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Hydrological dataset of a sub-humid continental plain basin (Buenos Aires, Argentina)

机译:子湿润大陆普通盆地的水文数据集(布宜诺斯艾利斯,阿根廷)

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The Chaco-Pampean Plain (Argentina) is the strongest economic region and the most inhabited in the country, comprising approximately 66% of the country's population (26,500 million) . In this region, surface slopes are very low (<0.1%) and due to the current climatological features, floods and droughts alternate over time. Salinity and alkalinity of water and soil increase towards the flattest sector of the basin, as well as the contents of arsenic and fluoride, which restrict their human use. Worldwide, population growth and global warming, in addition to political decisions, are leading to abrupt land use changes. Under this premise, identifying and quantifying the hydrological processes that control water quantity and its chemical quality become an imperative task . This data article provides a long-term hydrological dataset from a sector of the Chaco-Pampean Plain, the Del Azul creek basin. Hydrological data such as flow rates and piezometric levels, and physical–chemical (i.e., major and minor solutes, and trace elements) and isotopic (δ18O, δ2H; andd-excess) data from rainwater, surface (creek and wetland) and groundwater (at two depths) are available. Rainwater samples are derived from three precipitation collectors installed at different altitudes (monitoring period: 2010–2019;n?=?57). Surface water samples were collected at three sampling sites located along the Del Azul Creek and six wetlands (monitoring period: 2018–2019;n?=?12). Groundwater samples were collected from 17 piezometers with depths ranging between 3 and 10?m, and from 12 piezometers of 30?m depth, all located throughout the entire basin (monitoring period: 2018–2019;n?=?115). Sampling campaigns were performed during the austral dry (summer) and wet (spring) seasons. This dataset provides useful information to understand a) how water moves from recharge to discharge areas, b) how water acquires salinity, and c) how particular solutes of concern, such as arsenic and fluoride, are distributed in space and time across in an extensive plain.
机译:Chaco-Pampean Plain(阿根廷)是最强的经济区和全国最有居住的国家,包括该国约66%的人口(265亿)。在该地区,表面斜坡非常低(<0.1%),由于目前的气候功能,洪水和干旱随着时间的推移。水和土壤盐度和土壤碱度朝向盆地的扁平扇区,以及砷和氟化物的含量,限制了他们的人类使用。除了政治决策之外,世界范围内,人口增长和全球变暖导致突然利用土地使用变化。在此前提下,识别和量化控制水量的水文过程及其化学品质量成为必要的任务。该数据文章提供了来自Del Azul Creek盆地的Chaco-Pampean平原部门的长期水文数据集。水文数据如流量和压力水平,以及来自雨水,表面(Creek和Wetheldland)和地下水(在两个深处)可用。雨水样本源自三个安装在不同高度的降水收集器(监测期:2010-2019; n?=?57)。在沿着Del Azul Creek和六次湿地的三个取样位点收集地表水样品(监测期:2018-2019; N?=?12)。从17个压力仪收集地下水样品,深度在3到10μm的深度范围内,以及12个压力计30?M深度,所有位于整个盆地(监测期:2018-2019; n?=?115)。在澳大利亚(夏季)和潮湿(春季)季节中进行了采样运动。该数据集提供了理解A)水从充电区域,B)如何水分地获取盐度,以及C)如何在广泛的空间和时间内分布在砷和氟化物中的特定求解清楚的。

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