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En el instante 23 de junio de 2026, 16:13:03 UTC,
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Modificado el valor del campo
spatial_coverage
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en Using the radium quartet to quantify submarine groundwater discharge and porewater exchange
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| 95 | "notes": "The specific ingrowth rates of different radium isotopes | 95 | "notes": "The specific ingrowth rates of different radium isotopes | ||
| 96 | make them valuable tracers to distinguish processes occurring at | 96 | make them valuable tracers to distinguish processes occurring at | ||
| 97 | different temporal scales. Here we demonstrate the use of the radium | 97 | different temporal scales. Here we demonstrate the use of the radium | ||
| 98 | quartet (223Ra, 224Ra, 226Ra and 228Ra) to differentiate flows of | 98 | quartet (223Ra, 224Ra, 226Ra and 228Ra) to differentiate flows of | ||
| 99 | submarine groundwater discharge and porewater exchange to a coastal | 99 | submarine groundwater discharge and porewater exchange to a coastal | ||
| 100 | embayment (Alfacs Bay, NW Mediterranean Sea), based on the assumption | 100 | embayment (Alfacs Bay, NW Mediterranean Sea), based on the assumption | ||
| 101 | that these processes occur on different time scales. In order to | 101 | that these processes occur on different time scales. In order to | ||
| 102 | evaluate the seasonal dynamics of groundwater and porewater inputs to | 102 | evaluate the seasonal dynamics of groundwater and porewater inputs to | ||
| 103 | the bay, we conducted three seasonal samplings at Alfacs Bay, during | 103 | the bay, we conducted three seasonal samplings at Alfacs Bay, during | ||
| 104 | which samples for Ra isotopes were collected from bay waters, | 104 | which samples for Ra isotopes were collected from bay waters, | ||
| 105 | groundwater springs, porewaters and irrigation channels. Activities of | 105 | groundwater springs, porewaters and irrigation channels. Activities of | ||
| 106 | short\u0002lived Ra isotopes in the bay showed a strong seasonality, | 106 | short\u0002lived Ra isotopes in the bay showed a strong seasonality, | ||
| 107 | (e.g. average 224Ra activities in summer (\u000132 dpm 100 L\u00031 ) | 107 | (e.g. average 224Ra activities in summer (\u000132 dpm 100 L\u00031 ) | ||
| 108 | up to 4 times higher than in winter (\u00018 dpm 100 L\u00031 )). In | 108 | up to 4 times higher than in winter (\u00018 dpm 100 L\u00031 )). In | ||
| 109 | contrast, the activities of the long-lived Ra isotopes were fairly | 109 | contrast, the activities of the long-lived Ra isotopes were fairly | ||
| 110 | constant throughout the year (e.g. activities of 226Ra were \u000116 | 110 | constant throughout the year (e.g. activities of 226Ra were \u000116 | ||
| 111 | and \u000114 dpm 100 L\u00031 in summer and winter, respectively). The | 111 | and \u000114 dpm 100 L\u00031 in summer and winter, respectively). The | ||
| 112 | rela\u0002tively short exposure to sediments of recirculation fluxes | 112 | rela\u0002tively short exposure to sediments of recirculation fluxes | ||
| 113 | resulted in porewaters significantly enriched in short-lived Ra | 113 | resulted in porewaters significantly enriched in short-lived Ra | ||
| 114 | iso\u0002topes relative to the long-lived ones. The distinct | 114 | iso\u0002topes relative to the long-lived ones. The distinct | ||
| 115 | signatures of different sources allowed us to construct seasonal Ra | 115 | signatures of different sources allowed us to construct seasonal Ra | ||
| 116 | mass balances to estimate both groundwater dis\u0002charge, which | 116 | mass balances to estimate both groundwater dis\u0002charge, which | ||
| 117 | ranges from (40 \u00b1 60)\u0004103 m3 \u0004d\u00031 in summer to | 117 | ranges from (40 \u00b1 60)\u0004103 m3 \u0004d\u00031 in summer to | ||
| 118 | (310 \u00b1 200)\u0004103 m3 \u0004d\u00031 in winter, and porewater | 118 | (310 \u00b1 200)\u0004103 m3 \u0004d\u00031 in winter, and porewater | ||
| 119 | exchange fluxes, ranging from (1200 \u00b1 120)\u0004103 m3 | 119 | exchange fluxes, ranging from (1200 \u00b1 120)\u0004103 m3 | ||
| 120 | \u0004d\u00031 in summer to (270 \u00b1 40)\u0004103 m3 \u0004d\u00031 | 120 | \u0004d\u00031 in summer to (270 \u00b1 40)\u0004103 m3 \u0004d\u00031 | ||
| 121 | in winter. Whereas the seasonal variability of groundwater inputs is | 121 | in winter. Whereas the seasonal variability of groundwater inputs is | ||
| 122 | likely governed by the terrestrial hydraulic gradient, a qualitative | 122 | likely governed by the terrestrial hydraulic gradient, a qualitative | ||
| 123 | evaluation of the drivers of pore\u0002water exchange suggested that | 123 | evaluation of the drivers of pore\u0002water exchange suggested that | ||
| 124 | the strong seasonality of the seawater recirculation inputs is likely | 124 | the strong seasonality of the seawater recirculation inputs is likely | ||
| 125 | mediated by seasonal cycles on the activity of benthic infauna. Ra | 125 | mediated by seasonal cycles on the activity of benthic infauna. Ra | ||
| 126 | isotopes are thus valuable tracers to differentiate fluxes of both | 126 | isotopes are thus valuable tracers to differentiate fluxes of both | ||
| 127 | submarine groundwater discharge and porewater exchange, allowing a | 127 | submarine groundwater discharge and porewater exchange, allowing a | ||
| 128 | more accurate evaluation of the fluxes of freshwater and solutes to | 128 | more accurate evaluation of the fluxes of freshwater and solutes to | ||
| 129 | coastal ecosystems, as well as their implications for coastal | 129 | coastal ecosystems, as well as their implications for coastal | ||
| 130 | biogeochemical cycles.", | 130 | biogeochemical cycles.", | ||
| 131 | "notes_translated": { | 131 | "notes_translated": { | ||
| 132 | "es": "The specific ingrowth rates of different radium isotopes | 132 | "es": "The specific ingrowth rates of different radium isotopes | ||
| 133 | make them valuable tracers to distinguish processes occurring at | 133 | make them valuable tracers to distinguish processes occurring at | ||
| 134 | different temporal scales. Here we demonstrate the use of the radium | 134 | different temporal scales. Here we demonstrate the use of the radium | ||
| 135 | quartet (223Ra, 224Ra, 226Ra and 228Ra) to differentiate flows of | 135 | quartet (223Ra, 224Ra, 226Ra and 228Ra) to differentiate flows of | ||
| 136 | submarine groundwater discharge and porewater exchange to a coastal | 136 | submarine groundwater discharge and porewater exchange to a coastal | ||
| 137 | embayment (Alfacs Bay, NW Mediterranean Sea), based on the assumption | 137 | embayment (Alfacs Bay, NW Mediterranean Sea), based on the assumption | ||
| 138 | that these processes occur on different time scales. In order to | 138 | that these processes occur on different time scales. In order to | ||
| 139 | evaluate the seasonal dynamics of groundwater and porewater inputs to | 139 | evaluate the seasonal dynamics of groundwater and porewater inputs to | ||
| 140 | the bay, we conducted three seasonal samplings at Alfacs Bay, during | 140 | the bay, we conducted three seasonal samplings at Alfacs Bay, during | ||
| 141 | which samples for Ra isotopes were collected from bay waters, | 141 | which samples for Ra isotopes were collected from bay waters, | ||
| 142 | groundwater springs, porewaters and irrigation channels. Activities of | 142 | groundwater springs, porewaters and irrigation channels. Activities of | ||
| 143 | short\u0002lived Ra isotopes in the bay showed a strong seasonality, | 143 | short\u0002lived Ra isotopes in the bay showed a strong seasonality, | ||
| 144 | (e.g. average 224Ra activities in summer (\u000132 dpm 100 L\u00031 ) | 144 | (e.g. average 224Ra activities in summer (\u000132 dpm 100 L\u00031 ) | ||
| 145 | up to 4 times higher than in winter (\u00018 dpm 100 L\u00031 )). In | 145 | up to 4 times higher than in winter (\u00018 dpm 100 L\u00031 )). In | ||
| 146 | contrast, the activities of the long-lived Ra isotopes were fairly | 146 | contrast, the activities of the long-lived Ra isotopes were fairly | ||
| 147 | constant throughout the year (e.g. activities of 226Ra were \u000116 | 147 | constant throughout the year (e.g. activities of 226Ra were \u000116 | ||
| 148 | and \u000114 dpm 100 L\u00031 in summer and winter, respectively). The | 148 | and \u000114 dpm 100 L\u00031 in summer and winter, respectively). The | ||
| 149 | rela\u0002tively short exposure to sediments of recirculation fluxes | 149 | rela\u0002tively short exposure to sediments of recirculation fluxes | ||
| 150 | resulted in porewaters significantly enriched in short-lived Ra | 150 | resulted in porewaters significantly enriched in short-lived Ra | ||
| 151 | iso\u0002topes relative to the long-lived ones. The distinct | 151 | iso\u0002topes relative to the long-lived ones. The distinct | ||
| 152 | signatures of different sources allowed us to construct seasonal Ra | 152 | signatures of different sources allowed us to construct seasonal Ra | ||
| 153 | mass balances to estimate both groundwater dis\u0002charge, which | 153 | mass balances to estimate both groundwater dis\u0002charge, which | ||
| 154 | ranges from (40 \u00b1 60)\u0004103 m3 \u0004d\u00031 in summer to | 154 | ranges from (40 \u00b1 60)\u0004103 m3 \u0004d\u00031 in summer to | ||
| 155 | (310 \u00b1 200)\u0004103 m3 \u0004d\u00031 in winter, and porewater | 155 | (310 \u00b1 200)\u0004103 m3 \u0004d\u00031 in winter, and porewater | ||
| 156 | exchange fluxes, ranging from (1200 \u00b1 120)\u0004103 m3 | 156 | exchange fluxes, ranging from (1200 \u00b1 120)\u0004103 m3 | ||
| 157 | \u0004d\u00031 in summer to (270 \u00b1 40)\u0004103 m3 \u0004d\u00031 | 157 | \u0004d\u00031 in summer to (270 \u00b1 40)\u0004103 m3 \u0004d\u00031 | ||
| 158 | in winter. Whereas the seasonal variability of groundwater inputs is | 158 | in winter. Whereas the seasonal variability of groundwater inputs is | ||
| 159 | likely governed by the terrestrial hydraulic gradient, a qualitative | 159 | likely governed by the terrestrial hydraulic gradient, a qualitative | ||
| 160 | evaluation of the drivers of pore\u0002water exchange suggested that | 160 | evaluation of the drivers of pore\u0002water exchange suggested that | ||
| 161 | the strong seasonality of the seawater recirculation inputs is likely | 161 | the strong seasonality of the seawater recirculation inputs is likely | ||
| 162 | mediated by seasonal cycles on the activity of benthic infauna. Ra | 162 | mediated by seasonal cycles on the activity of benthic infauna. Ra | ||
| 163 | isotopes are thus valuable tracers to differentiate fluxes of both | 163 | isotopes are thus valuable tracers to differentiate fluxes of both | ||
| 164 | submarine groundwater discharge and porewater exchange, allowing a | 164 | submarine groundwater discharge and porewater exchange, allowing a | ||
| 165 | more accurate evaluation of the fluxes of freshwater and solutes to | 165 | more accurate evaluation of the fluxes of freshwater and solutes to | ||
| 166 | coastal ecosystems, as well as their implications for coastal | 166 | coastal ecosystems, as well as their implications for coastal | ||
| 167 | biogeochemical cycles." | 167 | biogeochemical cycles." | ||
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