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En el instante 23 de junio de 2026, 15:51:31 UTC,
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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 Storage of organic carbon, nitrogen and phosphorus in the soil–plant system of Phragmites australis stands from a eutrophicated Mediterranean salt marsh
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| 8 | "author": "Gonz\u00e1lez Alcaraz, M.N., Egea, C., Jim\u00e9nez | 8 | "author": "Gonz\u00e1lez Alcaraz, M.N., Egea, C., Jim\u00e9nez | ||
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| 43 | "name": "Gonz\u00e1lez Alcaraz, M.N., Egea, C., Jim\u00e9nez | 43 | "name": "Gonz\u00e1lez Alcaraz, M.N., Egea, C., Jim\u00e9nez | ||
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| 66 | "suelo" | 66 | "suelo" | ||
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| n | 81 | "metadata_modified": "2026-06-23T14:48:35.779901", | n | 81 | "metadata_modified": "2026-06-23T15:51:31.603302", |
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| 85 | "miteco_data_population": { | 85 | "miteco_data_population": { | ||
| 86 | "es": "" | 86 | "es": "" | ||
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| 88 | "miteco_data_territory": { | 88 | "miteco_data_territory": { | ||
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| 92 | //publications.europa.eu/resource/authority/dataset-type/STATISTICAL", | 92 | //publications.europa.eu/resource/authority/dataset-type/STATISTICAL", | ||
| 93 | "miteco_geo_level": "1", | 93 | "miteco_geo_level": "1", | ||
| 94 | "modified": "2026-06-23", | 94 | "modified": "2026-06-23", | ||
| 95 | "name": "e01c5742-fb24-5f37-8f3b-6b9c81bdf4b7", | 95 | "name": "e01c5742-fb24-5f37-8f3b-6b9c81bdf4b7", | ||
| 96 | "notes": "In this study we quantified the different forms of | 96 | "notes": "In this study we quantified the different forms of | ||
| 97 | nitrogen, organic carbon and phosphorus in two eutrophicated | 97 | nitrogen, organic carbon and phosphorus in two eutrophicated | ||
| 98 | watercourses flowing into a coastal salt marsh of the Mar Menor lagoon | 98 | watercourses flowing into a coastal salt marsh of the Mar Menor lagoon | ||
| 99 | and analysed the role of the water flow regime in the nutrient loads | 99 | and analysed the role of the water flow regime in the nutrient loads | ||
| 100 | flowing into the salt marsh. We discuss the degree to which the | 100 | flowing into the salt marsh. We discuss the degree to which the | ||
| 101 | soil\u2013plant system in stands of Phragmites australis could be | 101 | soil\u2013plant system in stands of Phragmites australis could be | ||
| 102 | affected by the discharges of nutrients and estimate the stocks of | 102 | affected by the discharges of nutrients and estimate the stocks of | ||
| 103 | nitrogen, phosphorus and organic carbon in different compartments of | 103 | nitrogen, phosphorus and organic carbon in different compartments of | ||
| 104 | the system. The base flow sustained an important discharge of surplus | 104 | the system. The base flow sustained an important discharge of surplus | ||
| 105 | water of agricultural origin enriched in dissolved organic carbon | 105 | water of agricultural origin enriched in dissolved organic carbon | ||
| 106 | (12.7 T y\u22121 ) and nitrogen (78.3 T y\u22121 , 85 % N\u2013NO3 | 106 | (12.7 T y\u22121 ) and nitrogen (78.3 T y\u22121 , 85 % N\u2013NO3 | ||
| 107 | \u2212 and 15% organic\u2013N) into the salt marsh, while inputs from | 107 | \u2212 and 15% organic\u2013N) into the salt marsh, while inputs from | ||
| 108 | wastewater-treatment plants were of much lower magnitude (5.5 T | 108 | wastewater-treatment plants were of much lower magnitude (5.5 T | ||
| 109 | y\u22121 of dissolved organic carbon and 4.1 T y\u22121 of nitrogen, | 109 | y\u22121 of dissolved organic carbon and 4.1 T y\u22121 of nitrogen, | ||
| 110 | 57 % N\u2013NH4 + and 43% organic\u2013N). The annual loads of | 110 | 57 % N\u2013NH4 + and 43% organic\u2013N). The annual loads of | ||
| 111 | phosphorus of agricultural origin and from urban wastewater were 1.87 | 111 | phosphorus of agricultural origin and from urban wastewater were 1.87 | ||
| 112 | T y\u22121 and 0.97 T y\u22121 , respectively. The data show that the | 112 | T y\u22121 and 0.97 T y\u22121 , respectively. The data show that the | ||
| 113 | high amounts of inorganic nitrogen from agricultural activity are | 113 | high amounts of inorganic nitrogen from agricultural activity are | ||
| 114 | absorbed by vegetation or denitrified, while organic nitrogen probably | 114 | absorbed by vegetation or denitrified, while organic nitrogen probably | ||
| 115 | helps to compen\u0002sate for soil nitrogen lost by mineralisation. | 115 | helps to compen\u0002sate for soil nitrogen lost by mineralisation. | ||
| 116 | The soils of the salt marsh may be considered a sink for phosphorus | 116 | The soils of the salt marsh may be considered a sink for phosphorus | ||
| 117 | flowing into it in wastewater. The tissues of P. australis showed | 117 | flowing into it in wastewater. The tissues of P. australis showed | ||
| 118 | differing patterns of accumulation and transloca\u0002tion of carbon, | 118 | differing patterns of accumulation and transloca\u0002tion of carbon, | ||
| 119 | nitrogen and phosphorus; the concentrations of these three elements | 119 | nitrogen and phosphorus; the concentrations of these three elements | ||
| 120 | changed with the season but apparently were not affected by the | 120 | changed with the season but apparently were not affected by the | ||
| 121 | eutrophicated water that the plants received. Soil salinity, pH, Fe | 121 | eutrophicated water that the plants received. Soil salinity, pH, Fe | ||
| 122 | concentrations and phosphorus content had little influence on litter | 122 | concentrations and phosphorus content had little influence on litter | ||
| 123 | quality. Dry stems were important reser\u0002voirs of organic carbon | 123 | quality. Dry stems were important reser\u0002voirs of organic carbon | ||
| 124 | since they persisted throughout the year, while dry leaves were the | 124 | since they persisted throughout the year, while dry leaves were the | ||
| 125 | main contributors to the litter, which was mineralised partially | 125 | main contributors to the litter, which was mineralised partially | ||
| 126 | during spring and summer. Calculations of primary productiv\u0002ity | 126 | during spring and summer. Calculations of primary productiv\u0002ity | ||
| 127 | showed a positive balance of carbon in the below-ground biomass (595 g | 127 | showed a positive balance of carbon in the below-ground biomass (595 g | ||
| 128 | m\u22122 y\u22121 ), above-ground (2610 g m\u22122 y\u22121 ) and | 128 | m\u22122 y\u22121 ), above-ground (2610 g m\u22122 y\u22121 ) and | ||
| 129 | litter (260 g m\u22122 y\u22121 ). The average soil organic carbon | 129 | litter (260 g m\u22122 y\u22121 ). The average soil organic carbon | ||
| 130 | concentration decreased in one of the plots studied, probably because | 130 | concentration decreased in one of the plots studied, probably because | ||
| 131 | mineralisation was favoured since the soil was dry most of the time. | 131 | mineralisation was favoured since the soil was dry most of the time. | ||
| 132 | Hence, our data suggest that although the high biomass production of | 132 | Hence, our data suggest that although the high biomass production of | ||
| 133 | Phragmites favours carbon sequestration in plant biomass, soil organic | 133 | Phragmites favours carbon sequestration in plant biomass, soil organic | ||
| 134 | carbon losses in stands of this species may be very important | 134 | carbon losses in stands of this species may be very important | ||
| 135 | throughout the year.", | 135 | throughout the year.", | ||
| 136 | "notes_translated": { | 136 | "notes_translated": { | ||
| 137 | "es": "In this study we quantified the different forms of | 137 | "es": "In this study we quantified the different forms of | ||
| 138 | nitrogen, organic carbon and phosphorus in two eutrophicated | 138 | nitrogen, organic carbon and phosphorus in two eutrophicated | ||
| 139 | watercourses flowing into a coastal salt marsh of the Mar Menor lagoon | 139 | watercourses flowing into a coastal salt marsh of the Mar Menor lagoon | ||
| 140 | and analysed the role of the water flow regime in the nutrient loads | 140 | and analysed the role of the water flow regime in the nutrient loads | ||
| 141 | flowing into the salt marsh. We discuss the degree to which the | 141 | flowing into the salt marsh. We discuss the degree to which the | ||
| 142 | soil\u2013plant system in stands of Phragmites australis could be | 142 | soil\u2013plant system in stands of Phragmites australis could be | ||
| 143 | affected by the discharges of nutrients and estimate the stocks of | 143 | affected by the discharges of nutrients and estimate the stocks of | ||
| 144 | nitrogen, phosphorus and organic carbon in different compartments of | 144 | nitrogen, phosphorus and organic carbon in different compartments of | ||
| 145 | the system. The base flow sustained an important discharge of surplus | 145 | the system. The base flow sustained an important discharge of surplus | ||
| 146 | water of agricultural origin enriched in dissolved organic carbon | 146 | water of agricultural origin enriched in dissolved organic carbon | ||
| 147 | (12.7 T y\u22121 ) and nitrogen (78.3 T y\u22121 , 85 % N\u2013NO3 | 147 | (12.7 T y\u22121 ) and nitrogen (78.3 T y\u22121 , 85 % N\u2013NO3 | ||
| 148 | \u2212 and 15% organic\u2013N) into the salt marsh, while inputs from | 148 | \u2212 and 15% organic\u2013N) into the salt marsh, while inputs from | ||
| 149 | wastewater-treatment plants were of much lower magnitude (5.5 T | 149 | wastewater-treatment plants were of much lower magnitude (5.5 T | ||
| 150 | y\u22121 of dissolved organic carbon and 4.1 T y\u22121 of nitrogen, | 150 | y\u22121 of dissolved organic carbon and 4.1 T y\u22121 of nitrogen, | ||
| 151 | 57 % N\u2013NH4 + and 43% organic\u2013N). The annual loads of | 151 | 57 % N\u2013NH4 + and 43% organic\u2013N). The annual loads of | ||
| 152 | phosphorus of agricultural origin and from urban wastewater were 1.87 | 152 | phosphorus of agricultural origin and from urban wastewater were 1.87 | ||
| 153 | T y\u22121 and 0.97 T y\u22121 , respectively. The data show that the | 153 | T y\u22121 and 0.97 T y\u22121 , respectively. The data show that the | ||
| 154 | high amounts of inorganic nitrogen from agricultural activity are | 154 | high amounts of inorganic nitrogen from agricultural activity are | ||
| 155 | absorbed by vegetation or denitrified, while organic nitrogen probably | 155 | absorbed by vegetation or denitrified, while organic nitrogen probably | ||
| 156 | helps to compen\u0002sate for soil nitrogen lost by mineralisation. | 156 | helps to compen\u0002sate for soil nitrogen lost by mineralisation. | ||
| 157 | The soils of the salt marsh may be considered a sink for phosphorus | 157 | The soils of the salt marsh may be considered a sink for phosphorus | ||
| 158 | flowing into it in wastewater. The tissues of P. australis showed | 158 | flowing into it in wastewater. The tissues of P. australis showed | ||
| 159 | differing patterns of accumulation and transloca\u0002tion of carbon, | 159 | differing patterns of accumulation and transloca\u0002tion of carbon, | ||
| 160 | nitrogen and phosphorus; the concentrations of these three elements | 160 | nitrogen and phosphorus; the concentrations of these three elements | ||
| 161 | changed with the season but apparently were not affected by the | 161 | changed with the season but apparently were not affected by the | ||
| 162 | eutrophicated water that the plants received. Soil salinity, pH, Fe | 162 | eutrophicated water that the plants received. Soil salinity, pH, Fe | ||
| 163 | concentrations and phosphorus content had little influence on litter | 163 | concentrations and phosphorus content had little influence on litter | ||
| 164 | quality. Dry stems were important reser\u0002voirs of organic carbon | 164 | quality. Dry stems were important reser\u0002voirs of organic carbon | ||
| 165 | since they persisted throughout the year, while dry leaves were the | 165 | since they persisted throughout the year, while dry leaves were the | ||
| 166 | main contributors to the litter, which was mineralised partially | 166 | main contributors to the litter, which was mineralised partially | ||
| 167 | during spring and summer. Calculations of primary productiv\u0002ity | 167 | during spring and summer. Calculations of primary productiv\u0002ity | ||
| 168 | showed a positive balance of carbon in the below-ground biomass (595 g | 168 | showed a positive balance of carbon in the below-ground biomass (595 g | ||
| 169 | m\u22122 y\u22121 ), above-ground (2610 g m\u22122 y\u22121 ) and | 169 | m\u22122 y\u22121 ), above-ground (2610 g m\u22122 y\u22121 ) and | ||
| 170 | litter (260 g m\u22122 y\u22121 ). The average soil organic carbon | 170 | litter (260 g m\u22122 y\u22121 ). The average soil organic carbon | ||
| 171 | concentration decreased in one of the plots studied, probably because | 171 | concentration decreased in one of the plots studied, probably because | ||
| 172 | mineralisation was favoured since the soil was dry most of the time. | 172 | mineralisation was favoured since the soil was dry most of the time. | ||
| 173 | Hence, our data suggest that although the high biomass production of | 173 | Hence, our data suggest that although the high biomass production of | ||
| 174 | Phragmites favours carbon sequestration in plant biomass, soil organic | 174 | Phragmites favours carbon sequestration in plant biomass, soil organic | ||
| 175 | carbon losses in stands of this species may be very important | 175 | carbon losses in stands of this species may be very important | ||
| 176 | throughout the year." | 176 | throughout the year." | ||
| 177 | }, | 177 | }, | ||
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