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) en Assessing different methods to quantify Submarine Groundwater Discharge
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| 87 | "notes": "Submarine Groundwater Discharge (SGD) is recognized as a | 97 | "notes": "Submarine Groundwater Discharge (SGD) is recognized as a | ||
| 88 | major source of water and solutes to the coastal ocean, and it is | 98 | major source of water and solutes to the coastal ocean, and it is | ||
| 89 | particularly relevant in arid or semi-arid zones. SGD is generally | 99 | particularly relevant in arid or semi-arid zones. SGD is generally | ||
| 90 | defined as the flow of groundwater from continental margins to the | 100 | defined as the flow of groundwater from continental margins to the | ||
| 91 | coastal ocean, including thus both fresh groundwater from aquifer | 101 | coastal ocean, including thus both fresh groundwater from aquifer | ||
| 92 | recharge and seawater recirculation through the coastal aquifer. Due | 102 | recharge and seawater recirculation through the coastal aquifer. Due | ||
| 93 | to its high heterogeneity both in space and time, SGD is difficult to | 103 | to its high heterogeneity both in space and time, SGD is difficult to | ||
| 94 | detect and quantify. As a consequence, numerous methods to study SGD | 104 | detect and quantify. As a consequence, numerous methods to study SGD | ||
| 95 | have been developed over the last decades. These approaches mainly | 105 | have been developed over the last decades. These approaches mainly | ||
| 96 | include hydrogeological approaches, geophysical techniques, direct | 106 | include hydrogeological approaches, geophysical techniques, direct | ||
| 97 | seepage measurements, and the use of geochemical tracers. Each method | 107 | seepage measurements, and the use of geochemical tracers. Each method | ||
| 98 | presents its challenges, limitations, and advantages and each one | 108 | presents its challenges, limitations, and advantages and each one | ||
| 99 | works on different spatial and temporal scales, thus targeting | 109 | works on different spatial and temporal scales, thus targeting | ||
| 100 | different components of SGD. Therefore, comparing SGD studies with | 110 | different components of SGD. Therefore, comparing SGD studies with | ||
| 101 | estimates derived from different methods is often complex and | 111 | estimates derived from different methods is often complex and | ||
| 102 | misleading if the characteristics and assumptions of each | 112 | misleading if the characteristics and assumptions of each | ||
| 103 | quantification technique are not taken into account. This highlights | 113 | quantification technique are not taken into account. This highlights | ||
| 104 | the need to conduct studies comparing SGD derived from different | 114 | the need to conduct studies comparing SGD derived from different | ||
| 105 | methods, not only to obtain more accurate SGD estimates but also to | 115 | methods, not only to obtain more accurate SGD estimates but also to | ||
| 106 | obtain instrumental information on the characteristics of the | 116 | obtain instrumental information on the characteristics of the | ||
| 107 | estimated fluxes. To this aim, a combined use of different approaches | 117 | estimated fluxes. To this aim, a combined use of different approaches | ||
| 108 | to estimate SGD was applied in a Mediterranean coastal lagoon (Mar | 118 | to estimate SGD was applied in a Mediterranean coastal lagoon (Mar | ||
| 109 | Menor, Spain), including direct measurements with seepage meters, | 119 | Menor, Spain), including direct measurements with seepage meters, | ||
| 110 | radium isotopes, and radon mass balance, 224Ra/228Th disequilibrium in | 120 | radium isotopes, and radon mass balance, 224Ra/228Th disequilibrium in | ||
| 111 | coastal sediments, radon vertical profiles in porewater sediments, and | 121 | coastal sediments, radon vertical profiles in porewater sediments, and | ||
| 112 | hydrologic modeling. Mar Menor is Europe's biggest saline coastal | 122 | hydrologic modeling. Mar Menor is Europe's biggest saline coastal | ||
| 113 | lagoon, and it is connected to a highly anthropized quaternary | 123 | lagoon, and it is connected to a highly anthropized quaternary | ||
| 114 | aquifer. In this coastal system, SGD is likely playing a major role in | 124 | aquifer. In this coastal system, SGD is likely playing a major role in | ||
| 115 | the eutrophication of the lagoon. However, despite the economic and | 125 | the eutrophication of the lagoon. However, despite the economic and | ||
| 116 | biological importance of this lagoon, data about this system is still | 126 | biological importance of this lagoon, data about this system is still | ||
| 117 | incomplete, and mostly only hydrological modeling has been | 127 | incomplete, and mostly only hydrological modeling has been | ||
| 118 | performed.", | 128 | performed.", | ||
| 119 | "notes_translated": { | 129 | "notes_translated": { | ||
| 120 | "es": "Submarine Groundwater Discharge (SGD) is recognized as a | 130 | "es": "Submarine Groundwater Discharge (SGD) is recognized as a | ||
| 121 | major source of water and solutes to the coastal ocean, and it is | 131 | major source of water and solutes to the coastal ocean, and it is | ||
| 122 | particularly relevant in arid or semi-arid zones. SGD is generally | 132 | particularly relevant in arid or semi-arid zones. SGD is generally | ||
| 123 | defined as the flow of groundwater from continental margins to the | 133 | defined as the flow of groundwater from continental margins to the | ||
| 124 | coastal ocean, including thus both fresh groundwater from aquifer | 134 | coastal ocean, including thus both fresh groundwater from aquifer | ||
| 125 | recharge and seawater recirculation through the coastal aquifer. Due | 135 | recharge and seawater recirculation through the coastal aquifer. Due | ||
| 126 | to its high heterogeneity both in space and time, SGD is difficult to | 136 | to its high heterogeneity both in space and time, SGD is difficult to | ||
| 127 | detect and quantify. As a consequence, numerous methods to study SGD | 137 | detect and quantify. As a consequence, numerous methods to study SGD | ||
| 128 | have been developed over the last decades. These approaches mainly | 138 | have been developed over the last decades. These approaches mainly | ||
| 129 | include hydrogeological approaches, geophysical techniques, direct | 139 | include hydrogeological approaches, geophysical techniques, direct | ||
| 130 | seepage measurements, and the use of geochemical tracers. Each method | 140 | seepage measurements, and the use of geochemical tracers. Each method | ||
| 131 | presents its challenges, limitations, and advantages and each one | 141 | presents its challenges, limitations, and advantages and each one | ||
| 132 | works on different spatial and temporal scales, thus targeting | 142 | works on different spatial and temporal scales, thus targeting | ||
| 133 | different components of SGD. Therefore, comparing SGD studies with | 143 | different components of SGD. Therefore, comparing SGD studies with | ||
| 134 | estimates derived from different methods is often complex and | 144 | estimates derived from different methods is often complex and | ||
| 135 | misleading if the characteristics and assumptions of each | 145 | misleading if the characteristics and assumptions of each | ||
| 136 | quantification technique are not taken into account. This highlights | 146 | quantification technique are not taken into account. This highlights | ||
| 137 | the need to conduct studies comparing SGD derived from different | 147 | the need to conduct studies comparing SGD derived from different | ||
| 138 | methods, not only to obtain more accurate SGD estimates but also to | 148 | methods, not only to obtain more accurate SGD estimates but also to | ||
| 139 | obtain instrumental information on the characteristics of the | 149 | obtain instrumental information on the characteristics of the | ||
| 140 | estimated fluxes. To this aim, a combined use of different approaches | 150 | estimated fluxes. To this aim, a combined use of different approaches | ||
| 141 | to estimate SGD was applied in a Mediterranean coastal lagoon (Mar | 151 | to estimate SGD was applied in a Mediterranean coastal lagoon (Mar | ||
| 142 | Menor, Spain), including direct measurements with seepage meters, | 152 | Menor, Spain), including direct measurements with seepage meters, | ||
| 143 | radium isotopes, and radon mass balance, 224Ra/228Th disequilibrium in | 153 | radium isotopes, and radon mass balance, 224Ra/228Th disequilibrium in | ||
| 144 | coastal sediments, radon vertical profiles in porewater sediments, and | 154 | coastal sediments, radon vertical profiles in porewater sediments, and | ||
| 145 | hydrologic modeling. Mar Menor is Europe's biggest saline coastal | 155 | hydrologic modeling. Mar Menor is Europe's biggest saline coastal | ||
| 146 | lagoon, and it is connected to a highly anthropized quaternary | 156 | lagoon, and it is connected to a highly anthropized quaternary | ||
| 147 | aquifer. In this coastal system, SGD is likely playing a major role in | 157 | aquifer. In this coastal system, SGD is likely playing a major role in | ||
| 148 | the eutrophication of the lagoon. However, despite the economic and | 158 | the eutrophication of the lagoon. However, despite the economic and | ||
| 149 | biological importance of this lagoon, data about this system is still | 159 | biological importance of this lagoon, data about this system is still | ||
| 150 | incomplete, and mostly only hydrological modeling has been performed." | 160 | incomplete, and mostly only hydrological modeling has been performed." | ||
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| 279 | "id": "004084d1-68d8-46ca-842a-c10278540bc9", | 289 | "id": "004084d1-68d8-46ca-842a-c10278540bc9", | ||
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| 290 | ], | 300 | ], | ||
| 291 | "title": "Assessing different methods to quantify Submarine | 301 | "title": "Assessing different methods to quantify Submarine | ||
| 292 | Groundwater Discharge", | 302 | Groundwater Discharge", | ||
| 293 | "title_translated": { | 303 | "title_translated": { | ||
| 294 | "es": "Assessing different methods to quantify Submarine | 304 | "es": "Assessing different methods to quantify Submarine | ||
| 295 | Groundwater Discharge" | 305 | Groundwater Discharge" | ||
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| 299 | "type": "dataset", | 309 | "type": "dataset", | ||
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| 302 | "version_notes": { | 312 | "version_notes": { | ||
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| 304 | } | 314 | } | ||
| 305 | } | 315 | } |