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Sr Isotopes as Mixing and Lithological Tracers; The Ebro River Basin☆ Sr同位素混合示踪及岩性示踪埃布罗河流域
Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.028
P. Négrel, E. Petelet-Giraud, R. Millot
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引用次数: 3
The Geochemistry of Hydraulic Fracturing Fluids 水力压裂液的地球化学研究
Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.011
Avner Vengosh , Andrew Kondash , Jennie Harkness , Nancy Lauer , Nathaniel Warner , Thomas H. Darrah

The inorganic geochemistry of hydraulic fracturing fluids is reviewed with new insights on the role of entrapped formation waters in unconventional shale gas and tight sand formations on the quality of flowback and produced waters that are extracted with hydrocarbons. The rapid increase of the salinity of flowback fluids during production, combined with geochemical and isotopic changes, indicate mixing of the highly saline formation water with the injected water. The salinity increase suggests that the volume of the injected water that is returned to the surface with the flowback water is much smaller than previous estimates, and thus the majority of the injected water is retained within the shale formations. The high salinity of the flowback and produced water is associated with high concentrations of halides, ammonium, metals, metalloids, and radium nuclides that pose environmental and human health risks upon the release of the hydraulic fracturing fluids to the environment.

综述了水力压裂液的无机地球化学特征,并对非常规页岩气和致密砂岩地层中圈闭地层水对返排和采出水质量的影响有了新的认识。在生产过程中,返排液矿化度的快速升高,结合地球化学和同位素变化,表明高盐地层水与注入水混合。盐度的增加表明,与返排水一起返回地表的注入水量比之前估计的要小得多,因此大部分注入水被保留在页岩地层中。返排水和采出水的高盐度与高浓度的卤化物、铵、金属、类金属和镭核素有关,在将水力压裂液释放到环境中时,这些物质会对环境和人类健康构成风险。
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引用次数: 43
Hydrogeochemical Assessment of Tibães Waters (NW Portugal) tib<s:1>水域(葡萄牙西北部)水文地球化学评价
Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.030
M. Afonso, M. E. Lopes, H. Chaminé
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引用次数: 1
Great Role of W.M. Edmunds in the Development of Hydrogeochemistry in Russia 埃德蒙兹在俄罗斯水文地球化学发展中的重要作用
Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.054
O.V. Chudaev, V.A. Chudaeva

This article discusses the joint work of Professor W.M. Edmunds (UK) with his Russian colleagues. He had an important role in the development of hydrogeochemistry in Russia. He was an initiator of the joint research projects with Russian scientists and was actively supporting the idea of holding international conferences on the territory of Russia. In addition, as a follower of V.I. Vernadsky, he was actively promoting Vernadsky's ideas outside of Russia.

本文讨论了英国埃德蒙兹教授与俄罗斯同事的合作工作。他在俄罗斯水文地球化学的发展中发挥了重要作用。他是与俄罗斯科学家联合研究项目的发起人,并积极支持在俄罗斯领土上举行国际会议的想法。此外,作为维尔纳德斯基的追随者,他在俄罗斯境外积极推广维尔纳德斯基的思想。
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引用次数: 0
The Occurrences of Ca2UO2(CO3)3 Complex in Fe(II) Containing Deep Groundwater at Forsmark, Eastern Sweden☆ 瑞典东部Forsmark含铁(II)深层地下水中Ca2UO2(CO3)3络合物的赋存特征[j]
Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2016.12.111
E. Tullborg, J. Suksi, G. Geipel, Lindsay Krall, L. Auqué, M. Gimeno, I. Puigdomenech
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引用次数: 17
Laboratory Insights into Water-rock-CO2 Interactions Controlling the Isotopic Composition of CO2 Leaking from Storage Sites 水-岩石-二氧化碳相互作用控制二氧化碳从储存地点泄漏的同位素组成的实验室见解
Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.052
M. Nightingale, B. Mayer, M. Shevalier, S. Yun
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引用次数: 0
FEBEX In-Situ Test: Preliminary Results of the Geochemical Characterization of the Metal/Bentonite Interface FEBEX原位测试:金属/膨润土界面地球化学表征的初步结果
Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.045
E. Torres, M. Turrero, D. Moreno, L. Sanchez, A. Garralón
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引用次数: 4
Study of Water-rock Interaction in Sulfide Mining Tailings using Geochemical and Geoelectrical Methods 利用地球化学和地电方法研究硫化尾矿中水岩相互作用
Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.019
Nataliya Yurkevich , Svetlana Bortnikova , Vladimir Olenchenko , Nataliya Abrosimova , Olga Saeva , Yuriy Karin

Sulphide-bearing mill wastes of the Ursk Ore Processing Plant situated in the Kemerovo region (Russia) were investigated in the 2013 – 2015. Multipurpose studies of the Ursk mining tailings allowed to determine the composition of the wastes pore waters, acid mine drainages and affected groundwater. Electrical resistivity tomography (ERT) was used to trace the geoelectric zoning of the wastes, expressed as a consistent change of the electrical resistivity from zone to zone. Layers with low resistivity indicate areas with pore spaces filled by highly mineralized solutions with high concentrations of Cu, Zn, Cd, As, and Sb up to 12 g/L in total.

2013年至2015年,对位于克麦罗沃地区(俄罗斯)的乌尔斯克矿石加工厂的含硫化物废物进行了调查。对乌尔斯克采矿尾矿的多目的研究可以确定废物孔隙水、酸性矿山排水和受影响地下水的组成。利用电阻率层析成像技术(ERT)对垃圾的地电分区进行了跟踪,并将其表示为各带间电阻率的一致变化。在低电阻率层中,孔隙空间被Cu、Zn、Cd、As和Sb等元素的高矿化溶液填充,最高可达12 g/L。
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引用次数: 8
Volcanic Conduits of the Chã das Caldeiras Caldera (Fogo Island, Cape Verde) – REE and Fe Crystalchemistry Chã das Caldeiras火山口火山导管(佛得角Fogo岛)- REE和Fe晶体化学
Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.023
R. Marques, M. Prudencio, J. Waerenborgh, F. Rocha, E. F. Silva, M. Dias, Bruno J. C. Vieira, J. Marques, D. Franco
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引用次数: 3
Hydrothermal Systems in the Salt Domes of South Iran 伊朗南部盐丘的热液系统
Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.016
M. Mortazavi, S. Heuss-Aßbichler, M. Shahri
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引用次数: 11
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