{"help": "https://pro.iepnb.gob.es/catalogo/api/3/action/help_show?name=package_show", "success": true, "result": {"access_rights": "http://inspire.ec.europa.eu/metadata-codelist/LimitationsOnPublicAccess/noLimitations", "alternate_identifier": "DOI: 10.1007/s10040-010-0658-1", "applicable_legislation": ["http://data.europa.eu/eli/reg_impl/2023/138/oj"], "author": "Jim\u00e9nez Mart\u00ednez, J., Candela, L., Molinero, J. y Tamoh, K.", "author_email": "joaquin.jimenez@upc.edu", "author_name": "Jim\u00e9nez Mart\u00ednez, J., Candela, L., Molinero, J. y Tamoh, K.", "classification_variables": {"es": ""}, "conforms_to": ["https://www.boe.es/eli/es/res/2013/02/19/(4)"], "contact_email": "organismo@example.org", "contact_name": "Organismo publicador del Cat\u00e1logo", "contact_role": "http://inspire.ec.europa.eu/metadata-codelist/ResponsiblePartyRole/pointOfContact", "contact_uri": "http://datos.gob.es/recurso/sector-publico/org/Organismo/EA0000000", "contact_url": "https://organismo.example.org/", "created": "2024-11-05", "creator_user_id": "d24a314a-79ce-48c0-abd9-54cb42706da4", "dataset_scope": "non_spatial_dataset", "dcat_type": "http://id.loc.gov/vocabulary/marcgt/art", "encoding": "UTF-8", "featured": false, "graphic_overview": "https://media.springernature.com/lw685/springer-static/image/art%3A10.1007%2Fs10040-010-0658-1/MediaObjects/10040_2010_658_Fig1_HTML.gif?as=webp", "hvd": "hvd", "hvd_category": ["http://data.europa.eu/bna/c_dd313021"], "id": "5a09523d-bbdb-5291-a180-b9eabc8e2e9a", "identifier": "5a09523d-bbdb-5291-a180-b9eabc8e2e9a", "isopen": true, "keyword_iepnb": ["agricultura", "demarcacion_hidrografica", "gestion_sostenible", "hidrodinamicas"], "language": "http://publications.europa.eu/resource/authority/language/SPA", "license_id": "cc-by", "license_title": "Creative Commons Attribution", "license_url": "http://www.opendefinition.org/licenses/cc-by", "lineage_source": ["Hydrogeology journal", "vol 18", "no 8", "1811-1824"], "maintainer": "", "maintainer_name": "", "metadata_created": "2026-06-23T14:55:35.784588", "metadata_modified": "2026-06-25T12:37:53.245250", "metadata_profile": ["https://semiceu.github.io/DCAT-AP/releases/3.0.0/"], "miteco_data_population": {"es": ""}, "miteco_data_territory": {"es": ""}, "miteco_dataset_type": "http://publications.europa.eu/resource/authority/dataset-type/STATISTICAL", "miteco_geo_level": "1", "modified": "2026-06-25", "name": "5a09523d-bbdb-5291-a180-b9eabc8e2e9a", "notes": "For semi-arid regions, methods of assessing aquifer recharge usually consider the potential evapotrans\u0002piration. Actual evapotranspiration rates can be below potential rates for long periods of time, even in irrigated systems. Accurate estimations of aquifer recharge in semi\u0002arid areas under irrigated agriculture are essential for sustainable water-resources management. A method to estimate aquifer recharge from irrigated farmland has been tested. The water-balance-modelling approach was based on VisualBALAN v. 2.0, a computer code that simulates water balance in the soil, vadose zone and aquifer. The study was carried out in the Campo de Cartagena (SE Spain) in the period 1999\u20132008 for three different groups of crops: annual row crops (lettuce and melon), perennial vegetables (artichoke) and fruit trees (citrus). Computed mean-annual-recharge values (from irrigation +precipitation) during the study period were 397mm for annual row crops, 201mm for perennial vegetables and 194mm for fruit trees: 31.4, 20.7 and 20.5% of the total applied water, respectively. 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The study was carried out in the Campo de Cartagena (SE Spain) in the period 1999\u20132008 for three different groups of crops: annual row crops (lettuce and melon), perennial vegetables (artichoke) and fruit trees (citrus). Computed mean-annual-recharge values (from irrigation +precipitation) during the study period were 397mm for annual row crops, 201mm for perennial vegetables and 194mm for fruit trees: 31.4, 20.7 and 20.5% of the total applied water, respectively. The effects of rainfall events on the final recharge were clearly observed, due to the continuously high water content in soil which facilitated the infiltration process. 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