Influence of contaminated Vistula River water on the groundwater entering the Zakrzówek limestone quarry, Cracow region, Poland
Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry wate...
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2000 |
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| Umfang: |
7 |
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| Reproduktion: |
Springer Online Journal Archives 1860-2002 |
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| Übergeordnetes Werk: |
in: Environmental geology - 1975, 39(2000) vom: März/Apr., Seite 398-404 |
| Übergeordnetes Werk: |
volume:39 ; year:2000 ; month:03/04 ; pages:398-404 ; extent:7 |
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| 520 | |a Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. | ||
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(DE-627)NLEJ200815776 DE-627 ger DE-627 rakwb eng Influence of contaminated Vistula River water on the groundwater entering the Zakrzówek limestone quarry, Cracow region, Poland 2000 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. Springer Online Journal Archives 1860-2002 Motyka, J. oth Postawa, A. oth in Environmental geology 1975 39(2000) vom: März/Apr., Seite 398-404 (DE-627)NLEJ188995161 (DE-600)1459034-7 1432-0495 nnns volume:39 year:2000 month:03/04 pages:398-404 extent:7 http://dx.doi.org/10.1007/s002540050020 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 39 2000 3/4 398-404 7 |
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(DE-627)NLEJ200815776 DE-627 ger DE-627 rakwb eng Influence of contaminated Vistula River water on the groundwater entering the Zakrzówek limestone quarry, Cracow region, Poland 2000 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. Springer Online Journal Archives 1860-2002 Motyka, J. oth Postawa, A. oth in Environmental geology 1975 39(2000) vom: März/Apr., Seite 398-404 (DE-627)NLEJ188995161 (DE-600)1459034-7 1432-0495 nnns volume:39 year:2000 month:03/04 pages:398-404 extent:7 http://dx.doi.org/10.1007/s002540050020 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 39 2000 3/4 398-404 7 |
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(DE-627)NLEJ200815776 DE-627 ger DE-627 rakwb eng Influence of contaminated Vistula River water on the groundwater entering the Zakrzówek limestone quarry, Cracow region, Poland 2000 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. Springer Online Journal Archives 1860-2002 Motyka, J. oth Postawa, A. oth in Environmental geology 1975 39(2000) vom: März/Apr., Seite 398-404 (DE-627)NLEJ188995161 (DE-600)1459034-7 1432-0495 nnns volume:39 year:2000 month:03/04 pages:398-404 extent:7 http://dx.doi.org/10.1007/s002540050020 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 39 2000 3/4 398-404 7 |
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(DE-627)NLEJ200815776 DE-627 ger DE-627 rakwb eng Influence of contaminated Vistula River water on the groundwater entering the Zakrzówek limestone quarry, Cracow region, Poland 2000 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. Springer Online Journal Archives 1860-2002 Motyka, J. oth Postawa, A. oth in Environmental geology 1975 39(2000) vom: März/Apr., Seite 398-404 (DE-627)NLEJ188995161 (DE-600)1459034-7 1432-0495 nnns volume:39 year:2000 month:03/04 pages:398-404 extent:7 http://dx.doi.org/10.1007/s002540050020 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 39 2000 3/4 398-404 7 |
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(DE-627)NLEJ200815776 DE-627 ger DE-627 rakwb eng Influence of contaminated Vistula River water on the groundwater entering the Zakrzówek limestone quarry, Cracow region, Poland 2000 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. Springer Online Journal Archives 1860-2002 Motyka, J. oth Postawa, A. oth in Environmental geology 1975 39(2000) vom: März/Apr., Seite 398-404 (DE-627)NLEJ188995161 (DE-600)1459034-7 1432-0495 nnns volume:39 year:2000 month:03/04 pages:398-404 extent:7 http://dx.doi.org/10.1007/s002540050020 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 39 2000 3/4 398-404 7 |
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Influence of contaminated Vistula River water on the groundwater entering the Zakrzówek limestone quarry, Cracow region, Poland |
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Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. |
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Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. |
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Abstract Chemical composition of water inflows in the Zakrzówek quarry, developed in fractured and karstified Upper Jurassic limestones, is controlled by infiltration of polluted water from the Vistula River and by infiltrating meteoric water. The river water TDS value is 2.5 g/dm3. The quarry waters have 0.6–2.0 g/dm3 TDS. Highly mineralised waters belong to Cl-Na type. With decreasing TDS the percentage of sulphates, calcium, magnesium and hydrocarbonates increases. This seems to result from various processes including dilution of polluted river water, leaching of aquifer rocks, and ion exchange. The transfer time of river water to the quarry is about 100–120 days. Concentration of contaminants contained in the river water declines during the migration through limestones to the quarry. |
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