Hydrochemical properties of groundwater samples in Semarang area, Java Island, Indonesia (1992, 1993, 2003, 2006, and 2007)

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Autores principales: Putranto, Thomas Triadi, Rüde, Thomas, Irawan, Dasapta Erwin
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2016
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_version_ 1867171841176502272
author Putranto, Thomas Triadi
Rüde, Thomas
Irawan, Dasapta Erwin
author_facet Putranto, Thomas Triadi
Rüde, Thomas
Irawan, Dasapta Erwin
collection Datos científicos de ciencias marinas y ambientales
contents In Semarang City, groundwater has been exploited as a natural resource since 1841. The groundwater exploited in deep wells is concentrated in confined aquifers. The previous hydrogeological model was developed in one unit of aquifer and refined then by using several hydrostratigraphical units following a regional hydrogeological map without any further analysis. At present, there is a lack of precise hydrogeological model which integrates geological and hydrogeological data, in particular for multiple aquifers in Semarang. Thus, the aim of this paper is to develop a hydrogeological model for the multiple aquifers in Semarang using an integrated data approach. Groundwater samples in the confined aquifers have been analyzed to define the water type and its lateral distribution. Two hydrogeological cross sections were then created based on several borelog data to define a hydrostratigraphical unit (HSU). The HSU result indicates the hydrogeological model of Semarang consists of two aquifers, three aquitards, and one aquiclude. Aquifer 1 is unconfined, while Aquifer 2 is confined. Aquifer 2 is classified into three groups (2a, 2b, and 2c) based on analyses of major ion content and hydrostratigraphical cross sections.
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id pangaea_https___doi_org_10_1594_PANGAEA_862987
institution PANGAEA
language en
publishDate 2016
publisher PANGAEA
record_format pangaea
spellingShingle Hydrochemical properties of groundwater samples in Semarang area, Java Island, Indonesia (1992, 1993, 2003, 2006, and 2007)
Putranto, Thomas Triadi
Rüde, Thomas
Irawan, Dasapta Erwin
Aquifer type; Area/locality; Balance; Bicarbonate ion; Calcium; Calculated; Chloride; Conductivity, electrical; DATE/TIME; Depth, well; ELEVATION; Event label; Facies name/code; Handheld GPS, Garmin; Java Island, northern coast; Latitude of event; Longitude of event; Magnesium; N_1; N_2; N_3; N_7; pH; Portable water detector; Portable water quality meter (Hanna Instruments); Potassium; Sample position; Sampling well; SB_100; SB_112; SB_120; SB_176; SB_185; SB_189; SB_190; SB_198; SB_206; SB_210; SB_211; SB_213; SB_214; SB_215; SB_217; SB_219; SB_220; SB_225; SB_226; SB_235; SB_256; SB_262; SB_265; SB_270; SB_271; SB_273; SB_278; SB_281; SB_282; SB_283; SB_297; SB_299; SB_321; SB_325; SB_33; SB_332; SB_344; SB_347; SB_348; SB_36; SB_590; SB_60; SB_726; SB_758; SB_790; SB_793; SB_92; SB_951; Sodium; SP_136; SP_138; SP_139; SP_341; SP_342; SP_764; Spectrophotometric; Sulfate; Total dissolved solids; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator; Water level; WELL
In Semarang City, groundwater has been exploited as a natural resource since 1841. The groundwater exploited in deep wells is concentrated in confined aquifers. The previous hydrogeological model was developed in one unit of aquifer and refined then by using several hydrostratigraphical units following a regional hydrogeological map without any further analysis. At present, there is a lack of precise hydrogeological model which integrates geological and hydrogeological data, in particular for multiple aquifers in Semarang. Thus, the aim of this paper is to develop a hydrogeological model for the multiple aquifers in Semarang using an integrated data approach. Groundwater samples in the confined aquifers have been analyzed to define the water type and its lateral distribution. Two hydrogeological cross sections were then created based on several borelog data to define a hydrostratigraphical unit (HSU). The HSU result indicates the hydrogeological model of Semarang consists of two aquifers, three aquitards, and one aquiclude. Aquifer 1 is unconfined, while Aquifer 2 is confined. Aquifer 2 is classified into three groups (2a, 2b, and 2c) based on analyses of major ion content and hydrostratigraphical cross sections.
title Hydrochemical properties of groundwater samples in Semarang area, Java Island, Indonesia (1992, 1993, 2003, 2006, and 2007)
topic Aquifer type; Area/locality; Balance; Bicarbonate ion; Calcium; Calculated; Chloride; Conductivity, electrical; DATE/TIME; Depth, well; ELEVATION; Event label; Facies name/code; Handheld GPS, Garmin; Java Island, northern coast; Latitude of event; Longitude of event; Magnesium; N_1; N_2; N_3; N_7; pH; Portable water detector; Portable water quality meter (Hanna Instruments); Potassium; Sample position; Sampling well; SB_100; SB_112; SB_120; SB_176; SB_185; SB_189; SB_190; SB_198; SB_206; SB_210; SB_211; SB_213; SB_214; SB_215; SB_217; SB_219; SB_220; SB_225; SB_226; SB_235; SB_256; SB_262; SB_265; SB_270; SB_271; SB_273; SB_278; SB_281; SB_282; SB_283; SB_297; SB_299; SB_321; SB_325; SB_33; SB_332; SB_344; SB_347; SB_348; SB_36; SB_590; SB_60; SB_726; SB_758; SB_790; SB_793; SB_92; SB_951; Sodium; SP_136; SP_138; SP_139; SP_341; SP_342; SP_764; Spectrophotometric; Sulfate; Total dissolved solids; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator; Water level; WELL
url https://doi.org/10.1594/PANGAEA.862987