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en Nitrate removal and potential soil N2O emissions in eutrophic salt marshes with and without Phragmites australis -
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del recurso Distribución HTML a2026-06-25
(anteriormente2026-06-23
) en Nitrate removal and potential soil N2O emissions in eutrophic salt marshes with and without Phragmites australis
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| 93 | "notes": "Wetlands are highly effective systems mitigating the | 103 | "notes": "Wetlands are highly effective systems mitigating the | ||
| 94 | negative effects of N excess, but at the same time they | 104 | negative effects of N excess, but at the same time they | ||
| 95 | con\u0002tribute to global warming through greenhouse gas emissions. | 105 | con\u0002tribute to global warming through greenhouse gas emissions. | ||
| 96 | The present study aimed to ascertain the role of Phragmites australis | 106 | The present study aimed to ascertain the role of Phragmites australis | ||
| 97 | in N transformations in eutrophic semiarid salt marshes, under low | 107 | in N transformations in eutrophic semiarid salt marshes, under low | ||
| 98 | (NO3 \u2212 = 20 mg L\u22121 ) and high (NO3 \u2212 = 200 mg L\u22121 | 108 | (NO3 \u2212 = 20 mg L\u22121 ) and high (NO3 \u2212 = 200 mg L\u22121 | ||
| 99 | ) nutrient level and alternating flooding-drying phases. Methacrylate | 109 | ) nutrient level and alternating flooding-drying phases. Methacrylate | ||
| 100 | mesocosms were filled with a saline soil, with and without the | 110 | mesocosms were filled with a saline soil, with and without the | ||
| 101 | presence of Phragmites stands, and subjected to alternating | 111 | presence of Phragmites stands, and subjected to alternating | ||
| 102 | flooding-drying conditions. For 44 weeks the soil Eh was regularly | 112 | flooding-drying conditions. For 44 weeks the soil Eh was regularly | ||
| 103 | monitored at two depths and the N-NO3 \u2212 and N-NH4 + concentration | 113 | monitored at two depths and the N-NO3 \u2212 and N-NH4 + concentration | ||
| 104 | in pore water and drainage and the potential soil N-N2O emissions to | 114 | in pore water and drainage and the potential soil N-N2O emissions to | ||
| 105 | the atmosphere measured. In the surface soil layers, more than the 80% | 115 | the atmosphere measured. In the surface soil layers, more than the 80% | ||
| 106 | of N-NO3 \u2212 was removed regardless of the presence of plants, the | 116 | of N-NO3 \u2212 was removed regardless of the presence of plants, the | ||
| 107 | nutrient level and the season of the year. Denitrification seemed to | 117 | nutrient level and the season of the year. Denitrification seemed to | ||
| 108 | be the main responsible of this. In the subsurface soil layers N-NO3 | 118 | be the main responsible of this. In the subsurface soil layers N-NO3 | ||
| 109 | \u2212 decreased an average of ~83% in presence of Phragmites and ~32% | 119 | \u2212 decreased an average of ~83% in presence of Phragmites and ~32% | ||
| 110 | without plants during the warmer period (soil temp. ~15 to ~30 | 120 | without plants during the warmer period (soil temp. ~15 to ~30 | ||
| 111 | \u00b0C), but the effectiveness was reduced to b10% during the colder | 121 | \u00b0C), but the effectiveness was reduced to b10% during the colder | ||
| 112 | period (soil temp. ~10 to ~15 \u00b0C). The N-NH4 + increased during | 122 | period (soil temp. ~10 to ~15 \u00b0C). The N-NH4 + increased during | ||
| 113 | the flooding phases (reaching 2\u2013 6 mg L\u22121 ), and the results | 123 | the flooding phases (reaching 2\u2013 6 mg L\u22121 ), and the results | ||
| 114 | indicated that it was nitrified during the following drying phases. A | 124 | indicated that it was nitrified during the following drying phases. A | ||
| 115 | tendency to lower potential soil N-N2O emissions was observed in | 125 | tendency to lower potential soil N-N2O emissions was observed in | ||
| 116 | treatments with Phragmites during drying phases, pointing that the | 126 | treatments with Phragmites during drying phases, pointing that the | ||
| 117 | plants absorbed this newly formed N-NO3 \u2212. Hence, we propose | 127 | plants absorbed this newly formed N-NO3 \u2212. Hence, we propose | ||
| 118 | harvesting Phragmites stands at the be\u0002ginning of the summer, but | 128 | harvesting Phragmites stands at the be\u0002ginning of the summer, but | ||
| 119 | after a lag time to permit N-NO3 \u2212 absorption by plants before | 129 | after a lag time to permit N-NO3 \u2212 absorption by plants before | ||
| 120 | the complete drying of the watercourses.", | 130 | the complete drying of the watercourses.", | ||
| 121 | "notes_translated": { | 131 | "notes_translated": { | ||
| 122 | "es": "Wetlands are highly effective systems mitigating the | 132 | "es": "Wetlands are highly effective systems mitigating the | ||
| 123 | negative effects of N excess, but at the same time they | 133 | negative effects of N excess, but at the same time they | ||
| 124 | con\u0002tribute to global warming through greenhouse gas emissions. | 134 | con\u0002tribute to global warming through greenhouse gas emissions. | ||
| 125 | The present study aimed to ascertain the role of Phragmites australis | 135 | The present study aimed to ascertain the role of Phragmites australis | ||
| 126 | in N transformations in eutrophic semiarid salt marshes, under low | 136 | in N transformations in eutrophic semiarid salt marshes, under low | ||
| 127 | (NO3 \u2212 = 20 mg L\u22121 ) and high (NO3 \u2212 = 200 mg L\u22121 | 137 | (NO3 \u2212 = 20 mg L\u22121 ) and high (NO3 \u2212 = 200 mg L\u22121 | ||
| 128 | ) nutrient level and alternating flooding-drying phases. Methacrylate | 138 | ) nutrient level and alternating flooding-drying phases. Methacrylate | ||
| 129 | mesocosms were filled with a saline soil, with and without the | 139 | mesocosms were filled with a saline soil, with and without the | ||
| 130 | presence of Phragmites stands, and subjected to alternating | 140 | presence of Phragmites stands, and subjected to alternating | ||
| 131 | flooding-drying conditions. For 44 weeks the soil Eh was regularly | 141 | flooding-drying conditions. For 44 weeks the soil Eh was regularly | ||
| 132 | monitored at two depths and the N-NO3 \u2212 and N-NH4 + concentration | 142 | monitored at two depths and the N-NO3 \u2212 and N-NH4 + concentration | ||
| 133 | in pore water and drainage and the potential soil N-N2O emissions to | 143 | in pore water and drainage and the potential soil N-N2O emissions to | ||
| 134 | the atmosphere measured. In the surface soil layers, more than the 80% | 144 | the atmosphere measured. In the surface soil layers, more than the 80% | ||
| 135 | of N-NO3 \u2212 was removed regardless of the presence of plants, the | 145 | of N-NO3 \u2212 was removed regardless of the presence of plants, the | ||
| 136 | nutrient level and the season of the year. Denitrification seemed to | 146 | nutrient level and the season of the year. Denitrification seemed to | ||
| 137 | be the main responsible of this. In the subsurface soil layers N-NO3 | 147 | be the main responsible of this. In the subsurface soil layers N-NO3 | ||
| 138 | \u2212 decreased an average of ~83% in presence of Phragmites and ~32% | 148 | \u2212 decreased an average of ~83% in presence of Phragmites and ~32% | ||
| 139 | without plants during the warmer period (soil temp. ~15 to ~30 | 149 | without plants during the warmer period (soil temp. ~15 to ~30 | ||
| 140 | \u00b0C), but the effectiveness was reduced to b10% during the colder | 150 | \u00b0C), but the effectiveness was reduced to b10% during the colder | ||
| 141 | period (soil temp. ~10 to ~15 \u00b0C). The N-NH4 + increased during | 151 | period (soil temp. ~10 to ~15 \u00b0C). The N-NH4 + increased during | ||
| 142 | the flooding phases (reaching 2\u2013 6 mg L\u22121 ), and the results | 152 | the flooding phases (reaching 2\u2013 6 mg L\u22121 ), and the results | ||
| 143 | indicated that it was nitrified during the following drying phases. A | 153 | indicated that it was nitrified during the following drying phases. A | ||
| 144 | tendency to lower potential soil N-N2O emissions was observed in | 154 | tendency to lower potential soil N-N2O emissions was observed in | ||
| 145 | treatments with Phragmites during drying phases, pointing that the | 155 | treatments with Phragmites during drying phases, pointing that the | ||
| 146 | plants absorbed this newly formed N-NO3 \u2212. Hence, we propose | 156 | plants absorbed this newly formed N-NO3 \u2212. Hence, we propose | ||
| 147 | harvesting Phragmites stands at the be\u0002ginning of the summer, but | 157 | harvesting Phragmites stands at the be\u0002ginning of the summer, but | ||
| 148 | after a lag time to permit N-NO3 \u2212 absorption by plants before | 158 | after a lag time to permit N-NO3 \u2212 absorption by plants before | ||
| 149 | the complete drying of the watercourses." | 159 | the complete drying of the watercourses." | ||
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