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en Phosphorus retention and fractionation in an eutrophic wetland: A one-year mesocosms experiment under fluctuating flooding conditions -
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) en Phosphorus retention and fractionation in an eutrophic wetland: A one-year mesocosms experiment under fluctuating flooding conditions
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| 8 | "author": "Tercero, M.C., \u00c1lvarez Rogel, J., Conesa, H.M., | 8 | "author": "Tercero, M.C., \u00c1lvarez Rogel, J., Conesa, H.M., | ||
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| 94 | "name": "c73daf52-6c28-59d8-ab38-70afa6c24486", | 104 | "name": "c73daf52-6c28-59d8-ab38-70afa6c24486", | ||
| 95 | "notes": "This study aimed to evaluate the response of salt marshes | 105 | "notes": "This study aimed to evaluate the response of salt marshes | ||
| 96 | to pulses of PO4 3--enriched water, with and without the presence of | 106 | to pulses of PO4 3--enriched water, with and without the presence of | ||
| 97 | Phragmites australis. A one-year mesocosms experiment was performed in | 107 | Phragmites australis. A one-year mesocosms experiment was performed in | ||
| 98 | simulated soil profiles (fine-textured surface layers and sandy | 108 | simulated soil profiles (fine-textured surface layers and sandy | ||
| 99 | subsurface layers) from a coastal salt marsh of the Mar Menor lagoon | 109 | subsurface layers) from a coastal salt marsh of the Mar Menor lagoon | ||
| 100 | under alternating flooding-drying conditions with eutrophic water, | 110 | under alternating flooding-drying conditions with eutrophic water, | ||
| 101 | under low (1.95 mg L 1 P-PO4 3-) and high (19.5 mg L 1 P-PO4 3-) P | 111 | under low (1.95 mg L 1 P-PO4 3-) and high (19.5 mg L 1 P-PO4 3-) P | ||
| 102 | load, and with the presence/absence of Phragmites. The PO4 3- | 112 | load, and with the presence/absence of Phragmites. The PO4 3- | ||
| 103 | concentrations in soil porewater and drainage water were regularly | 113 | concentrations in soil porewater and drainage water were regularly | ||
| 104 | measured, and P accumulated in soils (including a fractionation | 114 | measured, and P accumulated in soils (including a fractionation | ||
| 105 | procedure) and plants (roots, rhizomes, stems and leaves) were | 115 | procedure) and plants (roots, rhizomes, stems and leaves) were | ||
| 106 | analyzed. The experimental mesocosms were highly effective in the | 116 | analyzed. The experimental mesocosms were highly effective in the | ||
| 107 | removal of P from the eutrophic flooding water (>90% reduction of the | 117 | removal of P from the eutrophic flooding water (>90% reduction of the | ||
| 108 | P added to the system both in the soil pore water and drainage water), | 118 | P added to the system both in the soil pore water and drainage water), | ||
| 109 | regardless of the nutrient load, the season of the year and the | 119 | regardless of the nutrient load, the season of the year and the | ||
| 110 | presence/absence of Phragmites. The soil was the main sink of the P | 120 | presence/absence of Phragmites. The soil was the main sink of the P | ||
| 111 | added to the system, while Phragmites had a minor role in P removal. | 121 | added to the system, while Phragmites had a minor role in P removal. | ||
| 112 | The biomass of Phragmites accumulated ~27% of the P added with the | 122 | The biomass of Phragmites accumulated ~27% of the P added with the | ||
| 113 | flooding water in the treatment with water of low P load while ~12% of | 123 | flooding water in the treatment with water of low P load while ~12% of | ||
| 114 | P in that of high P load; the rhizomes were the organs that | 124 | P in that of high P load; the rhizomes were the organs that | ||
| 115 | contributed the most (~67e72% of the total P retained by the plants). | 125 | contributed the most (~67e72% of the total P retained by the plants). | ||
| 116 | Ca/Mg compounds were the main contributors to the retention of P in | 126 | Ca/Mg compounds were the main contributors to the retention of P in | ||
| 117 | the soil compartment, especially in the fine-textured surface soil | 127 | the soil compartment, especially in the fine-textured surface soil | ||
| 118 | layers (~34e53% of the total P in the soil was present in this | 128 | layers (~34e53% of the total P in the soil was present in this | ||
| 119 | fraction). Phragmites favored the retention of P onto metal oxides | 129 | fraction). Phragmites favored the retention of P onto metal oxides | ||
| 120 | (~12% increase of the P retained in the metal oxides fraction in the | 130 | (~12% increase of the P retained in the metal oxides fraction in the | ||
| 121 | treatment with water of high P load). Hence, the use of constructed | 131 | treatment with water of high P load). Hence, the use of constructed | ||
| 122 | wetlands to ameliorate the negative impacts of P-enriched waters in | 132 | wetlands to ameliorate the negative impacts of P-enriched waters in | ||
| 123 | the Mar Menor lagoon and similar areas is recommended. We propose the | 133 | the Mar Menor lagoon and similar areas is recommended. We propose the | ||
| 124 | incorporation of fine-textured carbonated materials, with high content | 134 | incorporation of fine-textured carbonated materials, with high content | ||
| 125 | of Ca/Mg compounds, and the use of Phragmites to favor the retention | 135 | of Ca/Mg compounds, and the use of Phragmites to favor the retention | ||
| 126 | of P by these systems", | 136 | of P by these systems", | ||
| 127 | "notes_translated": { | 137 | "notes_translated": { | ||
| 128 | "es": "This study aimed to evaluate the response of salt marshes | 138 | "es": "This study aimed to evaluate the response of salt marshes | ||
| 129 | to pulses of PO4 3--enriched water, with and without the presence of | 139 | to pulses of PO4 3--enriched water, with and without the presence of | ||
| 130 | Phragmites australis. A one-year mesocosms experiment was performed in | 140 | Phragmites australis. A one-year mesocosms experiment was performed in | ||
| 131 | simulated soil profiles (fine-textured surface layers and sandy | 141 | simulated soil profiles (fine-textured surface layers and sandy | ||
| 132 | subsurface layers) from a coastal salt marsh of the Mar Menor lagoon | 142 | subsurface layers) from a coastal salt marsh of the Mar Menor lagoon | ||
| 133 | under alternating flooding-drying conditions with eutrophic water, | 143 | under alternating flooding-drying conditions with eutrophic water, | ||
| 134 | under low (1.95 mg L 1 P-PO4 3-) and high (19.5 mg L 1 P-PO4 3-) P | 144 | under low (1.95 mg L 1 P-PO4 3-) and high (19.5 mg L 1 P-PO4 3-) P | ||
| 135 | load, and with the presence/absence of Phragmites. The PO4 3- | 145 | load, and with the presence/absence of Phragmites. The PO4 3- | ||
| 136 | concentrations in soil porewater and drainage water were regularly | 146 | concentrations in soil porewater and drainage water were regularly | ||
| 137 | measured, and P accumulated in soils (including a fractionation | 147 | measured, and P accumulated in soils (including a fractionation | ||
| 138 | procedure) and plants (roots, rhizomes, stems and leaves) were | 148 | procedure) and plants (roots, rhizomes, stems and leaves) were | ||
| 139 | analyzed. The experimental mesocosms were highly effective in the | 149 | analyzed. The experimental mesocosms were highly effective in the | ||
| 140 | removal of P from the eutrophic flooding water (>90% reduction of the | 150 | removal of P from the eutrophic flooding water (>90% reduction of the | ||
| 141 | P added to the system both in the soil pore water and drainage water), | 151 | P added to the system both in the soil pore water and drainage water), | ||
| 142 | regardless of the nutrient load, the season of the year and the | 152 | regardless of the nutrient load, the season of the year and the | ||
| 143 | presence/absence of Phragmites. The soil was the main sink of the P | 153 | presence/absence of Phragmites. The soil was the main sink of the P | ||
| 144 | added to the system, while Phragmites had a minor role in P removal. | 154 | added to the system, while Phragmites had a minor role in P removal. | ||
| 145 | The biomass of Phragmites accumulated ~27% of the P added with the | 155 | The biomass of Phragmites accumulated ~27% of the P added with the | ||
| 146 | flooding water in the treatment with water of low P load while ~12% of | 156 | flooding water in the treatment with water of low P load while ~12% of | ||
| 147 | P in that of high P load; the rhizomes were the organs that | 157 | P in that of high P load; the rhizomes were the organs that | ||
| 148 | contributed the most (~67e72% of the total P retained by the plants). | 158 | contributed the most (~67e72% of the total P retained by the plants). | ||
| 149 | Ca/Mg compounds were the main contributors to the retention of P in | 159 | Ca/Mg compounds were the main contributors to the retention of P in | ||
| 150 | the soil compartment, especially in the fine-textured surface soil | 160 | the soil compartment, especially in the fine-textured surface soil | ||
| 151 | layers (~34e53% of the total P in the soil was present in this | 161 | layers (~34e53% of the total P in the soil was present in this | ||
| 152 | fraction). Phragmites favored the retention of P onto metal oxides | 162 | fraction). Phragmites favored the retention of P onto metal oxides | ||
| 153 | (~12% increase of the P retained in the metal oxides fraction in the | 163 | (~12% increase of the P retained in the metal oxides fraction in the | ||
| 154 | treatment with water of high P load). Hence, the use of constructed | 164 | treatment with water of high P load). Hence, the use of constructed | ||
| 155 | wetlands to ameliorate the negative impacts of P-enriched waters in | 165 | wetlands to ameliorate the negative impacts of P-enriched waters in | ||
| 156 | the Mar Menor lagoon and similar areas is recommended. We propose the | 166 | the Mar Menor lagoon and similar areas is recommended. We propose the | ||
| 157 | incorporation of fine-textured carbonated materials, with high content | 167 | incorporation of fine-textured carbonated materials, with high content | ||
| 158 | of Ca/Mg compounds, and the use of Phragmites to favor the retention | 168 | of Ca/Mg compounds, and the use of Phragmites to favor the retention | ||
| 159 | of P by these systems" | 169 | of P by these systems" | ||
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