干旱区生态环境知识资源中心(Arid): Hydrochemistry, delta D and delta O-18 to explain the distribution of water quality in a karst setting in the semi-arid region of Northeast Mexico

Arid

DOI	10.1007/s12665-020-09310-x
	Hydrochemistry, delta D and delta O-18 to explain the distribution of water quality in a karst setting in the semi-arid region of Northeast Mexico
	Ventura-Houle, Rene; Guevara-Mansilla, Oscar; Requena-Lara, Glenda; Andrade-Limas, Elizabeth; Lopez-Altarriba, Elisenda
通讯作者	Ventura-Houle, R (corresponding author), Univ Autonoma Tamaulipas, Ctr Univ Victoria, Fac Ingn & Ciencias, Ciudad Victoria 87134, Tamaulipas, Mexico.
来源期刊	ENVIRONMENTAL EARTH SCIENCES
ISSN	1866-6280
EISSN	1866-6299
出版年	2021
卷号	80 期号:1
英文摘要	Characterization of the groundwater flow systems can be used in conjunction with the geochemical evolution of groundwater to assess water-rock interaction processes, time of residence, and the regional hydrogeochemical evolution system. To identify the regime of groundwater flow, we consider it is essential to localize the geographic components of the hydrologic cycle, where the geologic environment determines the functional areas such as the recharge and discharge areas and the dynamics of water availability of the aquifer, as well as water quality. In this paper, we analyzed the groundwater flow systems on a section of chalky rocks, known as Plataforma Valle-San Luis Potosi (PVSL), located in the state of Tamaulipas, Northeast Mexico. The groundwater from the study area has dissolved Ca2+ and HCO3- as dominant ions; average concentrations are 118.9 and 253.9 mg/L, respectively. Thought to be derived from calcite dissolution, basically under the influence of the massif of the Sierra Madre Oriental, a karst Quaternary environment denominated El Abra Formation, a sedimentary rocks geology that dominates the regional geology. We used the cluster analysis to classify the primary element concentrations in two groups and three subgroups, where we could identify a local, intermediate, and regional flow. Defining the evolution of groundwater from recent waters on Ca2+ to HCO3- and dominance of SO4-2 to waters with more residence period, associated with the dissolution of gypsum from the Guaxcama Formation. That's was corroborate by utilization of delta D and delta 18O data which allow the identification of the recharge areas with mean values from - 7.94 delta 18O (parts per thousand) and 53.84 delta D (parts per thousand) on recharge areas, and - 8.19 parts per thousand delta O-18 and 57.83 parts per thousand delta D on intermediate flow. This result contributes to describe the geochemical process of groundwater and how it interacts with geological formations with El Abra Formation, the most crucial geological-water unity for the study area.
英文关键词	Environmental isotopes Groundwater flow system hydrochemistry Karst aquifer Mexico
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000606914700005
WOS关键词	GROUNDWATER-FLOW SYSTEMS ; EVOLUTION ; AQUIFER ; MANAGEMENT ; RESOURCES ; CHEMISTRY ; SIERRA ; BASIN
WOS类目	Environmental Sciences ; Geosciences, Multidisciplinary ; Water Resources
WOS研究方向	Environmental Sciences & Ecology ; Geology ; Water Resources
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/347853
作者单位	[Ventura-Houle, Rene; Andrade-Limas, Elizabeth; Lopez-Altarriba, Elisenda] Univ Autonoma Tamaulipas, Ctr Univ Victoria, Fac Ingn & Ciencias, Ciudad Victoria 87134, Tamaulipas, Mexico; [Guevara-Mansilla, Oscar] Inst Potosino Invest Cient & Tecnol, Camino La Presa San Jose 2055,Lomas 4 Secc, San Luis Potosi 78216, Slp, Mexico; [Requena-Lara, Glenda] Univ Autonoma Tamaulipas, Inst Ecol Aplicada, Div Golfo 356, Ciudad Victoria 87134, Tamaulipas, Mexico
推荐引用方式 GB/T 7714	Ventura-Houle, Rene,Guevara-Mansilla, Oscar,Requena-Lara, Glenda,et al. Hydrochemistry, delta D and delta O-18 to explain the distribution of water quality in a karst setting in the semi-arid region of Northeast Mexico[J],2021,80(1).
APA	Ventura-Houle, Rene,Guevara-Mansilla, Oscar,Requena-Lara, Glenda,Andrade-Limas, Elizabeth,&Lopez-Altarriba, Elisenda.(2021).Hydrochemistry, delta D and delta O-18 to explain the distribution of water quality in a karst setting in the semi-arid region of Northeast Mexico.ENVIRONMENTAL EARTH SCIENCES,80(1).
MLA	Ventura-Houle, Rene,et al."Hydrochemistry, delta D and delta O-18 to explain the distribution of water quality in a karst setting in the semi-arid region of Northeast Mexico".ENVIRONMENTAL EARTH SCIENCES 80.1(2021).