Cambios
En el instante 23 de junio de 2026, 15:59:26 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 Impacts of human activities on recharge in a multilayered semiarid aquifer (Campo de Cartagena, SE Spain)
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| 94 | "notes": "The development of intense agriculture in semiarid areas | 94 | "notes": "The development of intense agriculture in semiarid areas | ||
| 95 | modifies intensity and spatial distribution of groundwater recharge by | 95 | modifies intensity and spatial distribution of groundwater recharge by | ||
| 96 | summing irrigation return flow to limited rainfall infiltration. | 96 | summing irrigation return flow to limited rainfall infiltration. | ||
| 97 | Environmental tracers provide key information, but their | 97 | Environmental tracers provide key information, but their | ||
| 98 | interpretation is complicated by more complex groundwater flow | 98 | interpretation is complicated by more complex groundwater flow | ||
| 99 | patterns. In multilayered aquifers, the real origin of the groundwater | 99 | patterns. In multilayered aquifers, the real origin of the groundwater | ||
| 100 | samples is hard to assess because of local mixing processes occurring | 100 | samples is hard to assess because of local mixing processes occurring | ||
| 101 | inside long-screened boreholes. We use environmental tracers (14C, | 101 | inside long-screened boreholes. We use environmental tracers (14C, | ||
| 102 | 13C, 2 H, 18O, 3 H) to investigate the long-term evolution of recharge | 102 | 13C, 2 H, 18O, 3 H) to investigate the long-term evolution of recharge | ||
| 103 | in the five-layer Campo de Cartagena aquifer in South-Eastern Spain, | 103 | in the five-layer Campo de Cartagena aquifer in South-Eastern Spain, | ||
| 104 | in addition to high-resolution temperature loggings to identify the | 104 | in addition to high-resolution temperature loggings to identify the | ||
| 105 | depth of origin of groundwater. Despite the complex background, this | 105 | depth of origin of groundwater. Despite the complex background, this | ||
| 106 | methodology allowed a reliable interpretation of the geochemistry and | 106 | methodology allowed a reliable interpretation of the geochemistry and | ||
| 107 | provided a better understanding of the groundwater flow patterns. The | 107 | provided a better understanding of the groundwater flow patterns. The | ||
| 108 | tritium method did not give good quantitative results because of the | 108 | tritium method did not give good quantitative results because of the | ||
| 109 | high variability of the recharge signal but remained an excellent | 109 | high variability of the recharge signal but remained an excellent | ||
| 110 | indicator of recent recharge. Nonetheless, both pre-anthropization and | 110 | indicator of recent recharge. Nonetheless, both pre-anthropization and | ||
| 111 | post-anthropization recharge regime could be identified and quantified | 111 | post-anthropization recharge regime could be identified and quantified | ||
| 112 | by radiocarbon. Before the development of agriculture, recharge varied | 112 | by radiocarbon. Before the development of agriculture, recharge varied | ||
| 113 | from 17 mm.year-1 at the mountain ranges to 6 mm.year-1 in the plain, | 113 | from 17 mm.year-1 at the mountain ranges to 6 mm.year-1 in the plain, | ||
| 114 | whereas the mean annual rainfall is about 300 mm. In response to the | 114 | whereas the mean annual rainfall is about 300 mm. In response to the | ||
| 115 | increase of agricultural activity, recharge fluxes to the plain were | 115 | increase of agricultural activity, recharge fluxes to the plain were | ||
| 116 | amplified and nowadays reach up to 210 mm.year-1 in irrigated areas. | 116 | amplified and nowadays reach up to 210 mm.year-1 in irrigated areas. | ||
| 117 | These valu", | 117 | These valu", | ||
| 118 | "notes_translated": { | 118 | "notes_translated": { | ||
| 119 | "es": "The development of intense agriculture in semiarid areas | 119 | "es": "The development of intense agriculture in semiarid areas | ||
| 120 | modifies intensity and spatial distribution of groundwater recharge by | 120 | modifies intensity and spatial distribution of groundwater recharge by | ||
| 121 | summing irrigation return flow to limited rainfall infiltration. | 121 | summing irrigation return flow to limited rainfall infiltration. | ||
| 122 | Environmental tracers provide key information, but their | 122 | Environmental tracers provide key information, but their | ||
| 123 | interpretation is complicated by more complex groundwater flow | 123 | interpretation is complicated by more complex groundwater flow | ||
| 124 | patterns. In multilayered aquifers, the real origin of the groundwater | 124 | patterns. In multilayered aquifers, the real origin of the groundwater | ||
| 125 | samples is hard to assess because of local mixing processes occurring | 125 | samples is hard to assess because of local mixing processes occurring | ||
| 126 | inside long-screened boreholes. We use environmental tracers (14C, | 126 | inside long-screened boreholes. We use environmental tracers (14C, | ||
| 127 | 13C, 2 H, 18O, 3 H) to investigate the long-term evolution of recharge | 127 | 13C, 2 H, 18O, 3 H) to investigate the long-term evolution of recharge | ||
| 128 | in the five-layer Campo de Cartagena aquifer in South-Eastern Spain, | 128 | in the five-layer Campo de Cartagena aquifer in South-Eastern Spain, | ||
| 129 | in addition to high-resolution temperature loggings to identify the | 129 | in addition to high-resolution temperature loggings to identify the | ||
| 130 | depth of origin of groundwater. Despite the complex background, this | 130 | depth of origin of groundwater. Despite the complex background, this | ||
| 131 | methodology allowed a reliable interpretation of the geochemistry and | 131 | methodology allowed a reliable interpretation of the geochemistry and | ||
| 132 | provided a better understanding of the groundwater flow patterns. The | 132 | provided a better understanding of the groundwater flow patterns. The | ||
| 133 | tritium method did not give good quantitative results because of the | 133 | tritium method did not give good quantitative results because of the | ||
| 134 | high variability of the recharge signal but remained an excellent | 134 | high variability of the recharge signal but remained an excellent | ||
| 135 | indicator of recent recharge. Nonetheless, both pre-anthropization and | 135 | indicator of recent recharge. Nonetheless, both pre-anthropization and | ||
| 136 | post-anthropization recharge regime could be identified and quantified | 136 | post-anthropization recharge regime could be identified and quantified | ||
| 137 | by radiocarbon. Before the development of agriculture, recharge varied | 137 | by radiocarbon. Before the development of agriculture, recharge varied | ||
| 138 | from 17 mm.year-1 at the mountain ranges to 6 mm.year-1 in the plain, | 138 | from 17 mm.year-1 at the mountain ranges to 6 mm.year-1 in the plain, | ||
| 139 | whereas the mean annual rainfall is about 300 mm. In response to the | 139 | whereas the mean annual rainfall is about 300 mm. In response to the | ||
| 140 | increase of agricultural activity, recharge fluxes to the plain were | 140 | increase of agricultural activity, recharge fluxes to the plain were | ||
| 141 | amplified and nowadays reach up to 210 mm.year-1 in irrigated areas. | 141 | amplified and nowadays reach up to 210 mm.year-1 in irrigated areas. | ||
| 142 | These valu" | 142 | These valu" | ||
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| 275 | "text": "Regi\u00f3n de Murcia", | 246 | "text": "Regi\u00f3n de Murcia", | ||
| 276 | "uri": | 247 | "uri": | ||
| 277 | atos.gob.es/recurso/sector-publico/territorio/Autonomia/Region-Murcia" | 248 | atos.gob.es/recurso/sector-publico/territorio/Autonomia/Region-Murcia" | ||
| 278 | } | 249 | } | ||
| 279 | ], | 250 | ], | ||
| 280 | "spatial_uri": | 251 | "spatial_uri": | ||
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| 282 | "state": "active", | 253 | "state": "active", | ||
| 283 | "study_variables": { | 254 | "study_variables": { | ||
| 284 | "es": "" | 255 | "es": "" | ||
| 285 | }, | 256 | }, | ||
| 286 | "tag_uri": [ | 257 | "tag_uri": [ | ||
| 287 | 258 | ||||
| 288 | tp://inspire.ec.europa.eu/metadata-codelist/TopicCategory/environment" | 259 | tp://inspire.ec.europa.eu/metadata-codelist/TopicCategory/environment" | ||
| 289 | ], | 260 | ], | ||
| 290 | "tags": [ | 261 | "tags": [ | ||
| 291 | { | 262 | { | ||
| 292 | "display_name": "demarcacion_hidrografica", | 263 | "display_name": "demarcacion_hidrografica", | ||
| 293 | "id": "fb12d8a7-62fc-4f85-89f3-623b51a8a650", | 264 | "id": "fb12d8a7-62fc-4f85-89f3-623b51a8a650", | ||
| 294 | "name": "demarcacion_hidrografica", | 265 | "name": "demarcacion_hidrografica", | ||
| 295 | "state": "active", | 266 | "state": "active", | ||
| 296 | "vocabulary_id": null | 267 | "vocabulary_id": null | ||
| 297 | }, | 268 | }, | ||
| 298 | { | 269 | { | ||
| 299 | "display_name": "eutrofizacion", | 270 | "display_name": "eutrofizacion", | ||
| 300 | "id": "5fcdd244-0f78-4801-be7d-5a67c5bb55ec", | 271 | "id": "5fcdd244-0f78-4801-be7d-5a67c5bb55ec", | ||
| 301 | "name": "eutrofizacion", | 272 | "name": "eutrofizacion", | ||
| 302 | "state": "active", | 273 | "state": "active", | ||
| 303 | "vocabulary_id": null | 274 | "vocabulary_id": null | ||
| 304 | }, | 275 | }, | ||
| 305 | { | 276 | { | ||
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| 307 | "id": "ab71cc3e-3c99-4f3f-a20f-d4e8016c3b55", | 278 | "id": "ab71cc3e-3c99-4f3f-a20f-d4e8016c3b55", | ||
| 308 | "name": "gestion_sostenible", | 279 | "name": "gestion_sostenible", | ||
| 309 | "state": "active", | 280 | "state": "active", | ||
| 310 | "vocabulary_id": null | 281 | "vocabulary_id": null | ||
| 311 | }, | 282 | }, | ||
| 312 | { | 283 | { | ||
| 313 | "display_name": "impacto_humano", | 284 | "display_name": "impacto_humano", | ||
| 314 | "id": "f7473e8b-c9b0-4a89-a17c-1282accc49ac", | 285 | "id": "f7473e8b-c9b0-4a89-a17c-1282accc49ac", | ||
| 315 | "name": "impacto_humano", | 286 | "name": "impacto_humano", | ||
| 316 | "state": "active", | 287 | "state": "active", | ||
| 317 | "vocabulary_id": null | 288 | "vocabulary_id": null | ||
| 318 | }, | 289 | }, | ||
| 319 | { | 290 | { | ||
| 320 | "display_name": "marino-y-terrestre", | 291 | "display_name": "marino-y-terrestre", | ||
| 321 | "id": "ba2bc7ce-eaac-49a7-8f1b-c0a179486f10", | 292 | "id": "ba2bc7ce-eaac-49a7-8f1b-c0a179486f10", | ||
| 322 | "name": "marino-y-terrestre", | 293 | "name": "marino-y-terrestre", | ||
| 323 | "state": "active", | 294 | "state": "active", | ||
| 324 | "vocabulary_id": null | 295 | "vocabulary_id": null | ||
| 325 | }, | 296 | }, | ||
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| 327 | "display_name": "sistemas-karsticos-y-otros-sistemas-hidr", | 298 | "display_name": "sistemas-karsticos-y-otros-sistemas-hidr", | ||
| 328 | "id": "c737a1f9-75ea-45e1-aaa4-0f5120e7b9bc", | 299 | "id": "c737a1f9-75ea-45e1-aaa4-0f5120e7b9bc", | ||
| 329 | "name": "sistemas-karsticos-y-otros-sistemas-hidr", | 300 | "name": "sistemas-karsticos-y-otros-sistemas-hidr", | ||
| 330 | "state": "active", | 301 | "state": "active", | ||
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| 332 | } | 303 | } | ||
| 333 | ], | 304 | ], | ||
| 334 | "thematic_area": [ | 305 | "thematic_area": [ | ||
| 335 | "espacios_protegidos" | 306 | "espacios_protegidos" | ||
| 336 | ], | 307 | ], | ||
| 337 | "theme_es": [ | 308 | "theme_es": [ | ||
| 338 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | 309 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | ||
| 339 | ], | 310 | ], | ||
| 340 | "title": "Impacts of human activities on recharge in a multilayered | 311 | "title": "Impacts of human activities on recharge in a multilayered | ||
| 341 | semiarid aquifer (Campo de Cartagena, SE Spain)", | 312 | semiarid aquifer (Campo de Cartagena, SE Spain)", | ||
| 342 | "title_translated": { | 313 | "title_translated": { | ||
| 343 | "es": "Impacts of human activities on recharge in a multilayered | 314 | "es": "Impacts of human activities on recharge in a multilayered | ||
| 344 | semiarid aquifer (Campo de Cartagena, SE Spain)" | 315 | semiarid aquifer (Campo de Cartagena, SE Spain)" | ||
| 345 | }, | 316 | }, | ||
| 346 | "topic": | 317 | "topic": | ||
| 347 | "http://inspire.ec.europa.eu/metadata-codelist/TopicCategory/biota", | 318 | "http://inspire.ec.europa.eu/metadata-codelist/TopicCategory/biota", | ||
| 348 | "type": "dataset", | 319 | "type": "dataset", | ||
| 349 | "url": | 320 | "url": | ||
| 350 | //iepnb.es:443/catalogo/dataset/cbbd2a8d-0961-56a2-8774-b46a8af0ddff", | 321 | //iepnb.es:443/catalogo/dataset/cbbd2a8d-0961-56a2-8774-b46a8af0ddff", | ||
| 351 | "version_notes": { | 322 | "version_notes": { | ||
| 352 | "es": "" | 323 | "es": "" | ||
| 353 | } | 324 | } | ||
| 354 | } | 325 | } |