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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >A new approach for describing the relationship between electrical conductivity and major anion concentration in natural waters
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A new approach for describing the relationship between electrical conductivity and major anion concentration in natural waters

机译:描述天然水中电导率与主要阴离子浓度之间关系的新方法

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The concentrations of dissolved cations and anions are fundamental to the water quality of groundwaters, particularily pertaining to their use as a drinking water source. Currently, assessment of total dissolved solids requires laboratory-based analysis of each ionic species, and cannot be reliably tested in the field. Here, a new method is developed that distinguishes between changes in ion concentration or water type based upon field measurement of Electric Conductivity (EC) and the concentration of only one anion. The approach operates under the assumption that all cations contribute equally to EC, whereas almost twice as much of the HCO3- ion is needed to produce the same effect on total solute EC as those of Cl~- or SO42- ions for waters at neutral pH. Therefore, many groundwater systems can be treated as two anion systems when the groundwater chemical type and solute EC relationship is assessed. Moreover, by assuming neutral charge and that the correlation between anion concentration and EC is adequately described, changes to anion concentrations will produce corresponding change to cation concentrations. A database consisting of 3555 analyses of major chemical composition from Estonian groundwaters was used to develop the correlations described here, and data for 320 samples with measured EC values together with major chemical constituents was used to verify the new method. As a result, a binary plot has been compiled which can be used: (1) for prediction of chemical composition of groundwater if analytical results of Cl~- or HCO3- from anions and measured values of EC are available, or (2) for description of temporal changes in groundwater chemistry if the time series of the same measurements are available.
机译:溶解的阳离子和阴离子的浓度对于地下水的水质至关重要,特别是与用作饮用水源有关。当前,对总溶解固体的评估需要对每种离子物质进行基于实验室的分析,并且无法在现场进行可靠的测试。在这里,开发了一种新方法,该方法基于电导率(EC)的现场测量和仅一个阴离子的浓度来区分离子浓度或水类型的变化。该方法在所有阳离子对EC均贡献的假设下运行,而在中性pH值下,对总溶质EC产生与Cl〜-或SO42-离子相同的作用所需的HCO3-离子几乎是其两倍。 。因此,当评估地下水的化学类型和溶质EC关系时,许多地下水系统可被视为两个阴离子系统。此外,通过假设中性电荷并充分描述了阴离子浓度和EC之间的关系,阴离子浓度的变化将产生阳离子浓度的相应变化。一个数据库由3555个爱沙尼亚地下水的主要化学组成分析组成,用于建立此处描述的相关性,并使用320个样品的EC值和主要化学成分测得的数据来验证该新方法。结果,已编制了一个二元图,可用于:(1)如果可从阴离子和EC的测量值获得Cl〜-或HCO3-的分析结果,则用于预测地下水的化学组成,或(2)用于预测地下水的化学组成。如果可以进行相同测量的时间序列,则描述地下水化学的时间变化。

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