Cambios
En el instante 23 de junio de 2026, 16:05:43 UTC,
-
Modificado el valor del campo
spatial_coverage
a[{'bbox': '{"type": "Polygon", "coordinates": [[[-2.34, 37.38], [-0.69, 37.38], [-0.69, 38.76], [-2.34, 38.76], [-2.34, 37.38]]]}', 'centroid': '{"type": "Point", "coordinates": [-1.515, 38.07]}', 'text': 'Región de Murcia', 'uri': 'http://datos.gob.es/recurso/sector-publico/territorio/Autonomia/Region-Murcia'}]
en The Role of Leaky Boreholes in the Contamination of a Regional Confined Aquifer. A case Study: The Campo de Cartagena Region, Spain
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| 94 | "notes": "Poorly constructed wells (leaky or without a gravel pack) | 94 | "notes": "Poorly constructed wells (leaky or without a gravel pack) | ||
| 95 | and abandoned wells can behave as conduits for the interconnection of | 95 | and abandoned wells can behave as conduits for the interconnection of | ||
| 96 | aquifers at dif\u0002ferent depths and facilitate the transfer of | 96 | aquifers at dif\u0002ferent depths and facilitate the transfer of | ||
| 97 | contami\u0002nants between these aquifers. This is the case with Campo | 97 | contami\u0002nants between these aquifers. This is the case with Campo | ||
| 98 | de Cartagena (SE Spain) where the primary land use is intensive | 98 | de Cartagena (SE Spain) where the primary land use is intensive | ||
| 99 | irrigated agriculture, along with a high density of wells. The | 99 | irrigated agriculture, along with a high density of wells. The | ||
| 100 | unconfined aquifer is heavily impacted by a high concentration of | 100 | unconfined aquifer is heavily impacted by a high concentration of | ||
| 101 | nitrate associated with agricultural activities. The present work | 101 | nitrate associated with agricultural activities. The present work | ||
| 102 | provides a methodological approach to evaluate the impact of the | 102 | provides a methodological approach to evaluate the impact of the | ||
| 103 | unconfined aquifer on the water quality of the confined aquifer caused | 103 | unconfined aquifer on the water quality of the confined aquifer caused | ||
| 104 | by leaky wells in high\u0002density areas of production wells. The | 104 | by leaky wells in high\u0002density areas of production wells. The | ||
| 105 | research ap\u0002proach included the use of geochemical and isotopic | 105 | research ap\u0002proach included the use of geochemical and isotopic | ||
| 106 | tools; specifically, nitrate was used as a tracer for eval\u0002uating | 106 | tools; specifically, nitrate was used as a tracer for eval\u0002uating | ||
| 107 | the impact, and the code MIX_PROGRAM was used for mixing calculations. | 107 | the impact, and the code MIX_PROGRAM was used for mixing calculations. | ||
| 108 | Results show an increase of the impact of the unconfined aquifer on | 108 | Results show an increase of the impact of the unconfined aquifer on | ||
| 109 | the confined aquifer along the groundwater flow direction toward the | 109 | the confined aquifer along the groundwater flow direction toward the | ||
| 110 | coast, although this general pattern is controlled by local factors | 110 | coast, although this general pattern is controlled by local factors | ||
| 111 | (pumping, intensity of agricultural prac\u0002tices, density of wells, | 111 | (pumping, intensity of agricultural prac\u0002tices, density of wells, | ||
| 112 | and groundwater residence time).", | 112 | and groundwater residence time).", | ||
| 113 | "notes_translated": { | 113 | "notes_translated": { | ||
| 114 | "es": "Poorly constructed wells (leaky or without a gravel pack) | 114 | "es": "Poorly constructed wells (leaky or without a gravel pack) | ||
| 115 | and abandoned wells can behave as conduits for the interconnection of | 115 | and abandoned wells can behave as conduits for the interconnection of | ||
| 116 | aquifers at dif\u0002ferent depths and facilitate the transfer of | 116 | aquifers at dif\u0002ferent depths and facilitate the transfer of | ||
| 117 | contami\u0002nants between these aquifers. This is the case with Campo | 117 | contami\u0002nants between these aquifers. This is the case with Campo | ||
| 118 | de Cartagena (SE Spain) where the primary land use is intensive | 118 | de Cartagena (SE Spain) where the primary land use is intensive | ||
| 119 | irrigated agriculture, along with a high density of wells. The | 119 | irrigated agriculture, along with a high density of wells. The | ||
| 120 | unconfined aquifer is heavily impacted by a high concentration of | 120 | unconfined aquifer is heavily impacted by a high concentration of | ||
| 121 | nitrate associated with agricultural activities. The present work | 121 | nitrate associated with agricultural activities. The present work | ||
| 122 | provides a methodological approach to evaluate the impact of the | 122 | provides a methodological approach to evaluate the impact of the | ||
| 123 | unconfined aquifer on the water quality of the confined aquifer caused | 123 | unconfined aquifer on the water quality of the confined aquifer caused | ||
| 124 | by leaky wells in high\u0002density areas of production wells. The | 124 | by leaky wells in high\u0002density areas of production wells. The | ||
| 125 | research ap\u0002proach included the use of geochemical and isotopic | 125 | research ap\u0002proach included the use of geochemical and isotopic | ||
| 126 | tools; specifically, nitrate was used as a tracer for eval\u0002uating | 126 | tools; specifically, nitrate was used as a tracer for eval\u0002uating | ||
| 127 | the impact, and the code MIX_PROGRAM was used for mixing calculations. | 127 | the impact, and the code MIX_PROGRAM was used for mixing calculations. | ||
| 128 | Results show an increase of the impact of the unconfined aquifer on | 128 | Results show an increase of the impact of the unconfined aquifer on | ||
| 129 | the confined aquifer along the groundwater flow direction toward the | 129 | the confined aquifer along the groundwater flow direction toward the | ||
| 130 | coast, although this general pattern is controlled by local factors | 130 | coast, although this general pattern is controlled by local factors | ||
| 131 | (pumping, intensity of agricultural prac\u0002tices, density of wells, | 131 | (pumping, intensity of agricultural prac\u0002tices, density of wells, | ||
| 132 | and groundwater residence time)." | 132 | and groundwater residence time)." | ||
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| 278 | tp://inspire.ec.europa.eu/metadata-codelist/TopicCategory/environment" | 249 | tp://inspire.ec.europa.eu/metadata-codelist/TopicCategory/environment" | ||
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| 291 | "name": "contaminacion", | 262 | "name": "contaminacion", | ||
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| 321 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | 292 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | ||
| 322 | ], | 293 | ], | ||
| 323 | "title": "The Role of Leaky Boreholes in the Contamination of a | 294 | "title": "The Role of Leaky Boreholes in the Contamination of a | ||
| 324 | Regional Confined Aquifer. A case Study: The Campo de Cartagena | 295 | Regional Confined Aquifer. A case Study: The Campo de Cartagena | ||
| 325 | Region, Spain", | 296 | Region, Spain", | ||
| 326 | "title_translated": { | 297 | "title_translated": { | ||
| 327 | "es": "The Role of Leaky Boreholes in the Contamination of a | 298 | "es": "The Role of Leaky Boreholes in the Contamination of a | ||
| 328 | Regional Confined Aquifer. A case Study: The Campo de Cartagena | 299 | Regional Confined Aquifer. A case Study: The Campo de Cartagena | ||
| 329 | Region, Spain" | 300 | Region, Spain" | ||
| 330 | }, | 301 | }, | ||
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| 332 | "http://inspire.ec.europa.eu/metadata-codelist/TopicCategory/biota", | 303 | "http://inspire.ec.europa.eu/metadata-codelist/TopicCategory/biota", | ||
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| 336 | "version_notes": { | 307 | "version_notes": { | ||
| 337 | "es": "" | 308 | "es": "" | ||
| 338 | } | 309 | } | ||
| 339 | } | 310 | } |