Procedia Earth and Planetary Science最新文献

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Water-rock Interaction Ascribed to Hyperalkaline Mineral Waters in the Cabeço de Vide Serpentinized Ultramafic Intrusive Massif (Central Portugal) 葡萄牙中部cabeo de Vide蛇纹石化超镁质侵入地块高碱性矿泉水的水岩相互作用
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2016.12.173
J. Marques, M. O. Neves, A. Miller, C. Rocha, S. Vance, L. Christensen, G. Etiope, P. Carreira, S. Suzuki
{"title":"Water-rock Interaction Ascribed to Hyperalkaline Mineral Waters in the Cabeço de Vide Serpentinized Ultramafic Intrusive Massif (Central Portugal)","authors":"J. Marques, M. O. Neves, A. Miller, C. Rocha, S. Vance, L. Christensen, G. Etiope, P. Carreira, S. Suzuki","doi":"10.1016/J.PROEPS.2016.12.173","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2016.12.173","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"238 5","pages":"646-649"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"72549961","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Geochemistry of Aquifer in Contact with Alum Shale: Evidence of Limited Contaminant Transfers 与明矾页岩接触的含水层地球化学:有限污染物转移的证据
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.029
J. Sterpenich, E. Gaucher, N. Schovsbo, Jérémy G. Lerat, R. Mosser-Ruck, J. Pironon
{"title":"Geochemistry of Aquifer in Contact with Alum Shale: Evidence of Limited Contaminant Transfers","authors":"J. Sterpenich, E. Gaucher, N. Schovsbo, Jérémy G. Lerat, R. Mosser-Ruck, J. Pironon","doi":"10.1016/J.PROEPS.2017.01.029","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2017.01.029","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"11 1","pages":"786-789"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"75125633","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Considerations About the Building of a Thermodynamic Database for the Chemical Description of Highly Saline Systems 建立高盐体系化学描述热力学数据库的思考
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.064
Arnault Lassin, Laurent André, Adeline Lach
{"title":"Considerations About the Building of a Thermodynamic Database for the Chemical Description of Highly Saline Systems","authors":"Arnault Lassin,&nbsp;Laurent André,&nbsp;Adeline Lach","doi":"10.1016/j.proeps.2016.12.064","DOIUrl":"10.1016/j.proeps.2016.12.064","url":null,"abstract":"<div><p>Amongst the existing models able to describe highly concentrated aqueous systems and solid-liquid or gas-liquid equilibria up to elevated temperatures and pressures, the semi-empirical Pitzer model has been shown to be powerful. Calculation codes are now available for applying this model to such complex natural and industrial systems. The key point remains the building of related thermodynamic databases of high quality. In this work, we present elements of a strategy to build and extend such a database for widespread use.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 304-307"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.064","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"75030533","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 4
Characterization of Pore Water, Ion Transport and Water-rock Interaction in Claystone by Advective Displacement Experiments☆ 粘土岩孔隙水、离子输运及水-岩相互作用的平流驱替实验表征
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.017
U. Mäder, H. Waber
{"title":"Characterization of Pore Water, Ion Transport and Water-rock Interaction in Claystone by Advective Displacement Experiments☆","authors":"U. Mäder, H. Waber","doi":"10.1016/J.PROEPS.2017.01.017","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2017.01.017","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"29 1","pages":"917-920"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"78014747","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 6
The Morphology of Gypsum Precipitated Under Hyper-saline Conditions – Preliminary Results from Dead Sea - Red Sea Mixtures 在高盐条件下沉淀的石膏的形态——死海-红海混合物的初步结果
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.095
A.G. Reiss , I. Gavrieli , J. Ganor
{"title":"The Morphology of Gypsum Precipitated Under Hyper-saline Conditions – Preliminary Results from Dead Sea - Red Sea Mixtures","authors":"A.G. Reiss ,&nbsp;I. Gavrieli ,&nbsp;J. Ganor","doi":"10.1016/j.proeps.2016.12.095","DOIUrl":"10.1016/j.proeps.2016.12.095","url":null,"abstract":"<div><p>Solutions of different chemical compositions will precipitate gypsum crystals with different morphology. The dependence of gypsum morphology on the chemical composition can therefore be a tool for interpreting the paleo-chemistry and environments of solutions from which gypsum in the geological record precipitated. In addition, the morphology of the gypsum that will precipitate in the Dead Sea once the Red Sea-Dead Sea conduit is built will determine if the crystals will remain in suspension in the surface brine, thereby leading to “whitening” of the lake. Despite its importance, little is known about the impact of the different parameters on the morphology of gypsum precipitated from natural brines. In the present study we conducted single point batch experiments with mixtures of Dead Sea - Red Sea brines and utilized image processing techniques to study the morphology of the gypsum that precipitated from different solution compositions at different degrees of oversaturation. The results from the first data set towards the understanding of what controls the morphology of gypsum while providing a preliminary tool for the forecast of the future of the Dead Sea are presented here.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 376-379"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.095","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"76252496","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 4
Laboratory Experiments on Forming the Chemical Composition of Flowback Brine from Hydraulic Fracturing with Energized Fluid 注能流体形成水力压裂返排盐水化学成分的室内实验
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2016.12.149
K. Labus, P. Kasza, M. Turek, P. Dydo, A. Jakóbik-Kolon, K. Wilk, G. Leśniak
{"title":"Laboratory Experiments on Forming the Chemical Composition of Flowback Brine from Hydraulic Fracturing with Energized Fluid","authors":"K. Labus, P. Kasza, M. Turek, P. Dydo, A. Jakóbik-Kolon, K. Wilk, G. Leśniak","doi":"10.1016/J.PROEPS.2016.12.149","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2016.12.149","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"1 1","pages":"582-585"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"76292084","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
Geochemical Characterization of U Tailings (Bois Noirs Limouzat, France) U尾矿的地球化学表征(Bois Noirs Limouzat, France
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.067
C. Chautard , C. Beaucaire , M. Gérard , V. Phrommavanh , J. Nos , L. Galoisy , G. Calas , R. Roy , M. Descostes
{"title":"Geochemical Characterization of U Tailings (Bois Noirs Limouzat, France)","authors":"C. Chautard ,&nbsp;C. Beaucaire ,&nbsp;M. Gérard ,&nbsp;V. Phrommavanh ,&nbsp;J. Nos ,&nbsp;L. Galoisy ,&nbsp;G. Calas ,&nbsp;R. Roy ,&nbsp;M. Descostes","doi":"10.1016/j.proeps.2016.12.067","DOIUrl":"10.1016/j.proeps.2016.12.067","url":null,"abstract":"<div><p>The uranium (U) mining site of Bois Noirs Limouzat located in the central France, produced 7,000 tons of U from 1959 to 1980. Tailings containing non extracted U and its radioactive progenies are currently stored under water in a basin extending over 18ha. To predict U (100-400 ppm) and <sup>226</sup>Ra (10-70Bq.g<sup>-1</sup>) mobility, a detailed chemical, mineralogical and radiological characterization of the phases is required. For this, tailings sampling was performed to collect undisturbed samples close of <em>in situ</em> conditions. Preliminary characterizations evidenced good correlation between facies (to link with the extraction mode), granulometry, U concentration and <sup>226</sup>Ra activity. U and <sup>226</sup>Ra are concentrated in the silty-clay facies mainly as inherited monazites and neoformation of uranyl phosphates known for their low solubility. Clay minerals and Fe-oxi-hydroxides are also encountered and may play an important role in radionuclide trapping by sorption processes. These preliminary results confirm the immobilization of U and <sup>226</sup>Ra within the tailings, even though, additional experiments are needed to determine the extent of U and <sup>226</sup>Ra sorbed on Fe-oxi-hydroxides and on clay minerals.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 308-311"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.067","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"80963546","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 7
Ferromagnesian Silicate and Ferrosulfide Rocks as a Source of Magnetite and Hydrogen 作为磁铁矿和氢来源的镁铁硅酸盐和硫化亚铁岩石
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2016.12.124
M. Bassez
{"title":"Ferromagnesian Silicate and Ferrosulfide Rocks as a Source of Magnetite and Hydrogen","authors":"M. Bassez","doi":"10.1016/J.PROEPS.2016.12.124","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2016.12.124","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"50 1","pages":"492-495"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79631728","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 9
87Sr/86Sr Ratios in Thermal Water from the Southern Upper Rhine Graben, Germany 德国上莱茵河地堑南部热水中87Sr/86Sr比值[j]
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.092
Gerhard Schmidt , Sami Al Najem , Margot Isenbeck-Schröter , Florian Freundt , Michael Kraml , Werner Aeschbach
{"title":"87Sr/86Sr Ratios in Thermal Water from the Southern Upper Rhine Graben, Germany","authors":"Gerhard Schmidt ,&nbsp;Sami Al Najem ,&nbsp;Margot Isenbeck-Schröter ,&nbsp;Florian Freundt ,&nbsp;Michael Kraml ,&nbsp;Werner Aeschbach","doi":"10.1016/j.proeps.2016.12.092","DOIUrl":"10.1016/j.proeps.2016.12.092","url":null,"abstract":"<div><p>The present study of thermal water from Bad Bellingen, Steinenstadt, Bad Krozingen, Mooswald, and Weinheim located in the southern part of the Upper Rhine Graben was undertaken in the framework of a multidisciplinary hydrogeochemical research project and concerns <sup>87</sup>Sr/<sup>86</sup>Sr isotope investigation. The aquifer lithologies of thermal waters are Triassic Upper Muschelkalk, Jurassic Hauptrogenstein and Tertiary Miocene sediments. The <sup>87</sup>Sr/<sup>86</sup>Sr ratios (N=9) range from 0.70912 to 0.71096. The Sr isotopic composition of thermal water is controlled by the fault system of the Rhine Graben rift. Fluids from Upper Muschelkalk aquifers ascent along the Eastern Boundary fault zone. The deep-water ascent most likely reaches into the crystalline basement.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 364-367"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.092","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90113350","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Environmental Assessment and Management of Phosphogypsum According to European and United States of America Regulations 根据欧洲和美国法规的磷石膏环境评价和管理
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2016.12.178
F. Macías, R. Pérez-López, C. R. Cánovas, S. Carrero, P. Cruz-Hernández
{"title":"Environmental Assessment and Management of Phosphogypsum According to European and United States of America Regulations","authors":"F. Macías, R. Pérez-López, C. R. Cánovas, S. Carrero, P. Cruz-Hernández","doi":"10.1016/J.PROEPS.2016.12.178","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2016.12.178","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"100 1","pages":"666-669"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"83348074","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 53
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