测年结果为151.6±2.2 Ma,进一步表明晚侏罗世由古太平洋俯冲推动的弧岩浆活动向弧后伸展过渡。这些研究还证实,早在156年前,屯溪盆地就已经是门门龙的主要栖息地。晚侏罗世古太平洋板块的俯冲在中国东部造成了广泛的岩浆活动。这种强烈的构造位移可能导致了相关盆地的环境突变。剧烈的火山活动极大地减少了门门龙的栖息地,促使向西北和向南的辐射趋势——呈现了一个连贯的火山爆发、环境灾难和恐龙迁徙的场景。
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引用次数: 0
Geology, geochemistry and mineralization of the Taishang-Shuiwangzhuang supergiant gold deposit (>700 t Au), northwestern Jiaodong Peninsula, China: A review 胶东半岛西北部太上-水王庄超大型金矿床地质、地球化学及成矿作用(bbb700 t Au
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.31035/cg2023152
Xiang-dong Liu , Zheng-jiang Ding , Zhong-yi Bao , Chun-ming Yan , Hao-cheng Yu , Jia-meng Fan , Tian-ci Xie , Zhi-ning Liu
The Taishang-Shuiwangzhuang gold deposit is located in the southeastern margin of Linglong gold field in the northern part of the Zhaoping Fault metallogenic belt of the Jiaodong gold province—the world's third-largest gold metallogenic area. Major prospecting breakthroughs have been made at the depth of 600–2500 m in recent years, with cumulative proven gold resources exceeding 700 t. Based on a large number of exploration data, the main characteristics of the deposit are described in detail, and the spatial coupling relationship between ore-controlling fault and main orebodies is discussed. The main orebodies occur as regular large veins, exhibiting branching and combination, expansion and contraction, and pinchout and reoccurrence. They extend in a gentle wave pattern along their strikes and dip directions and generally have a pitch direction of NEE and a plunge direction of NEE. As the ore-controlling fault, the Zhaoping Fault has the characteristics of wave-like fluctuation, with its dip angle presenting three steps of steep - slow transition within the depth range of 2500 m. The gold mineralization enrichment area is mainly distributed in the step parts where the fault plane changes from steeply to gently. The ore-forming age, ore-forming fluid and ore-forming material sources and the genesis of the ore deposit are analyzed based on the research results of ore deposit geochemistry. The ore-forming fluids were H2O-CO2-NaCltype hydrothermal solutions with a medium-low temperature and medium-low salinity. The H-O isotopic characteristics indicate that the fluids in the early ore-forming stage were possibly formed by degassing of basic magma and that meteoric water gradually entered the ore-forming fluids in the late ore-forming stage. The S and Pb isotopes indicate that the ore-forming materials mainly originate from the lower crust and contain a small quantity of mantle-derived components. The comprehensive analysis shows that the Taishang-shuiwangzhuang gold deposit was a typical “Jiaodong type” gold deposit. The strong crustmantle interactions, large-scale magmatism, and the material exchange arising from the transformation from the ancient lower crust to the juvenile lower crust during the Early Cretaceous provided abundant fluids and material sources for mineralization. Moreover, the detachment faults formed by the rapid magmatic uplift and the extensional tectonism created favorable temperature and pressure conditions and space for fluid accumulation and gold precipitation and mineralization.
太上-水王庄金矿床位于世界第三大金矿区胶东金矿省昭平断裂成矿带北段玲珑金矿田东南缘。近年来在600 ~ 2500 m深度取得重大找矿突破,累计探明金资源量超过700 t。在大量勘查资料的基础上,详细描述了矿床的主要特征,探讨了控矿断裂与主矿体的空间耦合关系。主矿体呈规则的大矿脉状赋存,表现为分支组合、扩张收缩、针状回出。它们沿走向和倾斜方向呈平缓波状延伸,一般为北东东倾倾方向和北东东倾倾方向。昭平断裂作为控矿断裂,具有波状起伏的特征,其倾角在2500 m深度范围内呈现陡缓过渡的3个台阶。金矿化富集区主要分布在断裂面由陡变缓的台阶部分。在矿床地球化学研究成果的基础上,分析了矿床的成矿时代、成矿流体和成矿物质来源及矿床成因。成矿流体为中低温、中低盐度的h2o - co2 - nacl型热液。氢氧同位素特征表明,成矿早期流体可能是由基性岩浆脱气形成的,成矿晚期大气降水逐渐进入成矿流体。S、Pb同位素表明成矿物质主要来源于下地壳,并含有少量幔源成分。综合分析表明,太上-水王庄金矿床为典型的“胶东型”金矿床。早白垩世强烈的壳幔相互作用、大规模的岩浆活动以及由古下地壳向幼下地壳转化所产生的物质交换,为成矿提供了丰富的流体和物质来源。快速岩浆隆升和伸展构造作用形成的拆离断裂为流体聚集和金的沉淀成矿创造了有利的温度和压力条件和空间。
{"title":"Geology, geochemistry and mineralization of the Taishang-Shuiwangzhuang supergiant gold deposit (>700 t Au), northwestern Jiaodong Peninsula, China: A review","authors":"Xiang-dong Liu ,&nbsp;Zheng-jiang Ding ,&nbsp;Zhong-yi Bao ,&nbsp;Chun-ming Yan ,&nbsp;Hao-cheng Yu ,&nbsp;Jia-meng Fan ,&nbsp;Tian-ci Xie ,&nbsp;Zhi-ning Liu","doi":"10.31035/cg2023152","DOIUrl":"10.31035/cg2023152","url":null,"abstract":"<div><div>The Taishang-Shuiwangzhuang gold deposit is located in the southeastern margin of Linglong gold field in the northern part of the Zhaoping Fault metallogenic belt of the Jiaodong gold province—the world's third-largest gold metallogenic area. Major prospecting breakthroughs have been made at the depth of 600–2500 m in recent years, with cumulative proven gold resources exceeding 700 t. Based on a large number of exploration data, the main characteristics of the deposit are described in detail, and the spatial coupling relationship between ore-controlling fault and main orebodies is discussed. The main orebodies occur as regular large veins, exhibiting branching and combination, expansion and contraction, and pinchout and reoccurrence. They extend in a gentle wave pattern along their strikes and dip directions and generally have a pitch direction of NEE and a plunge direction of NEE. As the ore-controlling fault, the Zhaoping Fault has the characteristics of wave-like fluctuation, with its dip angle presenting three steps of steep - slow transition within the depth range of 2500 m. The gold mineralization enrichment area is mainly distributed in the step parts where the fault plane changes from steeply to gently. The ore-forming age, ore-forming fluid and ore-forming material sources and the genesis of the ore deposit are analyzed based on the research results of ore deposit geochemistry. The ore-forming fluids were H<sub>2</sub>O-CO<sub>2</sub>-NaCltype hydrothermal solutions with a medium-low temperature and medium-low salinity. The H-O isotopic characteristics indicate that the fluids in the early ore-forming stage were possibly formed by degassing of basic magma and that meteoric water gradually entered the ore-forming fluids in the late ore-forming stage. The S and Pb isotopes indicate that the ore-forming materials mainly originate from the lower crust and contain a small quantity of mantle-derived components. The comprehensive analysis shows that the Taishang-shuiwangzhuang gold deposit was a typical “Jiaodong type” gold deposit. The strong crustmantle interactions, large-scale magmatism, and the material exchange arising from the transformation from the ancient lower crust to the juvenile lower crust during the Early Cretaceous provided abundant fluids and material sources for mineralization. Moreover, the detachment faults formed by the rapid magmatic uplift and the extensional tectonism created favorable temperature and pressure conditions and space for fluid accumulation and gold precipitation and mineralization.</div></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"8 4","pages":"Pages 843-861"},"PeriodicalIF":4.7,"publicationDate":"2025-11-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145537186","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"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
Improved new methods of seismic risk assessment and seismic zoning in Kazakhstan according to Eurocode 8 根据欧洲规范8改进了哈萨克斯坦地震风险评估和地震区划的新方法
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-18 DOI: 10.31035/cg2023151
Daulet Sarsenbaev , Abdulaziz Abdullaev , Nursarsen Uzbekov , Alla Sadykova , Yelizaveta Yessenzhigitova
This article aims to enhance seismic hazard assessment methods for Kazakhstan's seismotectonic conditions. It combines probabilistic seismic hazard analysis (PSHA), ground motion simulation, sitespecific geological and geotechnical data analysis, and seismic scenario analysis to develop Probabilistic General Seismic Zoning (GSZ) maps for Kazakhstan and Probabilistic Seismic Microzoning maps for Almaty. These maps align with Eurocode 8 principles, incorporating seismic intensity and engineering parameters like peak ground acceleration (PGA). The new procedure, applied in national projects, has resulted in GSZ maps for the country, seismic microzoning maps for Almaty, and detailed seismic zoning maps for East Kazakhstan. These maps, part of a regulatory document, guide earthquake-resistant design and construction. They offer a comprehensive assessment of seismic hazards, integrating traditional Medvedev–Sponheuer–Karnik (MSK-64) intensity scale points with quantitative parameters like peak ground acceleration. This innovative approach promises to advance methods for quantifying seismic hazards in specific regions.
本文旨在完善哈萨克斯坦地震构造条件的地震危险性评价方法。它结合了概率地震危害分析(PSHA)、地面运动模拟、特定地点的地质和岩土数据分析以及地震情景分析,为哈萨克斯坦开发了概率一般地震区划(GSZ)地图,为阿拉木图开发了概率地震微区划地图。这些地图与欧洲规范8的原则保持一致,结合了地震强度和峰值地面加速度(PGA)等工程参数。在国家项目中应用的新程序产生了国家的GSZ地图,阿拉木图的地震微分区地图和东哈萨克斯坦的详细地震分区地图。这些地图是规范性文件的一部分,指导抗震设计和施工。它们将传统的Medvedev-Sponheuer-Karnik (MSK-64)强度标度点与峰值地面加速度等定量参数相结合,提供了地震危险性的综合评估。这种创新的方法有望推进量化特定地区地震危险性的方法。
{"title":"Improved new methods of seismic risk assessment and seismic zoning in Kazakhstan according to Eurocode 8","authors":"Daulet Sarsenbaev ,&nbsp;Abdulaziz Abdullaev ,&nbsp;Nursarsen Uzbekov ,&nbsp;Alla Sadykova ,&nbsp;Yelizaveta Yessenzhigitova","doi":"10.31035/cg2023151","DOIUrl":"10.31035/cg2023151","url":null,"abstract":"<div><div>This article aims to enhance seismic hazard assessment methods for Kazakhstan's seismotectonic conditions. It combines probabilistic seismic hazard analysis (PSHA), ground motion simulation, sitespecific geological and geotechnical data analysis, and seismic scenario analysis to develop Probabilistic General Seismic Zoning (GSZ) maps for Kazakhstan and Probabilistic Seismic Microzoning maps for Almaty. These maps align with Eurocode 8 principles, incorporating seismic intensity and engineering parameters like peak ground acceleration (PGA). The new procedure, applied in national projects, has resulted in GSZ maps for the country, seismic microzoning maps for Almaty, and detailed seismic zoning maps for East Kazakhstan. These maps, part of a regulatory document, guide earthquake-resistant design and construction. They offer a comprehensive assessment of seismic hazards, integrating traditional Medvedev–Sponheuer–Karnik (MSK-64) intensity scale points with quantitative parameters like peak ground acceleration. This innovative approach promises to advance methods for quantifying seismic hazards in specific regions.</div></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"8 4","pages":"Pages 661-675"},"PeriodicalIF":4.7,"publicationDate":"2025-11-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145537190","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"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
Risks and governance of heavy metals in European soil applied phosphate fertilizers 施用磷肥的欧洲土壤重金属风险及治理
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-07-25 DOI: 10.1016/S2096-5192(25)00094-1
Lian-kai Zhang , Xiang Liu , Ya-jie Sun , Bernd G. Lottermoser , Roland Bol , Heike Windmann , Silvia H. Haneklaus , Ewald Schnug
Phosphorus (P) poses a global challenge to the environment and human health due to its natural association with heavy metals. Sustainable use of P is crucial to ensure food security for future generations. An analysis of the 150 phosphate fertilizers stored at the Institute for Crop and Soil Science in Germany has been conducted, supplemented by previously published data. The elements Cd, Bi, U, Cr, Zn, Tl, As, B, Sb, Ni, and Se are found in higher concentrations in sedimentary derived phosphates compared to igneous derived phosphates. Mineral fertilizers contain more than ten times the amount of U, Cd, B, and As compared to farmyard manure. Principal component analyses (PCA) indicate that U, Cd, Be, and Cr are primarily present in sedimentary derived phosphates and their concentrations are 2 to 10 times higher than those in igneous derived phosphates. Regarding heavy metal contamination, over 1000 potential combinations were identified; 36% of these were significant but weak (> 0.1). It is estimated that approximately 707 t of uranium enter farmland annually through the application of mineral phosphate fertilizers in European countries. This contribution addresses environmental issues related to the utilization of rock phosphate as well as alternative production methods for cleaner and safer phosphate fertilizers while presenting a roadmap with measures for mitigation.
由于磷与重金属的天然关联,对环境和人类健康构成了全球性挑战。磷的可持续利用对确保子孙后代的粮食安全至关重要。对储存在德国作物和土壤科学研究所的150种磷肥进行了分析,并辅以先前发表的数据。Cd、Bi、U、Cr、Zn、Tl、As、B、Sb、Ni、Se等元素在沉积衍生磷酸盐中的含量高于火成岩衍生磷酸盐。矿物肥料所含的U、Cd、B、As等元素是农家肥的10倍以上。主成分分析(PCA)表明,U、Cd、Be和Cr主要存在于沉积衍生磷酸盐中,其浓度比火成岩衍生磷酸盐高2 ~ 10倍。在重金属污染方面,确定了1000多种潜在的组合;其中36%显著但较弱(>;0.1)。据估计,在欧洲国家,每年约有707吨铀通过施用磷肥进入农田。这份报告处理了与磷矿利用有关的环境问题以及生产更清洁、更安全磷肥的替代方法,同时提出了载有缓解措施的路线图。
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引用次数: 0
Editorial Committee of China Geology 《中国地质》编辑委员会
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-07-25 DOI: 10.1016/S2096-5192(25)00102-8
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引用次数: 0
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China Geology
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