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) en Combining radon, short-lived radium isotopes and hydrodynamic modeling to assess submarine groundwater discharge from an anthropized semiarid watershed to a Mediterranean lagoon (Mar Menor, SE Spain)
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| 99 | "notes": "In highly anthropized watersheds, surface water | 109 | "notes": "In highly anthropized watersheds, surface water | ||
| 100 | tributaries may carry unexpected high quantities of radon and radium | 110 | tributaries may carry unexpected high quantities of radon and radium | ||
| 101 | to coastal lagoons. Investigating submarine groundwater discharge | 111 | to coastal lagoons. Investigating submarine groundwater discharge | ||
| 102 | (SGD) with radionuclide tracers is therefore a complex task. In order | 112 | (SGD) with radionuclide tracers is therefore a complex task. In order | ||
| 103 | to quantify SGD and decipher the influence of the different water | 113 | to quantify SGD and decipher the influence of the different water | ||
| 104 | sources, we combined a radon (Rn-222) and short-lived radium (Ra-223, | 114 | sources, we combined a radon (Rn-222) and short-lived radium (Ra-223, | ||
| 105 | Ra-224) survey with the hydrodynamic modeling of a lagoon. We applied | 115 | Ra-224) survey with the hydrodynamic modeling of a lagoon. We applied | ||
| 106 | it to the Mar Menor lagoon (SE Spain) where surface water tributaries | 116 | it to the Mar Menor lagoon (SE Spain) where surface water tributaries | ||
| 107 | and undocumented emissaries carry water from groundwater drainage and | 117 | and undocumented emissaries carry water from groundwater drainage and | ||
| 108 | brines from groundwater desalinization. We identified the areas of | 118 | brines from groundwater desalinization. We identified the areas of | ||
| 109 | influence of the plume of radionuclides from the river, located major | 119 | influence of the plume of radionuclides from the river, located major | ||
| 110 | areas of SGD and proposed a location for two submarine emissaries. | 120 | areas of SGD and proposed a location for two submarine emissaries. | ||
| 111 | Porewater, i.e. interstitial water from underlying sediments, was | 121 | Porewater, i.e. interstitial water from underlying sediments, was | ||
| 112 | found to be the most representative SGD end member, compared to | 122 | found to be the most representative SGD end member, compared to | ||
| 113 | continental groundwater collected from piezometers. Mass balances in | 123 | continental groundwater collected from piezometers. Mass balances in | ||
| 114 | winter and summer seasons provided yearly SGD fluxes of water of | 124 | winter and summer seasons provided yearly SGD fluxes of water of | ||
| 115 | 0.4-2.2 10(8) 3m(3)/y (Rn-222) 4.4-19.0 . 10(8) m(3)/y (Ra-224) and | 125 | 0.4-2.2 10(8) 3m(3)/y (Rn-222) 4.4-19.0 . 10(8) m(3)/y (Ra-224) and | ||
| 116 | 1.3 . 10(8) m(3)/y (Ra-223, measured in winter only). Tidal pumping | 126 | 1.3 . 10(8) m(3)/y (Ra-223, measured in winter only). Tidal pumping | ||
| 117 | was identified as a main driver for recirculated saline groundwater, | 127 | was identified as a main driver for recirculated saline groundwater, | ||
| 118 | while fresh submarine groundwater discharge from the aquifer ranged | 128 | while fresh submarine groundwater discharge from the aquifer ranged | ||
| 119 | between 2% and 23% of total SGD.", | 129 | between 2% and 23% of total SGD.", | ||
| 120 | "notes_translated": { | 130 | "notes_translated": { | ||
| 121 | "es": "In highly anthropized watersheds, surface water tributaries | 131 | "es": "In highly anthropized watersheds, surface water tributaries | ||
| 122 | may carry unexpected high quantities of radon and radium to coastal | 132 | may carry unexpected high quantities of radon and radium to coastal | ||
| 123 | lagoons. Investigating submarine groundwater discharge (SGD) with | 133 | lagoons. Investigating submarine groundwater discharge (SGD) with | ||
| 124 | radionuclide tracers is therefore a complex task. In order to quantify | 134 | radionuclide tracers is therefore a complex task. In order to quantify | ||
| 125 | SGD and decipher the influence of the different water sources, we | 135 | SGD and decipher the influence of the different water sources, we | ||
| 126 | combined a radon (Rn-222) and short-lived radium (Ra-223, Ra-224) | 136 | combined a radon (Rn-222) and short-lived radium (Ra-223, Ra-224) | ||
| 127 | survey with the hydrodynamic modeling of a lagoon. We applied it to | 137 | survey with the hydrodynamic modeling of a lagoon. We applied it to | ||
| 128 | the Mar Menor lagoon (SE Spain) where surface water tributaries and | 138 | the Mar Menor lagoon (SE Spain) where surface water tributaries and | ||
| 129 | undocumented emissaries carry water from groundwater drainage and | 139 | undocumented emissaries carry water from groundwater drainage and | ||
| 130 | brines from groundwater desalinization. We identified the areas of | 140 | brines from groundwater desalinization. We identified the areas of | ||
| 131 | influence of the plume of radionuclides from the river, located major | 141 | influence of the plume of radionuclides from the river, located major | ||
| 132 | areas of SGD and proposed a location for two submarine emissaries. | 142 | areas of SGD and proposed a location for two submarine emissaries. | ||
| 133 | Porewater, i.e. interstitial water from underlying sediments, was | 143 | Porewater, i.e. interstitial water from underlying sediments, was | ||
| 134 | found to be the most representative SGD end member, compared to | 144 | found to be the most representative SGD end member, compared to | ||
| 135 | continental groundwater collected from piezometers. Mass balances in | 145 | continental groundwater collected from piezometers. Mass balances in | ||
| 136 | winter and summer seasons provided yearly SGD fluxes of water of | 146 | winter and summer seasons provided yearly SGD fluxes of water of | ||
| 137 | 0.4-2.2 10(8) 3m(3)/y (Rn-222) 4.4-19.0 . 10(8) m(3)/y (Ra-224) and | 147 | 0.4-2.2 10(8) 3m(3)/y (Rn-222) 4.4-19.0 . 10(8) m(3)/y (Ra-224) and | ||
| 138 | 1.3 . 10(8) m(3)/y (Ra-223, measured in winter only). Tidal pumping | 148 | 1.3 . 10(8) m(3)/y (Ra-223, measured in winter only). Tidal pumping | ||
| 139 | was identified as a main driver for recirculated saline groundwater, | 149 | was identified as a main driver for recirculated saline groundwater, | ||
| 140 | while fresh submarine groundwater discharge from the aquifer ranged | 150 | while fresh submarine groundwater discharge from the aquifer ranged | ||
| 141 | between 2% and 23% of total SGD." | 151 | between 2% and 23% of total SGD." | ||
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| 324 | "title": "Combining radon, short-lived radium isotopes and | 334 | "title": "Combining radon, short-lived radium isotopes and | ||
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| 327 | Menor, SE Spain)", | 337 | Menor, SE Spain)", | ||
| 328 | "title_translated": { | 338 | "title_translated": { | ||
| 329 | "es": "Combining radon, short-lived radium isotopes and | 339 | "es": "Combining radon, short-lived radium isotopes and | ||
| 330 | hydrodynamic modeling to assess submarine groundwater discharge from | 340 | hydrodynamic modeling to assess submarine groundwater discharge from | ||
| 331 | an anthropized semiarid watershed to a Mediterranean lagoon (Mar | 341 | an anthropized semiarid watershed to a Mediterranean lagoon (Mar | ||
| 332 | Menor, SE Spain)" | 342 | Menor, SE Spain)" | ||
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| 336 | "type": "dataset", | 346 | "type": "dataset", | ||
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