2020
DOI: 10.2166/aqua.2020.100
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Evaluation of automated groundwater level measurements for transmissivity and storativity calculation

Abstract: In this paper, we discuss the accuracy of aquifer transmissivity (T) and storativity (S) values, obtained through the processing of hourly and 5-min groundwater level data, regularly and accurately recorded by automated stations. In particular, we discuss the role of the selection of (a) the initial undisturbed hydraulic head level, which might be influenced by prior pumping cycles, and (b) the exact time of start or shutdown of the pump, which might not be exactly recorded. Furthermore, the accuracy of T and … Show more

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Cited by 6 publications
(4 citation statements)
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“…Hydraulic conductivity Hydraulic conductivity characterizes the velocity of groundwater flow into the saturated zone and depends on the aquifer materials. Pumping tests are commonly employed to evaluate this hydrogeological parameter (Kirlas, 2021). Higher hydraulic conductivity values increase the potential for groundwater pollution (Victorine Neh et al 2015).…”
Section: Depth To Watermentioning
confidence: 99%
“…Hydraulic conductivity Hydraulic conductivity characterizes the velocity of groundwater flow into the saturated zone and depends on the aquifer materials. Pumping tests are commonly employed to evaluate this hydrogeological parameter (Kirlas, 2021). Higher hydraulic conductivity values increase the potential for groundwater pollution (Victorine Neh et al 2015).…”
Section: Depth To Watermentioning
confidence: 99%
“…Water demand for irrigation and domestic purposesis high, especially during the period spanning from May to September. Moreover, the combination of surface water scarcity and generally inadequate yearly rainfall renders groundwater the only viable source of water [57]. However, this fact has caused a noteworthy decrease in the groundwater level throughout the area.…”
Section: Study Areamentioning
confidence: 99%
“…Higher hydraulic conductivity values portend higher groundwater pollution potential [79]. In previous research, the Cooper-Jacob and the recovery test methods were employed to groundwater level data in order to estimate the hydrogeological parameters of the studied aquifer, namely hydraulic conductivity, transmissivity and storativity [55,57,80,81]. Results showed that the hydraulic conductivity ranged from about 1 × 10 −6 m/s to 2 × 10 −5 m/s, and its values were considered slightly low [55,57,80,81].…”
Section: Hydraulic Conductivitymentioning
confidence: 99%
“…This would suggest either that the porosity derived from this model in this upper part of the bedrock is reflective of the aquifer's effective storage capacity rather than the total porosity (including bound and unconnected groundwater), or that storativity and total porosity are not significantly different in these horizons. However, it is also likely that storativity values obtained from hydraulic testing are providing an overestimation of the actual aquifer storativity due to being representative of a small area abound the boreholes (because of the low pumping rates applicable for hydraulic testing such low productivity hydrogeological environment) affected by locally increased porosity associated to the downhole hammer drilling technique (Kirlas and Katsifarakis, 2020;Pongmanda and Suprapti, 2020). Such artificially increased porosity and storativity would have relatively more effect on deeper (more massive) than shallower bedrock horizons.…”
Section: Importance Of Accounting For Clay Minerals and Related Uncertaintiesmentioning
confidence: 99%