José Iván Morales-Arredondo, María Aurora Armienta Hernández, Joel Edmundo Ortega-Gutiérrez, Elisa Cuellar Ramirez
{"title":"对墨西哥城都会区封闭湖底火山沉积盆地含水层中 NO3- 和 N-NH3 含量来源的水文地质化学和同位素评估","authors":"José Iván Morales-Arredondo, María Aurora Armienta Hernández, Joel Edmundo Ortega-Gutiérrez, Elisa Cuellar Ramirez","doi":"10.1007/s11631-023-00668-w","DOIUrl":null,"url":null,"abstract":"<div><p>To explain the presence and spatial distribution of NO<sub>3</sub><sup>−</sup> and N–NH<sub>3</sub> in the Aquifer of the Metropolitan Area of Mexico City (AMAMC), a hydrogeochemical and isotopic analysis using <sup>13</sup>C<sub>DIC</sub> (as well as the stable isotopes <sup>18</sup>O and <sup>2</sup>H) in groundwater was conducted. This aquifer is located in an old closed lacustrine volcano-sedimentary basin; some wells hosted in the semi-confined zone contain high N–NH<sub>3</sub> concentrations, while others present NO<sub>3</sub><sup>−</sup> contents in the recharge zones (hosted in an oxidizing environment). In this study, a change in the isotopic signature (primarily in <sup>18</sup>O and <sup>2</sup>H) was observed from the recharge zones to the basin center in some of the wells with high NO<sub>3</sub><sup>−</sup> concentrations, this behavior can be attributed to evaporation during the incorporation of recently infiltrated water. In addition, the results for <sup>13</sup>C (along with <sup>2</sup>H) in wells with the highest N–NH<sub>3</sub> concentrations exhibited an atypically broad range of values. Results indicated the occurrence of hydrogeochemical and/or biochemical processes in the aquifer (in an oxidizing or reducing environment), such as organic degradation, bacterial decomposition (primarily in the ancient Lake Texcoco and which acts as a natural sink for carbon, nitrogen, sulfur, and phosphorus), besides rock weathering and dissolution, which may be responsible for a very marked isotopic modification of the <sup>13</sup>C (and, to a lesser extent, <sup>2</sup>H). Methanotrophic bacterial activity and methanogenic activity may be related to N–NH<sub>3</sub> removal processes by oxidation and residual water incorporation respectively, whereas the increase in the NO<sub>3</sub><sup>−</sup> content in some wells is due to the recent contribution of poor-quality water due to contamination.</p></div>","PeriodicalId":7151,"journal":{"name":"Acta Geochimica","volume":"43 4","pages":"719 - 736"},"PeriodicalIF":1.4000,"publicationDate":"2024-01-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s11631-023-00668-w.pdf","citationCount":"0","resultStr":"{\"title\":\"Hydrogeochemical and isotopic assessment of the origin of NO3− and N–NH3 contents in the aquifer located in a closed lacustrine volcano-sedimentary basin in the metropolitan area of Mexico City\",\"authors\":\"José Iván Morales-Arredondo, María Aurora Armienta Hernández, Joel Edmundo Ortega-Gutiérrez, Elisa Cuellar Ramirez\",\"doi\":\"10.1007/s11631-023-00668-w\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>To explain the presence and spatial distribution of NO<sub>3</sub><sup>−</sup> and N–NH<sub>3</sub> in the Aquifer of the Metropolitan Area of Mexico City (AMAMC), a hydrogeochemical and isotopic analysis using <sup>13</sup>C<sub>DIC</sub> (as well as the stable isotopes <sup>18</sup>O and <sup>2</sup>H) in groundwater was conducted. This aquifer is located in an old closed lacustrine volcano-sedimentary basin; some wells hosted in the semi-confined zone contain high N–NH<sub>3</sub> concentrations, while others present NO<sub>3</sub><sup>−</sup> contents in the recharge zones (hosted in an oxidizing environment). In this study, a change in the isotopic signature (primarily in <sup>18</sup>O and <sup>2</sup>H) was observed from the recharge zones to the basin center in some of the wells with high NO<sub>3</sub><sup>−</sup> concentrations, this behavior can be attributed to evaporation during the incorporation of recently infiltrated water. In addition, the results for <sup>13</sup>C (along with <sup>2</sup>H) in wells with the highest N–NH<sub>3</sub> concentrations exhibited an atypically broad range of values. Results indicated the occurrence of hydrogeochemical and/or biochemical processes in the aquifer (in an oxidizing or reducing environment), such as organic degradation, bacterial decomposition (primarily in the ancient Lake Texcoco and which acts as a natural sink for carbon, nitrogen, sulfur, and phosphorus), besides rock weathering and dissolution, which may be responsible for a very marked isotopic modification of the <sup>13</sup>C (and, to a lesser extent, <sup>2</sup>H). Methanotrophic bacterial activity and methanogenic activity may be related to N–NH<sub>3</sub> removal processes by oxidation and residual water incorporation respectively, whereas the increase in the NO<sub>3</sub><sup>−</sup> content in some wells is due to the recent contribution of poor-quality water due to contamination.</p></div>\",\"PeriodicalId\":7151,\"journal\":{\"name\":\"Acta Geochimica\",\"volume\":\"43 4\",\"pages\":\"719 - 736\"},\"PeriodicalIF\":1.4000,\"publicationDate\":\"2024-01-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://link.springer.com/content/pdf/10.1007/s11631-023-00668-w.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Acta Geochimica\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s11631-023-00668-w\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Geochimica","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s11631-023-00668-w","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Hydrogeochemical and isotopic assessment of the origin of NO3− and N–NH3 contents in the aquifer located in a closed lacustrine volcano-sedimentary basin in the metropolitan area of Mexico City
To explain the presence and spatial distribution of NO3− and N–NH3 in the Aquifer of the Metropolitan Area of Mexico City (AMAMC), a hydrogeochemical and isotopic analysis using 13CDIC (as well as the stable isotopes 18O and 2H) in groundwater was conducted. This aquifer is located in an old closed lacustrine volcano-sedimentary basin; some wells hosted in the semi-confined zone contain high N–NH3 concentrations, while others present NO3− contents in the recharge zones (hosted in an oxidizing environment). In this study, a change in the isotopic signature (primarily in 18O and 2H) was observed from the recharge zones to the basin center in some of the wells with high NO3− concentrations, this behavior can be attributed to evaporation during the incorporation of recently infiltrated water. In addition, the results for 13C (along with 2H) in wells with the highest N–NH3 concentrations exhibited an atypically broad range of values. Results indicated the occurrence of hydrogeochemical and/or biochemical processes in the aquifer (in an oxidizing or reducing environment), such as organic degradation, bacterial decomposition (primarily in the ancient Lake Texcoco and which acts as a natural sink for carbon, nitrogen, sulfur, and phosphorus), besides rock weathering and dissolution, which may be responsible for a very marked isotopic modification of the 13C (and, to a lesser extent, 2H). Methanotrophic bacterial activity and methanogenic activity may be related to N–NH3 removal processes by oxidation and residual water incorporation respectively, whereas the increase in the NO3− content in some wells is due to the recent contribution of poor-quality water due to contamination.
期刊介绍:
Acta Geochimica serves as the international forum for essential research on geochemistry, the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth‘s crust, its oceans and the entire Solar System, as well as a number of processes including mantle convection, the formation of planets and the origins of granite and basalt. The journal focuses on, but is not limited to the following aspects:
• Cosmochemistry
• Mantle Geochemistry
• Ore-deposit Geochemistry
• Organic Geochemistry
• Environmental Geochemistry
• Computational Geochemistry
• Isotope Geochemistry
• NanoGeochemistry
All research articles published in this journal have undergone rigorous peer review. In addition to original research articles, Acta Geochimica publishes reviews and short communications, aiming to rapidly disseminate the research results of timely interest, and comprehensive reviews of emerging topics in all the areas of geochemistry.