Procedia Earth and Planetary Science最新文献

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Characterization of Main AMD Inputs to the Odiel River Upper Reach (SW Spain) Odiel河上游(西班牙西南部)主要AMD输入特征
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2016.12.161
J. Riera, C. R. Cánovas, M. Olías
{"title":"Characterization of Main AMD Inputs to the Odiel River Upper Reach (SW Spain)","authors":"J. Riera, C. R. Cánovas, M. Olías","doi":"10.1016/J.PROEPS.2016.12.161","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2016.12.161","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"29 1","pages":"602-605"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"73990778","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: 5
Iodine Speciation and its Potential Influence on Iodine Enrichment in Groundwater from North China Plain 华北平原地下水碘形态及其对碘富集的潜在影响
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.069
Junxia Li, Kun Qian, Yijun Yang, Xianjun Xie
{"title":"Iodine Speciation and its Potential Influence on Iodine Enrichment in Groundwater from North China Plain","authors":"Junxia Li,&nbsp;Kun Qian,&nbsp;Yijun Yang,&nbsp;Xianjun Xie","doi":"10.1016/j.proeps.2016.12.069","DOIUrl":"10.1016/j.proeps.2016.12.069","url":null,"abstract":"<div><p>In order to reveal the pattern of spatial distribution of iodine in groundwater at North China Plain (NCP), a total of 136 groundwater samples were collected along the regional groundwater flow paths. The results showed that groundwater iodine ranged from 1.51 to 1106μg/L, and 31.4% of the samples have iodine concentrations higher than 150μg/L. High iodine groundwater samples are mainly observed in the coastal area of Bohai sea, and well depths greater than 350 m. The results of iodine speciation analysis showed that groundwater iodide, iodate and organic iodine had the ranges of &lt;0.025∼854μg/L, &lt;0.035∼293μg/L and &lt;10∼296μg/L, respectively, indicating that iodide is the dominant species of iodine in groundwater at NCP. Iodate is only observed in groundwater with Eh values higher than 0mV, suggesting that groundwater redox condition is the main factor controlling iodine speciation. The widespread sub-reducing/reducing condition and low affinity of iodide are the two main factors promoting the iodine enrichment in groundwater.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 312-315"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.069","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79275667","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: 6
The Mexican Center of Innovation in Geothermal Energy, CeMIE-Geo: Challenges and Opportunities ☆ 墨西哥地热能创新中心,CeMIE-Geo:挑战与机遇
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.013
J. M. R. Jones, T. Kretzschmar
{"title":"The Mexican Center of Innovation in Geothermal Energy, CeMIE-Geo: Challenges and Opportunities ☆","authors":"J. M. R. Jones, T. Kretzschmar","doi":"10.1016/J.PROEPS.2017.01.013","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2017.01.013","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"33 1","pages":"905-908"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"84462518","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
Contrasting Transit Times and Water-rock Interaction in Australian Upland Catchments Draining Peatland and Eucalypt Forest 对比运输时间和水岩相互作用在澳大利亚高地集水区排水泥炭地和桉树林
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.032
Ian Cartwright , Uwe Morgenstern
{"title":"Contrasting Transit Times and Water-rock Interaction in Australian Upland Catchments Draining Peatland and Eucalypt Forest","authors":"Ian Cartwright ,&nbsp;Uwe Morgenstern","doi":"10.1016/j.proeps.2016.12.032","DOIUrl":"10.1016/j.proeps.2016.12.032","url":null,"abstract":"<div><p>Catchments draining upland peat in the Victorian Alps, Australia contain water that has <sup>3</sup>H activities closely similar to modern rainfall implying very short transit times (&lt;2 years). By contrast the water that drains adjacent eucalypt forest has mean transit times of several years to decades. The differences in transit times most likely reflect the higher evapotranspiration rates in the eucalypt forests that results in lower infiltration rates and slower rates of flow. Major ion concentrations reflect a combination of evapotranspiration and water-rock interaction and may be used to provide first-order estimates of transit times. The short transit times in the peat imply that it does not represent a long-term store of water for the river systems during drought. The peat is also highly susceptible to drying during low rainfall periods, which renders it vulnerable to the periodic bushfires that impact the region.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 140-143"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.032","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"85494720","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
Sources of Geothermal Water in Jiangxi Province, SE-China: Evidences from Hydrochemistry and Isotopic Composition 中国东南部江西省地热水来源:水化学和同位素组成证据
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.057
Jiale Li, B. Gao, Yihui Dong, Gongxin Chen, Zhanxue Sun
{"title":"Sources of Geothermal Water in Jiangxi Province, SE-China: Evidences from Hydrochemistry and Isotopic Composition","authors":"Jiale Li, B. Gao, Yihui Dong, Gongxin Chen, Zhanxue Sun","doi":"10.1016/J.PROEPS.2017.01.057","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2017.01.057","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"40 1","pages":"837-840"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"81777470","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: 0
Modeling of the Hydrothermal Alteration at the Exploration and Production Well in Ömerbeyli, Germencik, Aydın, Turkey 土耳其Aydın Germencik Ömerbeyli探采井热液蚀变模拟
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.058
Onur Melih Kasımoğlu , Ismail Hakkı Karamanderesi , Nevzat Özgür , Tuğba Arife Çalışkan , Ibrahim Ibrahim Abubakar
{"title":"Modeling of the Hydrothermal Alteration at the Exploration and Production Well in Ömerbeyli, Germencik, Aydın, Turkey","authors":"Onur Melih Kasımoğlu ,&nbsp;Ismail Hakkı Karamanderesi ,&nbsp;Nevzat Özgür ,&nbsp;Tuğba Arife Çalışkan ,&nbsp;Ibrahim Ibrahim Abubakar","doi":"10.1016/j.proeps.2016.12.058","DOIUrl":"10.1016/j.proeps.2016.12.058","url":null,"abstract":"<div><p>The study area is situated 3 km NE of Ömerbeyli located 12 km W of province capital of Aydın in western Anatolia, Turkey. Here, an exploration, production and reinjection well with a depth of approximately 2.200 m has been drilled. In this well, we have collected 38 samples as rock fragments, in order to investigate hydrothermal alteration by x-ray diffraction and microscopical methods. In this geothermal area, the hydrothermal alteration mineralogy depends upon (i) temperature of geothermal system, (ii) pressure of the system, (iii) type of the rocks in reservoir, (iv) permeability of the reservoir rocks, (v) geochemical composition of the reservoir rocks and (vi) stability of the minerals of reservoir rocks. There is a close relationship between geothermal system and hydrothermal alteration. With respect to this relationship, the monitoring of geothermal systems can be ensured by the parameters such as temperatures and hydrothermal alteration zones providing that the hydrothermal alteration mineralogy has been investigated particularly. Therefore, the hydrothermal alteration mineralogy of the exploration, production and reinjection well with a depth of approximately 2.200 m in Ömerbeyli has been revealed.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 181-184"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.058","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"82318981","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: 0
Unraveling the Formation of Large Amounts of Calcite Scaling in Geothermal Wells in the Bavarian Molasse Basin: A Reactive Transport Modeling Approach 巴伐利亚Molasse盆地地热井中大量方解石结垢的形成:反应输运建模方法[j]
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.087
Christoph Wanner , Florian Eichinger , Thomas Jahrfeld , Larryn W. Diamond
{"title":"Unraveling the Formation of Large Amounts of Calcite Scaling in Geothermal Wells in the Bavarian Molasse Basin: A Reactive Transport Modeling Approach","authors":"Christoph Wanner ,&nbsp;Florian Eichinger ,&nbsp;Thomas Jahrfeld ,&nbsp;Larryn W. Diamond","doi":"10.1016/j.proeps.2016.12.087","DOIUrl":"10.1016/j.proeps.2016.12.087","url":null,"abstract":"<div><p>Results from reactive transport simulations performed for the geothermal plant in Kirchstockach, located in the Bavarian Molasse Basin in southern Germany, are presented to unravel the formation of calcite scaling. Simulation results successfully predict the calcite scaling profile observed along the production well if supersaturation with respect to calcite is specified for the model water leaving the pump at 800 m depth. This observation is in good agreement with a previous study suggesting that gas exsolution (i.e., boiling) occurring at the pump due to an unwanted pressure drop is the most likely driver for the formation of those calcite scalings.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 344-347"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.087","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"80151017","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
Compaction of Muddy Sediment and Its Significance to Groundwater Chemistry 泥质沉积物的压实作用及其对地下水化学的意义
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/j.proeps.2016.12.099
Yanjun Liu , Teng Ma , Yao Du
{"title":"Compaction of Muddy Sediment and Its Significance to Groundwater Chemistry","authors":"Yanjun Liu ,&nbsp;Teng Ma ,&nbsp;Yao Du","doi":"10.1016/j.proeps.2016.12.099","DOIUrl":"10.1016/j.proeps.2016.12.099","url":null,"abstract":"<div><p>Muddy sediment is one of the most common aquitards. During the burial compaction of mud, the pressure and temperature of strata increased with depth, in which some complex physical, chemical and biological reactions occurred. Meanwhile, a large amount of porewater, which interacts with microbes, organic matter and minerals in mud, would be discharged into adjacent aquifers. Numerous previous efforts by geologists have put forward some evidences, indicating that a portion of components (such as ions and nutrient) in groundwater are from muddy sediments. This paper provides a brief overview of efforts on different reactions in pore water in which environments change from oxidation to reduction and interfaces between the aquitard and the aquifer. Then, in the view of geological evolution, an idea is proposed that mud provided not only water but also material source for adjacent aquifer during its compaction and burial. In order to further understand the genesis of natural groundwater, especially natural inferior groundwater and brine, the diagenetic reaction and mineralization, water-rock interaction during the compaction of sediment should be considered, which will be of great significance in hydrogeology.</p></div>","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"17 ","pages":"Pages 392-395"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.proeps.2016.12.099","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"78635143","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: 8
Using Large Databases of Groundwater Chemistry in the Northern Midwest USA: The Effects of Geologic and Anthropogenic Factors 利用美国中西部北部地下水化学的大型数据库:地质和人为因素的影响
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2017.01.047
R. Wanty, A. Manning, Michael R Johnson, S. Kalkhoff, J. Garrett, J. Morrison, S. DaPelo, J. Mauk
{"title":"Using Large Databases of Groundwater Chemistry in the Northern Midwest USA: The Effects of Geologic and Anthropogenic Factors","authors":"R. Wanty, A. Manning, Michael R Johnson, S. Kalkhoff, J. Garrett, J. Morrison, S. DaPelo, J. Mauk","doi":"10.1016/J.PROEPS.2017.01.047","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2017.01.047","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"1 1","pages":"806-809"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"89565066","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: 0
Temporal variations of REE in several AMD sources of the Odiel River (SW Spain) 西班牙西南部Odiel河几个AMD源稀土元素的时间变化
Procedia Earth and Planetary Science Pub Date : 2017-01-01 DOI: 10.1016/J.PROEPS.2016.12.160
M. Olías, C. R. Cánovas, J. Riera
{"title":"Temporal variations of REE in several AMD sources of the Odiel River (SW Spain)","authors":"M. Olías, C. R. Cánovas, J. Riera","doi":"10.1016/J.PROEPS.2016.12.160","DOIUrl":"https://doi.org/10.1016/J.PROEPS.2016.12.160","url":null,"abstract":"","PeriodicalId":101039,"journal":{"name":"Procedia Earth and Planetary Science","volume":"79 1","pages":"706-709"},"PeriodicalIF":0.0,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"89919024","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: 5
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