Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina
Chemical analyses of major ions were performed in some of the pampasic ponds in the lower stream bed of Salado River drainage basin. Results indicated that total dissolved solids had a mean value of 1341 mg/l, where sodium was the most abundant of the cations (80.2%) and chloride (44.2%) and bicarbo...
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2000
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09430105_v39_n8_p951_Miretzky http://hdl.handle.net/20.500.12110/paper_09430105_v39_n8_p951_Miretzky |
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paper:paper_09430105_v39_n8_p951_Miretzky2023-06-08T15:53:37Z Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina Hydro chemical evolution Major ions composition Pampasic ponds Salinity Calcium compounds Chemical analysis Chlorine compounds Groundwater Ions Sediments Sodium Hydrochemistry Pampasic ponds Salinity Rivers cation exchange capacity hydrochemistry loess river water water quality Argentina Chemical analyses of major ions were performed in some of the pampasic ponds in the lower stream bed of Salado River drainage basin. Results indicated that total dissolved solids had a mean value of 1341 mg/l, where sodium was the most abundant of the cations (80.2%) and chloride (44.2%) and bicarbonate (37.4%) were the predominant anions. Saturation index showed oversaturation with respect to calcite and dolomite. Since groundwater is the main source of surface water, high sodium concentration in the ponds may be explained by a cation exchange process in the loessic sediments of the basin where calcium is replaced by sodium. Chemical analyses of major ions were performed in some of the pampasic ponds in the lower stream bed of Salado River drainage basin. Results indicated that total dissolved solids had a mean value of 1341 mg/l, where sodium was the most abundant of the cations (80.2%) and chloride (44.2%) and bicarbonate (37.4%) were the predominant anions. Saturation index showed oversaturation with respect to calcite and dolomite. Since groundwater is the main source of surface water, high sodium concentration in the ponds may be explained by a cation exchange process in the loessic sediments of the basin where calcium is replaced by sodium. 2000 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09430105_v39_n8_p951_Miretzky http://hdl.handle.net/20.500.12110/paper_09430105_v39_n8_p951_Miretzky |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
Hydro chemical evolution Major ions composition Pampasic ponds Salinity Calcium compounds Chemical analysis Chlorine compounds Groundwater Ions Sediments Sodium Hydrochemistry Pampasic ponds Salinity Rivers cation exchange capacity hydrochemistry loess river water water quality Argentina |
| spellingShingle |
Hydro chemical evolution Major ions composition Pampasic ponds Salinity Calcium compounds Chemical analysis Chlorine compounds Groundwater Ions Sediments Sodium Hydrochemistry Pampasic ponds Salinity Rivers cation exchange capacity hydrochemistry loess river water water quality Argentina Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina |
| topic_facet |
Hydro chemical evolution Major ions composition Pampasic ponds Salinity Calcium compounds Chemical analysis Chlorine compounds Groundwater Ions Sediments Sodium Hydrochemistry Pampasic ponds Salinity Rivers cation exchange capacity hydrochemistry loess river water water quality Argentina |
| description |
Chemical analyses of major ions were performed in some of the pampasic ponds in the lower stream bed of Salado River drainage basin. Results indicated that total dissolved solids had a mean value of 1341 mg/l, where sodium was the most abundant of the cations (80.2%) and chloride (44.2%) and bicarbonate (37.4%) were the predominant anions. Saturation index showed oversaturation with respect to calcite and dolomite. Since groundwater is the main source of surface water, high sodium concentration in the ponds may be explained by a cation exchange process in the loessic sediments of the basin where calcium is replaced by sodium. Chemical analyses of major ions were performed in some of the pampasic ponds in the lower stream bed of Salado River drainage basin. Results indicated that total dissolved solids had a mean value of 1341 mg/l, where sodium was the most abundant of the cations (80.2%) and chloride (44.2%) and bicarbonate (37.4%) were the predominant anions. Saturation index showed oversaturation with respect to calcite and dolomite. Since groundwater is the main source of surface water, high sodium concentration in the ponds may be explained by a cation exchange process in the loessic sediments of the basin where calcium is replaced by sodium. |
| title |
Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina |
| title_short |
Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina |
| title_full |
Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina |
| title_fullStr |
Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina |
| title_full_unstemmed |
Hydrochemistry of pampasic ponds in the lower stream bed of Salado River drainage basin, Argentina |
| title_sort |
hydrochemistry of pampasic ponds in the lower stream bed of salado river drainage basin, argentina |
| publishDate |
2000 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09430105_v39_n8_p951_Miretzky http://hdl.handle.net/20.500.12110/paper_09430105_v39_n8_p951_Miretzky |
| _version_ |
1768543904706068480 |