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Automated characterization of microfracture systems in organic-rich shales and their influence on porosity using convolutional neural networks on FIB-SEM images: A review 基于FIB-SEM图像的卷积神经网络自动表征富有机质页岩微裂缝系统及其对孔隙度的影响:综述
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-31 DOI: 10.1016/j.earscirev.2026.105415
Bo Liu , Qamar Yasin , Eshimiakhe Daniel , Ghulam Mohyuddin Sohail , Mengdi Sun , David A. Wood
Characterization of microfracture systems and nanopore networks in organic-rich shales is critical for understanding fluid transport, hydrocarbon storage capacity, and the feasibility of carbon dioxide (CO₂) sequestration. However, the inherent heterogeneity, complex morphology, and nano-scale features of shale microstructures present significant challenges for conventional image segmentation techniques. This study reviews and evaluates the performance of state-of-the-art deep learning architectures for automated high-precision segmentation of microfractures and pore systems in FIB-SEM images of organic-rich shales. To enhance the generalizability of each model, a hybrid training dataset comprising 5,000 real and 5,000 synthetically generated GAN-based FIB-SEM images is evaluated. Quantitative analysis reveals that Kite-Net (KiU-Net) outperforms both Swin UNET Transformers (Swin-UNETR) and Attention U-Net, achieving an overall segmentation accuracy of 94%, precision of 94%, and recall of 93%. Notably, KiU-Net excels in accurately delineating microfractures and complex pore geometries within kerogen-rich matrices. Based on KiU-Net's superior validation performance compared to the two other deep learning models, we employed it to segment 3D FIB-SEM image stacks, enabling volumetric reconstruction and analysis of pore connectivity. Results revealed marked morphological distinctions between organic and inorganic pores, with over 94% of pores existing as isolated, non-percolating clusters, a finding consistent with prior geological investigations. Cross-validation considering various shales and coals further validates the model's effectiveness across a range of lithofacies. Our study presents a scalable deep learning framework for analyzing nanoscale shale microstructures from images.
富有机质页岩中微裂缝系统和纳米孔网络的表征对于理解流体输送、油气储存能力和二氧化碳封存可行性至关重要。然而,页岩微观结构固有的非均质性、复杂的形态和纳米尺度特征给传统的图像分割技术带来了重大挑战。本研究回顾并评估了最先进的深度学习架构在富有机质页岩FIB-SEM图像中对微裂缝和孔隙系统进行自动化高精度分割的性能。为了增强每个模型的可泛化性,我们对一个混合训练数据集进行了评估,该数据集包括5000张真实图像和5000张合成生成的基于gan的FIB-SEM图像。定量分析表明,Kite-Net (KiU-Net)优于Swin UNET Transformers (swan - unetr)和Attention U-Net,总体分割准确率为94%,精密度为94%,召回率为93%。值得注意的是,KiU-Net在准确描绘富干酪根基质中的微裂缝和复杂孔隙几何形状方面表现出色。与其他两种深度学习模型相比,基于KiU-Net的卓越验证性能,我们将其用于分割3D FIB-SEM图像堆栈,从而实现体积重建和孔隙连通性分析。结果表明,有机孔隙和无机孔隙存在明显的形态差异,超过94%的孔隙以孤立的、非渗透的簇状存在,这与先前的地质调查结果一致。考虑各种页岩和煤的交叉验证进一步验证了该模型在一系列岩相中的有效性。我们的研究提出了一个可扩展的深度学习框架,用于从图像中分析纳米级页岩微观结构。
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引用次数: 0
Is daily extreme rainfall increasing in the Mediterranean basin? A critical review of the evidence 地中海盆地的每日极端降雨是否在增加?对证据的批判性审查
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-30 DOI: 10.1016/j.earscirev.2026.105409
José Carlos Gonzalez-Hidalgo , Santiago Beguería
This article reviews published research on trends in extreme precipitation events across the Mediterranean basin between 1980 and 2025. A total of 175 peer-reviewed studies were compiled using standardized search criteria across major bibliographic databases. The review focuses on reporting the diversity of findings as presented by their authors, while it does not assess the quality of data, methods, or definitions used in individual studies. To avoid misinterpretation, and ensure traceability of our research, key statements regarding trends transcribed directly from each paper's abstract, main text, or conclusions are compiled. The results highlight substantial spatial and temporal heterogeneity in reported trends, with few statistically significant and regionally consistent patterns. While in some subregions (particularly parts of Italy, southern France, some areas of Spanish east-coastland and North-Western Africa coastland) localized increases in high-magnitude rainfall events have been found, many areas show either no trend or statistically insignificant changes. The evidence does not support a basin-wide intensification of extreme precipitation, and observed trends appear more strongly influenced by local geographic and synoptic factors, or linked to specific analysis time windows, than by a coherent signal of global climate forcing. These findings underscore the importance of continued observation, high-resolution analysis, and cautious interpretation of regional extremes in a climate change context. A more unified methodological framework is needed to improve comparability across studies and support effective risk management and adaptation strategies in this highly exposed region.
本文回顾了1980年至2025年间地中海盆地极端降水事件趋势的已发表研究。通过主要书目数据库的标准化检索标准,共编制了175项同行评议研究。本综述的重点是报告作者提出的研究结果的多样性,而不评估单个研究中使用的数据、方法或定义的质量。为了避免误解,并确保我们研究的可追溯性,我们将直接从每篇论文的摘要、正文或结论中摘录有关趋势的关键陈述。结果突出了报告趋势的显著时空异质性,很少有统计上显著和区域一致的模式。虽然在一些分区域(特别是意大利部分地区、法国南部、西班牙东海岸和西北非洲海岸的一些地区)发现局部高强度降雨事件有所增加,但许多地区要么没有趋势变化,要么在统计上没有显著变化。证据不支持整个流域的极端降水加剧,观测到的趋势似乎更强烈地受到当地地理和天气因素的影响,或与特定的分析时间窗有关,而不是受到全球气候强迫的连贯信号的影响。这些发现强调了在气候变化背景下持续观测、高分辨率分析和谨慎解释区域极端事件的重要性。需要一个更统一的方法框架来提高研究之间的可比性,并支持这一高度暴露区域的有效风险管理和适应战略。
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引用次数: 0
Comparison of joint networks in limestones interbedded in shales 页岩中互层灰岩节理网络比较
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-29 DOI: 10.1016/j.earscirev.2026.105414
Marta Magán , David J. Sanderson , David C.P. Peacock
Joint networks exhibit a range of geometrical and topological features described by many different parameters. Data were collected using unmanned aerial vehicle images of ten limestone beds in the Lower Liassic rocks of Somerset, SW England, which were analysed using a GIS and relational database. Parameters were measured from digitizing maps and images of joint networks, and investigated using a range of parameters and statistical methods without assigning joints to sets. Geometry is analysed using: rose diagrams and cumulative plots of orientation, trace length statistics, and measures of intensity and block size; with the poly-modal orientation data treated by non-parametric methods (Kuiper tests). Topology is analysed based on the numbers of nodes, branches and regions.
The results show that the networks have similar topology, but have significant variations in intensity, block size and orientation between beds. The within-bed and between-bed variability is evaluated using analysis of variance methods. This allows discussion of stratigraphical and spatial variation, and the evolution of joint networks in multi-bedded sequences. Although bed thickness accounts for some of this variability, long, early formed joints are argued to control much of the network geometry and topology. The methods developed here can be applied directly, or with minor modification, to networks of veins, faults and other structures.
联合网络表现出一系列由许多不同参数描述的几何和拓扑特征。研究人员利用无人机对英格兰西南部萨默塞特郡下第三纪岩层中的10个石灰岩层进行了图像采集,并利用GIS和相关数据库对其进行了分析。从关节网络的数字化地图和图像中测量参数,并使用一系列参数和统计方法进行调查,而不将关节分配给集合。几何分析使用:玫瑰图和方向累积图,跟踪长度统计,和测量强度和块大小;用非参数方法(Kuiper检验)处理多模态定向数据。根据节点、分支和区域的数量来分析拓扑结构。结果表明,各层间的网络具有相似的拓扑结构,但在强度、块体大小和方向上存在显著差异。采用方差分析方法对床内和床间变异性进行了评价。这允许讨论地层和空间变化,以及多层序中节理网络的演化。尽管地层厚度对这种变化有一定的影响,但人们认为,早期形成的长节理控制了大部分网络的几何形状和拓扑结构。这里开发的方法可以直接应用,或稍加修改,用于脉网,断层和其他结构。
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引用次数: 0
Innovations in underground hydrogen storage with multiphysics simulations, optimization, and monitoring: A review 基于多物理场模拟、优化和监测的地下储氢技术创新综述
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-28 DOI: 10.1016/j.earscirev.2026.105411
Yue Zhang , Zhenxue Dai , Hung Vo Thanh , Mingxu Cao , Lulu Xu , Xiaoying Zhang , Bicheng Yan , Philip H. Stauffer , Huichao Yin , Kenneth C. Carroll , Mohamad Reza Soltanian
Underground Hydrogen Storage (UHS) is a promising solution for large-scale energy storage and a critical component in advancing low-carbon energy system. Ensuring the safety and efficiency of UHS necessitates a comprehensive understanding of multiphysical interactions driven by cyclic pore fluid pressure fluctuations and coupled physicochemical processes. This review examines the key geomechanical responses in UHS, including rock property variations under cyclic loading, fracture evolution and propagation, reservoir stress sensitivity, and fault stability. It also explores the impact of geochemical and microbial reactions on geomechanical characteristics. We provide an in-depth analysis of Thermal-Hydraulic-Mechanical-Chemical (THMC) coupled numerical simulations, highlighting their potential for future multi-scale modeling. Limitations of current machine learning (ML) approaches in addressing UHS challenges are highlighted, emphasizing the need for innovative ML-based methodologies. Operational strategies for hydrogen injection and production are reviewed, focusing on safety, efficiency, and economic viability. The necessity for multi-objective optimization (MOO) to balance storage efficiency, risk mitigation, and cost-effectiveness is also discussed. Current monitoring technologies are evaluated to ensure safe and efficient UHS operations. Finally, this review identifies critical knowledge gaps and underscores the importance of advancing geomechanical understanding under multiphysics-coupling. We highlight the need for ML-driven multiphysics theories, enhanced modeling techniques, and robust optimization strategies to improve UHS performance. This study serves as a comprehensive reference for future research and the large-scale implementation of UHS systems.
地下储氢(UHS)是一种很有前途的大规模储能解决方案,是推进低碳能源体系的关键组成部分。为了确保UHS的安全性和有效性,需要全面了解循环孔隙流体压力波动和耦合物理化学过程驱动的多物理相互作用。本文综述了UHS中关键的地质力学响应,包括循环加载下的岩石性质变化、裂缝演化和扩展、储层应力敏感性和断层稳定性。探讨了地球化学和微生物反应对地质力学特征的影响。我们对热-液压-机械-化学(THMC)耦合数值模拟进行了深入分析,强调了它们在未来多尺度建模中的潜力。强调了当前机器学习(ML)方法在解决UHS挑战方面的局限性,强调需要创新的基于ML的方法。综述了注氢和生产的操作策略,重点是安全性、效率和经济可行性。本文还讨论了采用多目标优化(MOO)来平衡存储效率、风险降低和成本效益的必要性。目前的监测技术进行评估,以确保安全和有效的UHS操作。最后,本综述指出了关键的知识缺口,并强调了在多物理场耦合下推进地质力学理解的重要性。我们强调需要机器学习驱动的多物理场理论、增强的建模技术和稳健的优化策略来提高UHS性能。本研究为未来的研究和UHS系统的大规模实施提供了全面的参考。
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引用次数: 0
Gravity maps of the African continental crustal and mantle structure 非洲大陆地壳和地幔结构的重力图
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-28 DOI: 10.1016/j.earscirev.2026.105412
Franck Eitel Kemgang Ghomsi , Robert Tenzer , Wenjin Chen , Alexey Baranov , Ojima Isaac Apeh , Tan Xiaolong , Hong Guoqing , Julienne Stroeve
The African continent is characterized by a complex tectonic and geological history, with its current configuration shaped by the assemblage of Precambrian cratons and fragments delineated by Proterozoic and Paleozoic mobile belts. Knowledge of its lithospheric structure has primarily been derived from sparsely and irregularly distributed seismic surveys, limiting continent-wide analysis. To address this issue, we utilize satellite (e.g., GOCE, GRACE) and terrestrial gravity observations, integrated with lithospheric structure models, to compile a suite of gravity maps on a 5′ × 5′ geographical grid. The maps of the free-air, Bouguer, crust-stripped, mantle, lithosphere-stripped, and sub-lithospheric mantle gravity disturbances enable detailed interpretation of Africa's lithospheric architecture. Our methodology enhances traditional gravimetric studies by applying advanced corrections for topographic, bathymetric, sediment, crustal, and lithospheric mantle density heterogeneities, revealing deeper structural signatures. The free-air gravity map exhibits a signature of topographic and upper crustal density variations, with positive anomalies (+50 to +150 mGal) over elevated regions (e.g., Ethiopian Plateau) and negative anomalies (−50 to −150 mGal) over sedimentary basins (e.g., Congo Basin). The Bouguer gravity map highlights tectonic and volcanic features, reflecting crustal thickness variations, with isostatic equilibrium in cratons and disequilibrium along continental rifts like the East African Rift System (EARS). The crust-stripped gravity map mirrors Moho geometry, showing a stark contrast between thin oceanic and thick continental crust. The mantle gravity map exhibits a thermal signature, with gravity lows marking active divergent margins along the East and West Rift Systems and highs coinciding with cold, stable Archean cratons. Combined Bouguer and mantle gravity analyses confirm a non-collisional origin of mountain ranges along the EARS. Notably, the southern portion of the EARS lacks a clear thermal signature, suggesting distributed deformation at diffuse plate boundaries. These findings, alongside signatures of the African Superswell and the Congo Craton subsidence, provide new insights into Africa's geodynamic evolution, supporting future geophysical and resource exploration efforts.
非洲大陆具有复杂的构造和地质历史,其目前的形态是由前寒武纪克拉通和元古代和古生代活动带所描绘的碎片组合而成的。对其岩石圈结构的了解主要来自稀疏和不规则分布的地震调查,限制了整个大陆的分析。为了解决这个问题,我们利用卫星(如GOCE, GRACE)和地面重力观测,结合岩石圈结构模型,在5 ‘ × 5 ’地理网格上编制了一套重力图。自由空气图、布格图、地壳剥离图、地幔图、岩石圈剥离图和岩石圈下地幔重力扰动图,使我们能够详细地解释非洲的岩石圈结构。我们的方法通过应用地形、水深、沉积物、地壳和岩石圈地幔密度非均质性的先进校正来增强传统的重力研究,揭示更深层次的结构特征。自由空气重力图显示了地形和上地壳密度变化的特征,高架地区(如埃塞俄比亚高原)呈正异常(+50 ~ +150 mGal),沉积盆地(如刚果盆地)呈负异常(- 50 ~ - 150 mGal)。布格重力图突出了构造和火山特征,反映了地壳厚度的变化,以及克拉通的均衡平衡和东非裂谷系统(EARS)等大陆裂谷的不平衡。地壳剥离重力图反映了莫霍几何形状,显示了薄的海洋地壳和厚的大陆地壳之间的鲜明对比。地幔重力图表现出热特征,重力低标志着东、西裂谷系活跃的辐散边缘,重力高标志着太古宙寒冷稳定的克拉通。结合布格和地幔重力分析证实了沿ear山脉的非碰撞起源。值得注意的是,ear的南部缺乏清晰的热特征,表明在扩散板块边界处存在分布变形。这些发现与非洲超级井和刚果克拉通沉降的特征一起,为非洲地球动力学演化提供了新的见解,为未来的地球物理和资源勘探工作提供了支持。
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引用次数: 0
Surging glaciers in Svalbard: Observing their distribution, characteristics and evolution 斯瓦尔巴群岛汹涌的冰川:观察它们的分布、特征和演变
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-26 DOI: 10.1016/j.earscirev.2026.105410
William D. Harcourt , Danni M. Pearce , Wojciech Gajek , Harold Lovell , Erik S. Mannerfelt , Andreas Kääb , Douglas I. Benn , Adrian Luckman , Richard Hann , Jack Kohler , Tazio Strozzi , Rebecca McCerery , Bethan J. Davies
Glacier surges are episodes of significantly increased ice flow due to ice-dynamical feedbacks, and are often repeated in a quasi-periodical manner. Ice mass is redistributed during a surge, which leads to surface lowering at high elevation as ice is transferred down-glacier and thickening nearer the terminus. In this paper, we review different approaches for monitoring and detecting glacier surges in Svalbard, one of the most prominent global clusters of surge-type glaciers. Current surge detection is mainly based upon tracking the speed of glaciers over time, measuring elevation and frontal changes, and more recently automatically detecting surface changes such as increased crevassing. Thermal and hydrological changes near the glacier bed drive surge dynamics and can be measured using geophysical sensors such as ground-penetrating radar (GPR) and seismometers. When glaciers surge, they often produce diagnostic landforms in subglacial and proglacial environments, allowing historical surging to be identified even if surges have not been directly observed.
Through this review, we have compiled an updated database of surge-type glaciers in Svalbard and find that 36% of glaciers display surge-type behaviour, which accounts for 75% of the total glacier area on Svalbard. Only 10% of all glaciers have been directly observed to surge, yet account for 48% of the total glacier area on Svalbard. Svalbard surge-type glaciers have gentler slopes, are generally longer, and extend across a larger elevation range compared to non surge-type glaciers across the archipelago. We find that the behaviour of surge-type glaciers is variable and more closely resembles a continuum from glaciers that do not surge to those which redistribute mass in a single event of strongly enhanced ice flux. We can describe the variability in surge behaviour using the concept of enthalpy and a six-stage surge model that characterises the build-up of energy at the glacier bed driven initially by thermal change and then ice acceleration which is prompted by changes in subglacial hydrology. Observations of glacier surges have improved significantly with routine mapping from satellites such as Sentinel-1, Sentinel-2 and the Landsat satellite series. Furthermore, an increasing number of geophysical measurements is enabling an improved understanding of subglacial processes before, during and after a surge, which is crucial for improving models of surge behaviour. As our observations of surges continue to improve, we expect to uncover new elements and details of surge behaviour, reaffirming the need to rethink the binary classification of glaciers as either ‘surge-type’ or ‘not surge-type’ in Svalbard and across the world.
冰川涌流是由于冰动力反馈导致冰流量显著增加的事件,通常以准周期性的方式重复发生。在涌浪期间,冰块被重新分配,这导致高海拔地区的地表下降,因为冰被转移到冰川下游,并在靠近冰川末端的地方变厚。本文综述了全球最著名的涌浪型冰川群之一斯瓦尔巴群岛冰川涌浪监测和探测的不同方法。目前的浪涌探测主要基于跟踪冰川随时间的速度,测量海拔和锋面的变化,以及最近自动探测地表变化,如增加的裂缝。冰川床附近的热变化和水文变化驱动浪涌动力学,可以使用地球物理传感器如探地雷达(GPR)和地震仪来测量。当冰川涌动时,它们通常会在冰下和前冰环境中产生诊断性地貌,即使没有直接观察到涌动,也可以识别历史上的涌动。通过这一综述,我们编制了一个更新的斯瓦尔巴群岛涌浪型冰川数据库,发现36%的冰川表现出涌浪型行为,占斯瓦尔巴群岛冰川总面积的75%。直接观测到的冰川中只有10%在激增,但却占斯瓦尔巴群岛冰川总面积的48%。与群岛上的非激流型冰川相比,斯瓦尔巴群岛的激流型冰川坡度较缓,通常较长,并且延伸的海拔范围更大。我们发现,涌浪型冰川的行为是可变的,更接近于一个连续体,从不涌浪的冰川到在冰通量强烈增强的单一事件中重新分配质量的冰川。我们可以用焓的概念和一个六阶段的涌浪模型来描述涌浪行为的可变性,该模型描述了冰川床上能量的积累,最初是由热变化驱动的,然后是由冰下水文变化引起的冰加速。通过Sentinel-1、Sentinel-2和Landsat卫星系列等卫星的常规制图,对冰川涌流的观测已经有了显著改善。此外,越来越多的地球物理测量使人们能够更好地了解浪涌之前、期间和之后的冰下过程,这对改进浪涌行为模型至关重要。随着我们对涌浪的观察不断改进,我们期望发现涌浪行为的新元素和细节,重申有必要重新思考斯瓦尔巴群岛和世界各地冰川的“涌浪型”和“非涌浪型”二元分类。
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引用次数: 0
Controls on commercial helium accumulation in coal seams: From fundamentals to an integration of basin geology and gas geochemistry 煤层中商业氦聚集的控制:从基础到盆地地质和天然气地球化学的整合
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-25 DOI: 10.1016/j.earscirev.2026.105402
Jianzhou Tang , Jinzhuang Xue , Shuangming Wang
Coal seams, as a result of the coalification of terrestrial plant matter, were previously regarded as unfavorable for economically significant helium accumulations. However, this viewpoint has been challenged by the increasing discoveries of helium-rich gas reservoirs in such settings. This review investigates the major controls on commercial helium accumulations in coal seams, using an integrated analysis of basin geology and gas geochemistry. Six main findings are summarized as follows. (1) Naturally occurring helium accumulates in nitrogen-, carbon dioxide-, methane-, and mixed-gas reservoirs, with nitrogen and methane reservoirs being the most favorable for commercial helium accumulation. (2) Commercial helium accumulation in coal seams is predominantly (> 70%) of external origin, although these seams are commonly enriched in thorium and uranium. (3) The formation of helium accumulations in coal seams largely depends on an external replenishment system, including source rocks, carrier fluids, migration pathways, and an open system. (4) Two key geological elements contribute to favorable trap conditions: one is coal seams that show high water saturation, effective pore connectivity, and adequate natural gas; and the other is overlying cap rocks that exhibit fine pore throats, high gas pressure, low temperature, and high associated fluid content. (5) An accumulation window at a depth of ca. 100–1250 m for helium in coal seams is proposed. (6) Three main geological patterns, namely basement uplift, basement fault and anticlinal crest patterns, are proposed for commercial helium accumulations in coal seams, and these patterns can be distinguished by variations in He/N2 ratios and N2, CO2, and CH4 contents. The findings presented herein are expected to provide guidance for helium exploration in coal seams.
由于陆生植物物质的煤化作用,煤层以前被认为不利于经济上重要的氦积累。然而,这一观点受到了越来越多的富氦气藏发现的挑战。本文结合盆地地质和天然气地球化学的综合分析,探讨了煤层中商业氦聚集的主要控制因素。六个主要发现总结如下。(1)天然氦在氮气、二氧化碳、甲烷和混合气藏中富集,其中氮气和甲烷气藏最有利于商业氦富集。(2)商业氦在煤层中的富集主要是外部成因(70%),尽管这些煤层通常富含钍和铀。(3)煤层氦聚集的形成在很大程度上取决于一个外部补给系统,包括烃源岩、载体流体、运移通道和开放系统。(4)形成有利圈闭条件的关键地质因素有两个:一是煤层含水饱和度高,孔隙连通性好,天然气充足;另一类为上覆盖层,其孔喉细、气压高、温度低、伴生流体含量高。(5)提出了煤层氦在100 ~ 1250 m的富集窗口。(6)煤层商业氦聚集的地质模式主要有基底隆起、基底断裂和背斜波峰三种,并可通过He/N₂比值和N₂、CO₂、CH₄含量的变化来区分。本文的研究成果有望为煤层氦勘探提供指导。
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引用次数: 0
Climatic and anthropogenic controls on late Holocene sediment transport to the Gulf of Mexico by the Mississippi River 气候和人为因素对晚全新世沉积物由密西西比河向墨西哥湾的运输的控制
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-24 DOI: 10.1016/j.earscirev.2026.105401
Peter D. Clift , Bailey Wycoff , Andrew Carter , Samuel Muñoz , Nikki Neubeck , Brittney Gregory , Carol A. Wilson , Tammy Rittenour , Jerzy Blusztajn , Tamer Ali
Models of large alluviated rivers suggest that erosional signals from the headwaters are not transported to the marine depocenter over many timescales because of extensive sediment buffering and recycling in flood plains. We present here a new integrated Late Holocene sedimentary record of the Mississippi River, synthesizing earlier analyses and new material from oxbow lakes, filled channel plugs and a continuous core from the delta to reconstruct a detailed 3000-year record of sediment compositions in the lower reaches. As well as major element data and new detrital zircon U-Pb dating since 860 y BP, our study presents a new basin-wide Sr and Nd isotope record. We show that weathering proxies are controlled by grain size, with little evidence for a long-term trend in chemical weathering in the last 3000 years. 87Sr/86Sr, but not εNd values are linked to grain size and the degree of chemical alteration, with coarser material generally lower in 87Sr/86Sr compared to fine sediment.
There is a long-term trend towards more erosion of ancient crust shown in suspended sediment, with greater flux from the Superior Province via the Upper Mississippi, increasing after 2000 y BP, when the climate dried, and humans adopted a more sedentary rather than hunter-gatherer lifestyle. This contrast with the sandy sediment that shows less erosion from the Trans-Hudson, Superior Province and Appalachian until ∼400 years ago. Another change is noted in both muddy and sandy sediment after ∼400 years ago, close to the start of the Little Ice Age, a time of colder and drier climate, when there was a gradual decrease in flux from the Rocky Mountain foreland basin via the Missouri River. The Mississippi River is not fully buffered on centennial scales prior to the installation of man-made levees. Short-term changes in zircon U-Pb populations indicate pulses of sediment supply to the lower reaches, likely related to floods. Maximum sediment supply from the Missouri River occurred at the Last Glacial Maximum and in the recent past (∼10 years).
A drying climate after 1000 years ago increased sediment delivery from the Appalachians, Trans-Hudson and Yavapai terranes by enhancing stream incision while reducing reworking of moraines eroded from the Superior Province. After ∼400 years ago human settlement of the Rocky Mountain foreland enhanced erosion from that region. Modern Mississippi sediment supply is heavily anthropogenically disrupted and thus makes a poor analog for older sediments deposited in the Gulf of Mexico.
大型冲积河流的模型表明,由于洪泛区广泛的沉积物缓冲和再循环,来自源头的侵蚀信号在许多时间尺度上不会被输送到海洋沉积中心。在此,我们提出了一个新的完整的晚全新世密西西比河沉积记录,综合了早期的分析和来自牛轭湖的新材料,填满的河道塞和三角洲的连续岩心,重建了下游3000年沉积物组成的详细记录。结合860 y BP以来的主要元素数据和碎屑锆石U-Pb定年,提出了新的全盆地Sr和Nd同位素记录。我们发现风化指标受粒度控制,在过去3000 年里化学风化的长期趋势几乎没有证据。87Sr/86Sr,但εNd值与粒度和化学蚀变程度无关,粗质沉积物的87Sr/86Sr含量普遍低于细质沉积物。
{"title":"Climatic and anthropogenic controls on late Holocene sediment transport to the Gulf of Mexico by the Mississippi River","authors":"Peter D. Clift ,&nbsp;Bailey Wycoff ,&nbsp;Andrew Carter ,&nbsp;Samuel Muñoz ,&nbsp;Nikki Neubeck ,&nbsp;Brittney Gregory ,&nbsp;Carol A. Wilson ,&nbsp;Tammy Rittenour ,&nbsp;Jerzy Blusztajn ,&nbsp;Tamer Ali","doi":"10.1016/j.earscirev.2026.105401","DOIUrl":"10.1016/j.earscirev.2026.105401","url":null,"abstract":"<div><div>Models of large alluviated rivers suggest that erosional signals from the headwaters are not transported to the marine depocenter over many timescales because of extensive sediment buffering and recycling in flood plains. We present here a new integrated Late Holocene sedimentary record of the Mississippi River, synthesizing earlier analyses and new material from oxbow lakes, filled channel plugs and a continuous core from the delta to reconstruct a detailed 3000-year record of sediment compositions in the lower reaches. As well as major element data and new detrital zircon U-Pb dating since 860 y BP, our study presents a new basin-wide Sr and Nd isotope record. We show that weathering proxies are controlled by grain size, with little evidence for a long-term trend in chemical weathering in the last 3000 years. <sup>87</sup>Sr/<sup>86</sup>Sr, but not ε<sub>Nd</sub> values are linked to grain size and the degree of chemical alteration, with coarser material generally lower in <sup>87</sup>Sr/<sup>86</sup>Sr compared to fine sediment.</div><div>There is a long-term trend towards more erosion of ancient crust shown in suspended sediment, with greater flux from the Superior Province via the Upper Mississippi, increasing after 2000 y BP, when the climate dried, and humans adopted a more sedentary rather than hunter-gatherer lifestyle. This contrast with the sandy sediment that shows less erosion from the Trans-Hudson, Superior Province and Appalachian until ∼400 years ago. Another change is noted in both muddy and sandy sediment after ∼400 years ago, close to the start of the Little Ice Age, a time of colder and drier climate, when there was a gradual decrease in flux from the Rocky Mountain foreland basin via the Missouri River. The Mississippi River is not fully buffered on centennial scales prior to the installation of man-made levees. Short-term changes in zircon U-Pb populations indicate pulses of sediment supply to the lower reaches, likely related to floods. Maximum sediment supply from the Missouri River occurred at the Last Glacial Maximum and in the recent past (∼10 years).</div><div>A drying climate after 1000 years ago increased sediment delivery from the Appalachians, Trans-Hudson and Yavapai terranes by enhancing stream incision while reducing reworking of moraines eroded from the Superior Province. After ∼400 years ago human settlement of the Rocky Mountain foreland enhanced erosion from that region. Modern Mississippi sediment supply is heavily anthropogenically disrupted and thus makes a poor analog for older sediments deposited in the Gulf of Mexico.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"275 ","pages":"Article 105401"},"PeriodicalIF":10.0,"publicationDate":"2026-01-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146048132","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"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
Formation and fluxes of natural hydrogen in the crust and upper mantle 地壳和上地幔中天然氢的形成和通量
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-22 DOI: 10.1016/j.earscirev.2026.105400
Kevin Wong , Martina Cascone , Donato Giovannelli , Alberto Vitale Brovarone
Molecular hydrogen (H2) is a fundamental component of planetary evolution and an important energy source for microbial life. It is now understood that natural mechanisms, spanning geological and biological processes, can produce high concentrations of hydrogen in natural fluids. Quantifying the processes that modulate natural hydrogen concentrations is necessary not only for conceptualising the distribution of life on Earth and elsewhere in the universe, but also for identifying settings where natural hydrogen may potentially accumulate to complement industrial hydrogen production. However, uncertainties persist in assessing these natural fluxes. In this review, we explore the biological and geological processes that can generate natural hydrogen. Compared to previous summary efforts, we include in our updated inventory hydrogen fluxes from biological processes, metamorphic degassing, and subduction zones. By integrating recent advances in quantifying hydrogen generation and transportation in geological environments, we demonstrate that significant concentrations and fluxes of hydrogen can arise in a plethora of settings worldwide, contributing towards a total abiotic production rate of 40 to 64< Mt H2 yr-1. We also highlight that geological environments characterised by high hydrogen production may be associated with high microbial hydrogen consumption (e.g., oceanic sediments). However, large uncertainties regarding the residence time of hydrogen within geological settings remain, and future research endeavours should aim to ascertain the long-term behaviour of hydrogen stored in the deep Earth to assess the viability of natural hydrogen as a renewable energy source.
分子氢(H2)是行星演化的基本组成部分,也是微生物生命的重要能量来源。现在人们了解,跨越地质和生物过程的自然机制可以在自然流体中产生高浓度的氢。量化调节天然氢浓度的过程是必要的,这不仅是为了概念化地球上和宇宙中其他地方的生命分布,也是为了确定天然氢可能积累以补充工业氢生产的环境。然而,在评估这些自然通量时,仍然存在不确定性。在这篇综述中,我们探讨了可以产生天然氢的生物和地质过程。与以前的总结工作相比,我们在更新的清单中包括了来自生物过程、变质脱气和俯冲带的氢通量。通过整合量化地质环境中氢气生成和运输的最新进展,我们证明,在世界各地的许多环境中,氢气的浓度和通量都可能显著增加,这有助于实现每年40至64mt H2的总非生物产量。我们还强调,以高产氢为特征的地质环境可能与高微生物耗氢(例如,海洋沉积物)有关。然而,关于氢气在地质环境中的停留时间仍然存在很大的不确定性,未来的研究工作应旨在确定储存在地球深处的氢气的长期行为,以评估天然氢气作为可再生能源的可行性。
{"title":"Formation and fluxes of natural hydrogen in the crust and upper mantle","authors":"Kevin Wong ,&nbsp;Martina Cascone ,&nbsp;Donato Giovannelli ,&nbsp;Alberto Vitale Brovarone","doi":"10.1016/j.earscirev.2026.105400","DOIUrl":"10.1016/j.earscirev.2026.105400","url":null,"abstract":"<div><div>Molecular hydrogen (H<sub>2</sub>) is a fundamental component of planetary evolution and an important energy source for microbial life. It is now understood that natural mechanisms, spanning geological and biological processes, can produce high concentrations of hydrogen in natural fluids. Quantifying the processes that modulate natural hydrogen concentrations is necessary not only for conceptualising the distribution of life on Earth and elsewhere in the universe, but also for identifying settings where natural hydrogen may potentially accumulate to complement industrial hydrogen production. However, uncertainties persist in assessing these natural fluxes. In this review, we explore the biological and geological processes that can generate natural hydrogen. Compared to previous summary efforts, we include in our updated inventory hydrogen fluxes from biological processes, metamorphic degassing, and subduction zones. By integrating recent advances in quantifying hydrogen generation and transportation in geological environments, we demonstrate that significant concentrations and fluxes of hydrogen can arise in a plethora of settings worldwide, contributing towards a total abiotic production rate of 40 to 64&lt; Mt H<sub>2</sub> yr<sup>-1</sup>. We also highlight that geological environments characterised by high hydrogen production may be associated with high microbial hydrogen consumption (e.g., oceanic sediments). However, large uncertainties regarding the residence time of hydrogen within geological settings remain, and future research endeavours should aim to ascertain the long-term behaviour of hydrogen stored in the deep Earth to assess the viability of natural hydrogen as a renewable energy source.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"275 ","pages":"Article 105400"},"PeriodicalIF":10.0,"publicationDate":"2026-01-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146033654","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"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
Advances and challenges in predicting wave runup in coastal regions: A scoping review of empirical, numerical, and AI-based approaches 预测沿海地区浪涌的进展和挑战:对经验、数值和基于人工智能的方法的范围审查
IF 1 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-18 DOI: 10.1016/j.earscirev.2026.105399
Erfan Amini , Mehrdad Baniesmaeil , Hossein Mehdipour , Mehdi Neshat , Reza Marsooli
Coastal regions, home to critical infrastructure and diverse ecosystems, are increasingly vulnerable to short-wave (incident-band) runup-induced hazards, including coastal erosion, flooding, and infrastructure damage. Accurately predicting short-wave runup is essential for effective coastal management, flood risk assessment, and climate adaptation strategies. This study presents a comprehensive scoping review of short-wave runup prediction methodologies, systematically evaluating empirical formulas, numerical models, and artificial intelligence (AI)-based approaches. We critically analyze their theoretical foundations, computational frameworks, and predictive capabilities under diverse coastal conditions. The review integrates a global wave runup dataset, providing a data-driven comparison of model performance across varying beach morphologies and hydrodynamic conditions. A key contribution of this review is conducting a cross-methodological evaluation, providing a structured assessment of the trade-offs between accuracy, computational demand, and real-world applicability across the three approaches. Furthermore, we examine the implications of climate change on wave runup prediction methodologies, emphasizing the effects of rising sea levels, changing storm characteristics, and changing wave energy on predictive reliability. The findings underscore the need for integrated modeling techniques to enhance predictive accuracy and support adaptive coastal management. By identifying research gaps and future directions, this review serves as a foundation for advancing wave runup prediction science, with direct applications in coastal engineering, risk mitigation, and climate resilience planning.
沿海地区是关键基础设施和多种生态系统的所在地,越来越容易受到短波(事件频带)径流引起的灾害的影响,包括海岸侵蚀、洪水和基础设施破坏。准确预测短波涨潮对于有效的海岸管理、洪水风险评估和气候适应战略至关重要。本研究对短波运行预测方法进行了全面的范围审查,系统地评估了经验公式,数值模型和基于人工智能(AI)的方法。我们批判性地分析了它们的理论基础、计算框架和在不同沿海条件下的预测能力。该综述整合了全球波浪运行数据集,提供了不同海滩形态和水动力条件下模型性能的数据驱动比较。本综述的一个关键贡献是进行了跨方法的评估,对三种方法之间的准确性、计算需求和实际适用性之间的权衡提供了结构化的评估。此外,我们研究了气候变化对海浪上升预测方法的影响,强调了海平面上升、风暴特征变化和波浪能量变化对预测可靠性的影响。研究结果强调了集成建模技术的必要性,以提高预测准确性和支持适应性海岸管理。通过确定研究差距和未来的方向,本综述为推进海浪上升预测科学奠定了基础,并直接应用于沿海工程、风险缓解和气候适应规划。
{"title":"Advances and challenges in predicting wave runup in coastal regions: A scoping review of empirical, numerical, and AI-based approaches","authors":"Erfan Amini ,&nbsp;Mehrdad Baniesmaeil ,&nbsp;Hossein Mehdipour ,&nbsp;Mehdi Neshat ,&nbsp;Reza Marsooli","doi":"10.1016/j.earscirev.2026.105399","DOIUrl":"10.1016/j.earscirev.2026.105399","url":null,"abstract":"<div><div>Coastal regions, home to critical infrastructure and diverse ecosystems, are increasingly vulnerable to short-wave (incident-band) runup-induced hazards, including coastal erosion, flooding, and infrastructure damage. Accurately predicting short-wave runup is essential for effective coastal management, flood risk assessment, and climate adaptation strategies. This study presents a comprehensive scoping review of short-wave runup prediction methodologies, systematically evaluating empirical formulas, numerical models, and artificial intelligence (AI)-based approaches. We critically analyze their theoretical foundations, computational frameworks, and predictive capabilities under diverse coastal conditions. The review integrates a global wave runup dataset, providing a data-driven comparison of model performance across varying beach morphologies and hydrodynamic conditions. A key contribution of this review is conducting a cross-methodological evaluation, providing a structured assessment of the trade-offs between accuracy, computational demand, and real-world applicability across the three approaches. Furthermore, we examine the implications of climate change on wave runup prediction methodologies, emphasizing the effects of rising sea levels, changing storm characteristics, and changing wave energy on predictive reliability. The findings underscore the need for integrated modeling techniques to enhance predictive accuracy and support adaptive coastal management. By identifying research gaps and future directions, this review serves as a foundation for advancing wave runup prediction science, with direct applications in coastal engineering, risk mitigation, and climate resilience planning.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"275 ","pages":"Article 105399"},"PeriodicalIF":10.0,"publicationDate":"2026-01-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145995581","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"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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