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) en Evolution and phosphorus fractionation in saline Spolic Technosols flooded with eutrophic water
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| 94 | "name": "92b11f8c-c888-566d-be11-f6d6a7c0456c", | 104 | "name": "92b11f8c-c888-566d-be11-f6d6a7c0456c", | ||
| 95 | "notes": "Purpose The aim of this study was to evaluate the | 105 | "notes": "Purpose The aim of this study was to evaluate the | ||
| 96 | behaviour of P in saline Spolic Technosols flooded with eutrophic | 106 | behaviour of P in saline Spolic Technosols flooded with eutrophic | ||
| 97 | water, with and without plant rhizosphere, in order to assess the role | 107 | water, with and without plant rhizosphere, in order to assess the role | ||
| 98 | of these soils as sinks or sources of this nutrient. Materials and | 108 | of these soils as sinks or sources of this nutrient. Materials and | ||
| 99 | methods Samples were taken from basic (pH ~7.8), carbonated and acidic | 109 | methods Samples were taken from basic (pH ~7.8), carbonated and acidic | ||
| 100 | (pH ~6.2), de-carbonated soils of salt marshes polluted by mine | 110 | (pH ~6.2), de-carbonated soils of salt marshes polluted by mine | ||
| 101 | wastes. Three treatments were assayed: pots with Sarcocornia | 111 | wastes. Three treatments were assayed: pots with Sarcocornia | ||
| 102 | fruticosa, pots with Phragmites australis and pots without plants | 112 | fruticosa, pots with Phragmites australis and pots without plants | ||
| 103 | (bare soil). The pots were flooded for 15 weeks with eutrophic water | 113 | (bare soil). The pots were flooded for 15 weeks with eutrophic water | ||
| 104 | (PO4 3\u2212 ~6.92 mg L\u22121 ) and pH, Eh and water-soluble organic | 114 | (PO4 3\u2212 ~6.92 mg L\u22121 ) and pH, Eh and water-soluble organic | ||
| 105 | carbon and PO4 3\u2212 concentrations were monitored in the soil | 115 | carbon and PO4 3\u2212 concentrations were monitored in the soil | ||
| 106 | solution. A soil P fractionation was applied before and after the | 116 | solution. A soil P fractionation was applied before and after the | ||
| 107 | flooding period. Results and discussion The PO4 3\u2212 concentration | 117 | flooding period. Results and discussion The PO4 3\u2212 concentration | ||
| 108 | in the soil solution decreased rapidly in both soils, with and without | 118 | in the soil solution decreased rapidly in both soils, with and without | ||
| 109 | plant, being diminished by 80\u201390 % after 3 h of flooding. The | 119 | plant, being diminished by 80\u201390 % after 3 h of flooding. The | ||
| 110 | Fe/Mn/Al oxides and the Ca/Mg compounds played an important role in | 120 | Fe/Mn/Al oxides and the Ca/Mg compounds played an important role in | ||
| 111 | soil P retention. In pots with S. fruticosa, the reductive conditions | 121 | soil P retention. In pots with S. fruticosa, the reductive conditions | ||
| 112 | due to flooding induced P release from metal oxides and P retention to | 122 | due to flooding induced P release from metal oxides and P retention to | ||
| 113 | Ca/Mg compounds. In turn, P. australis may have favoured the release | 123 | Ca/Mg compounds. In turn, P. australis may have favoured the release | ||
| 114 | of P from carbonates, which was transferred to Fe/Mn/Al compounds. | 124 | of P from carbonates, which was transferred to Fe/Mn/Al compounds. | ||
| 115 | Conclusions The retention of P by the soil was the main mechanism | 125 | Conclusions The retention of P by the soil was the main mechanism | ||
| 116 | involved in the removal of PO4 3\u2212 from the eutrophic flooding | 126 | involved in the removal of PO4 3\u2212 from the eutrophic flooding | ||
| 117 | water but to evaluate the capacity of these systems as long-term P | 127 | water but to evaluate the capacity of these systems as long-term P | ||
| 118 | sinks, the combined effect of metals, Ca/Mg compounds and specific | 128 | sinks, the combined effect of metals, Ca/Mg compounds and specific | ||
| 119 | plant species should be considered.", | 129 | plant species should be considered.", | ||
| 120 | "notes_translated": { | 130 | "notes_translated": { | ||
| 121 | "es": "Purpose The aim of this study was to evaluate the behaviour | 131 | "es": "Purpose The aim of this study was to evaluate the behaviour | ||
| 122 | of P in saline Spolic Technosols flooded with eutrophic water, with | 132 | of P in saline Spolic Technosols flooded with eutrophic water, with | ||
| 123 | and without plant rhizosphere, in order to assess the role of these | 133 | and without plant rhizosphere, in order to assess the role of these | ||
| 124 | soils as sinks or sources of this nutrient. Materials and methods | 134 | soils as sinks or sources of this nutrient. Materials and methods | ||
| 125 | Samples were taken from basic (pH ~7.8), carbonated and acidic (pH | 135 | Samples were taken from basic (pH ~7.8), carbonated and acidic (pH | ||
| 126 | ~6.2), de-carbonated soils of salt marshes polluted by mine wastes. | 136 | ~6.2), de-carbonated soils of salt marshes polluted by mine wastes. | ||
| 127 | Three treatments were assayed: pots with Sarcocornia fruticosa, pots | 137 | Three treatments were assayed: pots with Sarcocornia fruticosa, pots | ||
| 128 | with Phragmites australis and pots without plants (bare soil). The | 138 | with Phragmites australis and pots without plants (bare soil). The | ||
| 129 | pots were flooded for 15 weeks with eutrophic water (PO4 3\u2212 ~6.92 | 139 | pots were flooded for 15 weeks with eutrophic water (PO4 3\u2212 ~6.92 | ||
| 130 | mg L\u22121 ) and pH, Eh and water-soluble organic carbon and PO4 | 140 | mg L\u22121 ) and pH, Eh and water-soluble organic carbon and PO4 | ||
| 131 | 3\u2212 concentrations were monitored in the soil solution. A soil P | 141 | 3\u2212 concentrations were monitored in the soil solution. A soil P | ||
| 132 | fractionation was applied before and after the flooding period. | 142 | fractionation was applied before and after the flooding period. | ||
| 133 | Results and discussion The PO4 3\u2212 concentration in the soil | 143 | Results and discussion The PO4 3\u2212 concentration in the soil | ||
| 134 | solution decreased rapidly in both soils, with and without plant, | 144 | solution decreased rapidly in both soils, with and without plant, | ||
| 135 | being diminished by 80\u201390 % after 3 h of flooding. The Fe/Mn/Al | 145 | being diminished by 80\u201390 % after 3 h of flooding. The Fe/Mn/Al | ||
| 136 | oxides and the Ca/Mg compounds played an important role in soil P | 146 | oxides and the Ca/Mg compounds played an important role in soil P | ||
| 137 | retention. In pots with S. fruticosa, the reductive conditions due to | 147 | retention. In pots with S. fruticosa, the reductive conditions due to | ||
| 138 | flooding induced P release from metal oxides and P retention to Ca/Mg | 148 | flooding induced P release from metal oxides and P retention to Ca/Mg | ||
| 139 | compounds. In turn, P. australis may have favoured the release of P | 149 | compounds. In turn, P. australis may have favoured the release of P | ||
| 140 | from carbonates, which was transferred to Fe/Mn/Al compounds. | 150 | from carbonates, which was transferred to Fe/Mn/Al compounds. | ||
| 141 | Conclusions The retention of P by the soil was the main mechanism | 151 | Conclusions The retention of P by the soil was the main mechanism | ||
| 142 | involved in the removal of PO4 3\u2212 from the eutrophic flooding | 152 | involved in the removal of PO4 3\u2212 from the eutrophic flooding | ||
| 143 | water but to evaluate the capacity of these systems as long-term P | 153 | water but to evaluate the capacity of these systems as long-term P | ||
| 144 | sinks, the combined effect of metals, Ca/Mg compounds and specific | 154 | sinks, the combined effect of metals, Ca/Mg compounds and specific | ||
| 145 | plant species should be considered." | 155 | plant species should be considered." | ||
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| 285 | }, | 295 | }, | ||
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| 291 | "vocabulary_id": null | 301 | "vocabulary_id": null | ||
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| 298 | "vocabulary_id": null | 308 | "vocabulary_id": null | ||
| 299 | }, | 309 | }, | ||
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| 312 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | 322 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | ||
| 313 | ], | 323 | ], | ||
| 314 | "title": "Evolution and phosphorus fractionation in saline Spolic | 324 | "title": "Evolution and phosphorus fractionation in saline Spolic | ||
| 315 | Technosols flooded with eutrophic water", | 325 | Technosols flooded with eutrophic water", | ||
| 316 | "title_translated": { | 326 | "title_translated": { | ||
| 317 | "es": "Evolution and phosphorus fractionation in saline Spolic | 327 | "es": "Evolution and phosphorus fractionation in saline Spolic | ||
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| 325 | "version_notes": { | 335 | "version_notes": { | ||
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| 327 | } | 337 | } | ||
| 328 | } | 338 | } |