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| 1 | Arsenic and fluoride in the groundwater of Mexico显示文摘 | Armienta M A Segovia N | 2008 | Environmental Geochemistry and Health2008，30，： | 1 |
| 2 | Groundwater arsenic variations:the role of local geology and rainfall显示文摘 | Rodríguez R Ramos JA Armienta A | 2004 | Appl Geochem2004，19，： | 1 |
| 3 | Variations of Pb in a mine-impacted tropical river,Taxco,Mexico:Use of geochemical,isotopic and statistical tools显示文摘 | Arcega-Cabrera F Armienta M A Daesslé L W Castillo-Blum S E Talavera O Dótor A | 2009 | Applied Geochemistry2009，24，： | 1 |
| 4 | Distribution,origin and fate of chromium in soils in Guanajuato,Mexico显示文摘 | Armienta M A Rodriguez R Ceniceros N | 1996 | Environmental Pollution1996，91，3： | 1 |
| 5 | Solid-phase control on the mobility of potentially toxic elements in an abandoned lead/zinc mine tailings impoundment, Taxco, Mexico显示文摘 | ROMERO F M ARMIENTA M A GONZALEZ- HERNANDEZ G | 2007 | Applied Geochemistry2007，22，1： | 1 |
| 6 | The role of arsenic-bearing rocks in groundwater pollution at Zimapan Valley Mexico显示文摘 | Armienta M A Villasenor G Rodriguez R | 2001 | Environmental Geology2001，40，2： | 1 |
| 7 | Geochemistry of metals from mine tailings in taxco, mexico显示文摘 | ARMIENTA M A TALAVERA O MORTON O | 2003 | Bulletin of Environmental Contamination and Toxicology2003，71，2： | 1 |
| 8 | Groundwater arsenic variations: the role of local geology and rainfall 显示文摘 | Rodriguez R Ramos JA Armienta A | 2004 | Appl Geochem2004，19，： | 1 |
| 9 | Arsenic distribmion in mesquile (Prosopis laevigala)and huizache (Acacia farnesiana)in the Zim apan mining area, Mexico 显示文摘 | Armienta M A Ongley L K Rodriguez R | 2008 | Geochemistry: Exploration Environment Anabysis2008，8，2： | 1 |
| 10 | Hydrogeochemical behavior of chromium in the unsaturated zone and in the aquifer of Leon Valley, Mexico 显示文摘 | Armienta M A Qere A | 1995 | Water Air and Soil Pollution1995，84，： | 1 |
| 11 | Arsenic and fluoride in thegroundwater of Mexico 显示文摘 | ARMIENTA M A SEGOVIA N | 2008 | Environmental Geochemistry andHealth2008，30，4： | 1 |
| 12 | Solid-phase control on the mobility of potentially toxic elements in an abandoned lead/zinc mine tailings impoundment, Taxco, Mexico 显示文摘 | Romero F M Armienta M A Gonzalez-Hernandez G | 2007 | Applied Geochemistry2007，22，： | 1 |
| 13 | One century of arsenic exposure in Latin America: A review of history and occurrence from 14 countries显示文摘 | Jochen Bundschuh Marta I. Litter Faruque Parvez Gabriela Román-Ross Hugo B. Nicolli Jiin-Shuh Jean Chen-Wuing Liu Dina López María A. Armienta Luiz R.G. Guilherme Alina Gomez Cuevas Lorena Cornejo Luis Cumbal Regla Toujaguez | 2011 | Science of the Total Environment2011，，： | 1 |
| 14 | Use of δ^(18)O, δ^(13)C and NO_(3)^(-) to identify hydrogeochemical processes related to contamination in an aquifer located in central Mexico显示文摘In this work,an isotopic analysis of δ^(18)O,δ^(13)C,and NO_(3)^(-) concentrations was carried out to identify the origin and the processes related to the contamination of an aquifer located in the state of Guanajuato,Mexico.The research identified the possible sources of δ^(13)C in groundwater.During groundwater flow,CO_(2) participates in different hydrogeochemical reactions in which the dissolution of carbonates or biochemical processes related to biodegradation stand out.Isotopic data of δ^(13)C,δ^(18)O,and the hydrogeochemical behavior of NO_(3)^(-) and HCO_(3)^(-) in water,in addition to isotopic data and the chemical composition of limestones in the study area,were determined to establish the isotopic signature and the processes undergone by the rocks.The isotopic signature of rock and water samples indicated that metamorphic limestones contributed with carbon dioxide to deep groundwater,while in the upper aquifer,bacterial metabolic reactions during nitrification–denitrification could modify the isotopic signature of δ^(13)C in some wells,although atmospheric contribution also plays a role.The modification of the carbon isotopic component is related to the precipitation of calcite in specific regions of the study area,input of atmospheric CO_(2),and soil(e.g.the possible participation of C4-type plants in the assimilation-release of carbon).This process is not confirmed or completely ruled out in this study since agriculture is excessively developed throughout the region.The joint interpretation of isotopic values and the hydrogeochemical behavior of major and conservative elements help in identifying possible pollution processes in which different carbon sources are related. | JoséIván Morales-Arredondo María Aurora Armienta Hernández Fátima Juárez-Aparicio Jorge Federico Landa-Arreguín Itzamna Zaknite Flores-Ocampo | 2022 | Acta Geochimica2022，41，3： | 0 |
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