Earth-Science Reviews最新文献

{"title":"Incorporating cross-scale insights into colloid-facilitated radionuclide transport in fractured rocks: A critical review","authors":"Funing Ma ,&nbsp;Zhenxue Dai ,&nbsp;Xiaoying Zhang ,&nbsp;Fangfei Cai ,&nbsp;Weiliang Wang ,&nbsp;Yong Tian ,&nbsp;Shangxian Yin ,&nbsp;Yue Ma ,&nbsp;Dayong Wang ,&nbsp;Mohamad Reza Soltanian ,&nbsp;Longcheng Liu ,&nbsp;Paul Reimus","doi":"10.1016/j.earscirev.2024.104974","DOIUrl":"10.1016/j.earscirev.2024.104974","url":null,"abstract":"<div><div>Driven by the global imperative for the geological disposal of high-level radioactive waste (HLW), notable progress has been made in predicting radionuclide transport within fractured rocks. Current research has recognized that the presence of colloids may significantly influence radionuclide transport. However, challenges remain in understanding and quantifying this process from a multi-scale perspective. This review provides a comprehensive overview of recent developments in understanding the role of colloids in facilitating radionuclide transport in multi-scale fractured rocks. We first revisit the fundamental characteristics and processes controlling the transport of colloids and radionuclides in fractured rocks, including the properties of fractured rocks, colloids, and radionuclides, as well as their complex interactions. Furthermore, we discuss recent advancements in lab- and field-scale experiments and modeling techniques that shed light on the mechanisms controlling colloid-facilitated radionuclide transport. The focus then shifts to scaling issues, including scale-dependent transport processes and parameters, as well as the upscaling theories that bridge the gap between lab-scale experiments and field-scale assessments. Finally, we identify unresolved problems and promising development trends in colloid-facilitated radionuclide transport, which offer new opportunities for enhancing the accuracy of long-term safety assessments in HLW geological repositories.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"259 ","pages":"Article 104974"},"PeriodicalIF":10.8,"publicationDate":"2024-11-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142655601","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}

{"title":"Fate of ‘forever chemicals’ in the global cryosphere","authors":"Yunqiao Zhou ,&nbsp;Xiaoping Wang ,&nbsp;Chuanfei Wang ,&nbsp;Zhiwei Ji ,&nbsp;Xuerui Niu ,&nbsp;Huike Dong","doi":"10.1016/j.earscirev.2024.104973","DOIUrl":"10.1016/j.earscirev.2024.104973","url":null,"abstract":"<div><div>The cryosphere serves as a significant sink in the global circulation of organic pollutants. Among them, per- and polyfluoroalkyl substances (PFAS), known as “forever chemical”, are of great concern as their concentrations surpass the Earth's planetary safety boundary. In this review, we synthesize knowledge on the fate of PFAS in the cryosphere, focusing on their sources, accumulation, release process, and ecological effects. Long-range atmospheric transport leads to widespread of PFAS in the cryosphere, whereas local activities are primarily responsible for the regional PFAS pollution. Because of the wide replacements of the ozone-depleting chlorofluorocarbons after the Montreal Protocol, the ultra-short chain (C &lt; 4) PFAS, particularly trifluoroacetic acid, have emerged as the predominant compounds in the cryosphere, which may become a focus of future research. Cryospheric components such as snowfall, sea ice, and permafrost are important accumulation reservoirs of PFAS, while under climate warming, air-snow exchange, sea-ice melting and permafrost thaw lead to redistribution of PFAS. During snow/ice melt, short-chain PFAS are released earlier than long-chain PFAS. The PFAS remaining in the proglacial environment exhibit a range of ecological effects on both micro- and higher trophic organisms through the food web, ultimately leading to biodiversity loss. Our analysis shed light on the fate of PFAS in the cryosphere under climate warming and highlighted the urgent need for their long-term monitoring and study of PFAS in glacial regions to protect the fragile ice world.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"259 ","pages":"Article 104973"},"PeriodicalIF":10.8,"publicationDate":"2024-11-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142655369","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}

{"title":"Hydrogen-induced mineral alteration: A review in the context of underground hydrogen storage (UHS) in saline aquifers","authors":"Heather Braid ,&nbsp;Kevin Taylor ,&nbsp;Edward Hough ,&nbsp;Chris Rochelle ,&nbsp;Vahid Niasar ,&nbsp;Lin Ma","doi":"10.1016/j.earscirev.2024.104975","DOIUrl":"10.1016/j.earscirev.2024.104975","url":null,"abstract":"<div><div>Hydrogen is considered a viable energy vector, it can be produced through the electrolysis of water and stored as a gaseous phase in the subsurface. Hydrogen storage in saline aquifers is not yet commercially operational, to increase the technological readiness, the complex interactions between rock, pore fluid, and hydrogen under reservoir conditions (increased pressure and temperature) need thorough understanding. It is acknowledged that abiotic geochemical reactions are a potential barrier for UHS as hydrogen is an electron donor and can form highly reactive hydrogen ions. Using a comparative approach, this study reviews the current disparity in the literature regarding the impacts and extents of hydrogen-induced abiotic reactions, to identify knowledge gaps requiring further investigation. Data from both experimental and modelled methods are summarised in relation to individual minerals, common in the subsurface, and their implications to efficiency and security of underground hydrogen storage. This review demonstrates a significant agreement concerning the lack of reaction between hydrogen and rock-forming silicate minerals, and a strong likelihood that under reservoir conditions (heightened temperature and pressure) hydrogen can reduce pyrite to pyrrhotite. It also reveals compelling evidence suggesting exposure to hydrogen can lead to the dissolution of sulphates (anhydrite) and carbonates (calcite). We conclude development of future hydrogen storage projects in saline aquifers should therefore focus on silicate-rich formations. And further work is needed to establish a clear understanding of extents and rates of potential mineral reactions to ensure storage security and efficiency in future projects.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"259 ","pages":"Article 104975"},"PeriodicalIF":10.8,"publicationDate":"2024-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142655604","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"A model of plate tectonic framework for the Southeast Asia margin in the mid-Cretaceous","authors":"Xiwu Luan","doi":"10.1016/j.earscirev.2024.104970","DOIUrl":"10.1016/j.earscirev.2024.104970","url":null,"abstract":"<div><div>The recent IODP drillings in the South China Sea (SCS) have greatly enhanced our understanding of the tectonics and evolution of the SCS, but also raised new questions on the opening of the SCS and the pre-SCS tectonic history. Recently available data on the South China block (SCB), SCS, Indochina block, Borneo, Sumatra, Andaman, Myanmar, and the Tibetan plateau allow an updated tectonic model for the Southeast Asian margin in the mid-Cretaceous (around 100 Ma). A global scale granitoid belt can be readily identified from Sikhote-Alin in the north all the way to Northwest Borneo and to the Qiangtang terrane, as representing a giant magmatic arc system in response to the direction change of the subduction of the Izinagi plate and the Indian-Australian plate at ∼100 Ma. This global subduction/magmatic system was displaced in the Early Cenozoic as the result of India-Asian collision, followed by the development of the escape tectonics characterized by strike-slip fault systems. The subsequent rifting further broke and dispersed the granitoid belts into fragments to the present locations in the Greater Southeast Asian tectonic realm.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"259 ","pages":"Article 104970"},"PeriodicalIF":10.8,"publicationDate":"2024-11-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142655368","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}

{"title":"The diversity, frequency and severity of natural hazard impacts on subsea telecommunications networks","authors":"Lucy Bricheno ,&nbsp;Isobel Yeo ,&nbsp;Michael Clare ,&nbsp;James Hunt ,&nbsp;Allan Griffiths ,&nbsp;Lionel Carter ,&nbsp;Peter J. Talling ,&nbsp;Megan Baker ,&nbsp;Stuart Wilson ,&nbsp;Matthew West ,&nbsp;Semisi Panuve ,&nbsp;Samuiela Fonua","doi":"10.1016/j.earscirev.2024.104972","DOIUrl":"10.1016/j.earscirev.2024.104972","url":null,"abstract":"<div><div>Subsea cables underpin global communications, carrying more than 99 % of all digital data traffic worldwide. While this &gt;1.6 million km-long network has been designed to be highly resilient, subsea cables can be damaged by a number of natural hazards that occur across all water depths in the ocean. Here, we explore the diversity of natural hazards that can damage cables, considering a broad frequency-magnitude spectrum. This paper is the first global perspective of actual and potential hazards affecting cables. As such, it is an accessible overview of the regional variability and complexity of hazards. Relatively rare and extreme events, such as super typhoons, submarine landslides or associated turbidity currents and volcanic eruptions, can synchronously cause widespread damage to multiple systems, in some cases disconnecting entire countries or dramatically slowing data traffic. We show that damage is rarely linked to an initial event, instead arising from cascades of processes that can lag by years. Not all instances of cable damage that relate to natural processes are linked to extreme events. We show that much smaller intensity meteorological and oceanographic processes such as storms and continuous seafloor currents that have been overlooked by previous studies can also damage subsea cables. New analysis of past instances of cable damage reveals that a significant proportion of previously unattributed faults may relate to such low-level but sustained impacts. It is these hazards that are most likely to change in frequency and magnitude in response to ongoing climate change but are also more predictable. Through mapping of exposure to these different hazards, we identify geographically-constrained hazard hotspots and identify various mitigation measures to enhance the evidence base and further strengthen subsea telecommunications network resilience.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"259 ","pages":"Article 104972"},"PeriodicalIF":10.8,"publicationDate":"2024-11-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142655371","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Reply to comment on: Late Cretaceous-Paleogene orogenic build-up of the Ecuadorian Andes: Review and discussion by Antenor Alemán","authors":"Etienne Jaillard","doi":"10.1016/j.earscirev.2024.104933","DOIUrl":"10.1016/j.earscirev.2024.104933","url":null,"abstract":"","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"258 ","pages":"Article 104933"},"PeriodicalIF":10.8,"publicationDate":"2024-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142651388","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}

{"title":"Corrigendum to “The uplift of the East Africa – Arabia swell” [Earth Science Review, 257 (2024), 104901]","authors":"Andrea Sembroni ,&nbsp;Claudio Faccenna ,&nbsp;Thorsten W. Becker ,&nbsp;Paola Molin","doi":"10.1016/j.earscirev.2024.104931","DOIUrl":"10.1016/j.earscirev.2024.104931","url":null,"abstract":"","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"258 ","pages":"Article 104931"},"PeriodicalIF":10.8,"publicationDate":"2024-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142651392","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}

{"title":"Floodplain lakes: Linking hydrology to ecology and conservation","authors":"Fan Xue ,&nbsp;Qi Zhang ,&nbsp;John M. Melack ,&nbsp;Hongwu Tang ,&nbsp;Saiyu Yuan ,&nbsp;Yuxue Jia ,&nbsp;Chenyang Xue ,&nbsp;Yanyan Song","doi":"10.1016/j.earscirev.2024.104967","DOIUrl":"10.1016/j.earscirev.2024.104967","url":null,"abstract":"<div><div>As human activities intensify and global climate change accelerates, floodplain lakes are experiencing hydrological transformations that profoundly impact their ecology. Based on an extensive review of published literature, current knowledge of floodplain lakes and links between hydrology and ecology are summarized and synthesized. River-lake interactions determine hydrological conditions in floodplain lakes, with high spatial heterogeneity influenced by topography, geophysical properties, and climate. Seasonal fluctuations in water level and hydrological connectivity affect the community structure of aquatic organisms and biogeochemical processes. The interplay of floods and terrain shapes vegetation dynamics. Hydrological regimes sustain the quantity and quality of habitats, along with food resources for waterbirds and other organisms. Although certain species have adaptive capacities to changing hydrology through life history strategies, behavioral modifications, or physiological adjustments, long-term pressures from reservoir construction, intensive land use, and other human activities appear to be inducing cumulative, non-linear impacts that may push these ecosystems towards critical thresholds. Sustained pressures increase the risk of regime shifts, threatening ecosystem functionality. Current research often overlooks the complex interactions and feedbacks within ecosystems, leading to uncertain predictions regarding species resilience and ecosystem function. Existing methods are insufficient for fully integrating both short-term disturbances and long-term pressure. Advancing understanding of species adaptations across different temporal scales remains a priority, highlighting the need for more comprehensive frameworks for biodiversity conservation that effectively account for changing environment. Future efforts should focus on comprehensive in-situ monitoring and observation strategies, jointly with the application of advanced mathematical models, to enhance our understanding of ecology of floodplain lakes.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"258 ","pages":"Article 104967"},"PeriodicalIF":10.8,"publicationDate":"2024-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142561351","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}

{"title":"A review of machine learning applications to geophysical logging inversion of unconventional gas reservoir parameters","authors":"Zihao Wang ,&nbsp;Yidong Cai ,&nbsp;Dameng Liu ,&nbsp;Jun Lu ,&nbsp;Feng Qiu ,&nbsp;Jinghong Hu ,&nbsp;Zhentao Li ,&nbsp;Ranjith Pathegama Gamage","doi":"10.1016/j.earscirev.2024.104969","DOIUrl":"10.1016/j.earscirev.2024.104969","url":null,"abstract":"<div><div>Reservoir parameters are crucial indicators for reservoir evaluation and development and provide insights into long-term reservoir behavior. The primary methods for evaluating these parameters include direct core observations, experimental testing, and indirect evaluation techniques. Since its introduction, geophysical logging has been used to evaluate and invert reservoir parameters owing to its wide coverage. With an increasing focus on unconventional natural gas reservoirs, more refined reservoir evaluations and multiparameter analyses are required for their development to address the complex and microscopic models differing from those of the conventional petroleum reservoirs. Geophysical logging is important in several unconventional fields. Machine learning (ML) was used in unconventional gas reservoirs as an effective method to establish relationships between parameters and logging features. However, the accuracy of evaluating storage layers using a single ML method is limited. Studies focusing only on algorithm updates and indicator values are problematic in terms of interpretability and production applications. A need to standardize the use of algorithms and introduce validation comparisons such as geological methods is evident. In this study, we reviewed ML algorithms and models commonly used for logging inversion applications. The current research status and issues were analyzed for different unconventional gas reservoir parameters. Our findings emphasize the importance of combining geological and other methods for logging inversion using ML. We also used the random forest algorithm to accurately predict the reservoir porosity, gas content, coal structure, and macrolithotypes. Combined with established permeability and vitrinite reflectance models, factor analysis was used to comprehensively analyze and evaluate the coalbed methane reservoirs in the study area. In our assessment of the challenges and future work on ML-based inversion, we observed a clear advantage for ML algorithms under geologically validated methods and experimental control. ML has great potential for optimizing the application of logging inversion for unconventional reservoir parameters.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"258 ","pages":"Article 104969"},"PeriodicalIF":10.8,"publicationDate":"2024-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142573283","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}

{"title":"Mapping the evolution of marine carbon during the last deglaciation: δ13C perspectives on the deglacial ocean carbon cycle","authors":"Ling Fang ,&nbsp;Ninglian Wang ,&nbsp;Minkyoung Kim","doi":"10.1016/j.earscirev.2024.104966","DOIUrl":"10.1016/j.earscirev.2024.104966","url":null,"abstract":"<div><div>The changes in the ocean circulation and biological pump played crucial roles in the rise in atmospheric CO₂ during the last deglaciation. However, our understanding remains limited regarding which processes―air-sea exchange, ocean circulation, and the biological pump―primarily influence the spatial dynamics of the oceanic carbon cycle. To address this knowledge gap, the present study compiles global stable carbon isotope (δ¹³C) records from various sources, including shallow and deep planktic, along with epifaunal and infaunal benthic foraminifera. The synthesis reveals a total increase of 0.37 ± 0.05 ‰ in marine δ¹³C values since the last glacial maximum. Of this increase, 68 ± 5 % is attributed to the response of the oceans in the southern hemisphere, while 32 ± 4 % is attributed to the northern hemisphere. By analyzing the difference between planktic and benthic foraminifera, a decreased vertical δ¹³C gradient (δ¹³C_sp–sb) is observed during the last deglaciation, indicating rapid carbon exchange between surface and deep waters during deglaciation. Additionally, the offset between the epifaunal and infaunal δ¹³C (δ¹³C_sb–db) provides insights into changes in productivity and bottom water oxygenation. Overall, the global synthesis suggests that the δ¹³C variation is largely controlled by ocean circulation in the northern hemisphere and at higher latitudes of the southern hemisphere, while primary production significantly influences subtropical regions. Furthermore, the δ¹³C confirms that the rise in atmospheric CO₂ during the first phase of Heinrich Stadial 1 (HS1) resulted from reduced primary production in subtropical regions along with strong ventilation in the second phase of HS1. Interestingly, the δ¹³C variations during the Younger Dryas (YD) suggest strong ventilation without evident changes in primary production. This four-dimensional dataset provides valuable insights into the transient changes in the ocean carbon cycle during deglaciation.</div></div>","PeriodicalId":11483,"journal":{"name":"Earth-Science Reviews","volume":"258 ","pages":"Article 104966"},"PeriodicalIF":10.8,"publicationDate":"2024-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142552466","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}