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) en Trace Element Concentrations in Saltmarsh Soils Strongly Affected by Wastes from Metal Sulphide Mining Areas
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| 95 | "notes": "Soil and water samples were analysed for trace metals and | 105 | "notes": "Soil and water samples were analysed for trace metals and | ||
| 96 | As in two watercourses and 14 sampling plots in a salt marsh polluted | 106 | As in two watercourses and 14 sampling plots in a salt marsh polluted | ||
| 97 | by mine wastes in SE Spain. Groundwater levels, soil pH and Eh were | 107 | by mine wastes in SE Spain. Groundwater levels, soil pH and Eh were | ||
| 98 | measured \u2018in situ\u2019 for a 12-month period in each sampling | 108 | measured \u2018in situ\u2019 for a 12-month period in each sampling | ||
| 99 | plot, and total calcium carbonate was also determined. Low | 109 | plot, and total calcium carbonate was also determined. Low | ||
| 100 | concentrations of soluble metals (maximum Mn 1.089 mg L\u22121 and | 110 | concentrations of soluble metals (maximum Mn 1.089 mg L\u22121 and | ||
| 101 | maximum Zn 0.553 mg L\u22121) were found in the watercourses. However, | 111 | maximum Zn 0.553 mg L\u22121) were found in the watercourses. However, | ||
| 102 | total metal contents were extremely high in the soils of a zone of the | 112 | total metal contents were extremely high in the soils of a zone of the | ||
| 103 | salt marsh (maximum 1,933 mg kg\u22121 of Mn, 62,280 mg kg\u22121 of | 113 | salt marsh (maximum 1,933 mg kg\u22121 of Mn, 62,280 mg kg\u22121 of | ||
| 104 | Zn, 16,845 mg kg\u22121 of Pb, 77 mg kg\u22121 of Cd, 418 mg kg\u22121 | 114 | Zn, 16,845 mg kg\u22121 of Pb, 77 mg kg\u22121 of Cd, 418 mg kg\u22121 | ||
| 105 | of Cu and 725 mg kg\u22121 of As), and soluble metals in the pore | 115 | of Cu and 725 mg kg\u22121 of As), and soluble metals in the pore | ||
| 106 | water reached 38.7 mg L\u22121 for Zn, 3.15 mg L\u22121 for Pb, 48.0 | 116 | water reached 38.7 mg L\u22121 for Zn, 3.15 mg L\u22121 for Pb, 48.0 | ||
| 107 | mg L\u22121 for Mn, 0.61 mg L\u22121 for Cd and 0.29 mg L\u22121 for | 117 | mg L\u22121 for Mn, 0.61 mg L\u22121 for Cd and 0.29 mg L\u22121 for | ||
| 108 | As. Variable concen trations with depth indicate a possible | 118 | As. Variable concen trations with depth indicate a possible | ||
| 109 | re-mobilisation of the metals, which could be related to spatial and | 119 | re-mobilisation of the metals, which could be related to spatial and | ||
| 110 | temporal variations of water table level, pH and Eh and to the | 120 | temporal variations of water table level, pH and Eh and to the | ||
| 111 | presence of calcium carbonate. A tendency for the Eh to decrease in | 121 | presence of calcium carbonate. A tendency for the Eh to decrease in | ||
| 112 | the warmest months and to increase in the coldest ones was found, | 122 | the warmest months and to increase in the coldest ones was found, | ||
| 113 | especially, in plots that received water with a high content of | 123 | especially, in plots that received water with a high content of | ||
| 114 | dissolved organic carbon. Hence, the existence of nutrient | 124 | dissolved organic carbon. Hence, the existence of nutrient | ||
| 115 | effluent-enriched water may modify the physical\u2013chemical | 125 | effluent-enriched water may modify the physical\u2013chemical | ||
| 116 | conditions of the soil\u2013water sys tem and influence metal | 126 | conditions of the soil\u2013water sys tem and influence metal | ||
| 117 | mobility.", | 127 | mobility.", | ||
| 118 | "notes_translated": { | 128 | "notes_translated": { | ||
| 119 | "es": "Soil and water samples were analysed for trace metals and | 129 | "es": "Soil and water samples were analysed for trace metals and | ||
| 120 | As in two watercourses and 14 sampling plots in a salt marsh polluted | 130 | As in two watercourses and 14 sampling plots in a salt marsh polluted | ||
| 121 | by mine wastes in SE Spain. Groundwater levels, soil pH and Eh were | 131 | by mine wastes in SE Spain. Groundwater levels, soil pH and Eh were | ||
| 122 | measured \u2018in situ\u2019 for a 12-month period in each sampling | 132 | measured \u2018in situ\u2019 for a 12-month period in each sampling | ||
| 123 | plot, and total calcium carbonate was also determined. Low | 133 | plot, and total calcium carbonate was also determined. Low | ||
| 124 | concentrations of soluble metals (maximum Mn 1.089 mg L\u22121 and | 134 | concentrations of soluble metals (maximum Mn 1.089 mg L\u22121 and | ||
| 125 | maximum Zn 0.553 mg L\u22121) were found in the watercourses. However, | 135 | maximum Zn 0.553 mg L\u22121) were found in the watercourses. However, | ||
| 126 | total metal contents were extremely high in the soils of a zone of the | 136 | total metal contents were extremely high in the soils of a zone of the | ||
| 127 | salt marsh (maximum 1,933 mg kg\u22121 of Mn, 62,280 mg kg\u22121 of | 137 | salt marsh (maximum 1,933 mg kg\u22121 of Mn, 62,280 mg kg\u22121 of | ||
| 128 | Zn, 16,845 mg kg\u22121 of Pb, 77 mg kg\u22121 of Cd, 418 mg kg\u22121 | 138 | Zn, 16,845 mg kg\u22121 of Pb, 77 mg kg\u22121 of Cd, 418 mg kg\u22121 | ||
| 129 | of Cu and 725 mg kg\u22121 of As), and soluble metals in the pore | 139 | of Cu and 725 mg kg\u22121 of As), and soluble metals in the pore | ||
| 130 | water reached 38.7 mg L\u22121 for Zn, 3.15 mg L\u22121 for Pb, 48.0 | 140 | water reached 38.7 mg L\u22121 for Zn, 3.15 mg L\u22121 for Pb, 48.0 | ||
| 131 | mg L\u22121 for Mn, 0.61 mg L\u22121 for Cd and 0.29 mg L\u22121 for | 141 | mg L\u22121 for Mn, 0.61 mg L\u22121 for Cd and 0.29 mg L\u22121 for | ||
| 132 | As. Variable concen trations with depth indicate a possible | 142 | As. Variable concen trations with depth indicate a possible | ||
| 133 | re-mobilisation of the metals, which could be related to spatial and | 143 | re-mobilisation of the metals, which could be related to spatial and | ||
| 134 | temporal variations of water table level, pH and Eh and to the | 144 | temporal variations of water table level, pH and Eh and to the | ||
| 135 | presence of calcium carbonate. A tendency for the Eh to decrease in | 145 | presence of calcium carbonate. A tendency for the Eh to decrease in | ||
| 136 | the warmest months and to increase in the coldest ones was found, | 146 | the warmest months and to increase in the coldest ones was found, | ||
| 137 | especially, in plots that received water with a high content of | 147 | especially, in plots that received water with a high content of | ||
| 138 | dissolved organic carbon. Hence, the existence of nutrient | 148 | dissolved organic carbon. Hence, the existence of nutrient | ||
| 139 | effluent-enriched water may modify the physical\u2013chemical | 149 | effluent-enriched water may modify the physical\u2013chemical | ||
| 140 | conditions of the soil\u2013water sys tem and influence metal | 150 | conditions of the soil\u2013water sys tem and influence metal | ||
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| 309 | ], | 319 | ], | ||
| 310 | "title": "Trace Element Concentrations in Saltmarsh Soils Strongly | 320 | "title": "Trace Element Concentrations in Saltmarsh Soils Strongly | ||
| 311 | Affected by Wastes from Metal Sulphide Mining Areas", | 321 | Affected by Wastes from Metal Sulphide Mining Areas", | ||
| 312 | "title_translated": { | 322 | "title_translated": { | ||
| 313 | "es": "Trace Element Concentrations in Saltmarsh Soils Strongly | 323 | "es": "Trace Element Concentrations in Saltmarsh Soils Strongly | ||
| 314 | Affected by Wastes from Metal Sulphide Mining Areas" | 324 | Affected by Wastes from Metal Sulphide Mining Areas" | ||
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