Nitrogen enrichment buffers phosphorus limitation by mobilizing mineral-bound soil phosphorus in grasslands
Phosphorus (P) limitation is expected to increase due to nitrogen (N)-induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pi) and organic matter (Pₒ). Here we assessed whether transformations of these P pools could increase plant available pools all...
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| Vydáno v: | Ecology (Durham) Ročník 103; číslo 3; s. 1 - 15 |
|---|---|
| Hlavní autoři: | , , , , , , , , , , , |
| Médium: | Journal Article |
| Jazyk: | angličtina |
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Hoboken, USA
John Wiley and Sons, Inc
01.03.2022
John Wiley & Sons, Inc Ecological Society of America |
| Témata: | |
| ISSN: | 0012-9658, 1939-9170, 1939-9170 |
| On-line přístup: | Získat plný text |
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| Abstract | Phosphorus (P) limitation is expected to increase due to nitrogen (N)-induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pi) and organic matter (Pₒ). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10-year field N addition experiment and a 3700-km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile Pi (mainly Ca-bound recalcitrant P) to more available forms of Pi (including Al- and Fe-bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect Pₒ. Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg−1, whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg−1 after the 10-year N addition, associated with an increase in Pi mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile Pi and immobile Pi. Our results provide a new mechanistic understanding of the important role of soil Pi mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. |
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| AbstractList | Phosphorus (P) limitation is expected to increase due to nitrogen (N)-induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (P
) and organic matter (P
). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10-year field N addition experiment and a 3700-km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile P
(mainly Ca-bound recalcitrant P) to more available forms of P
(including Al- and Fe-bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect P
. Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg
, whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg
after the 10-year N addition, associated with an increase in P
mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile P
and immobile P
. Our results provide a new mechanistic understanding of the important role of soil P
mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. Phosphorus (P) limitation is expected to increase due to nitrogen (N)‐induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pᵢ) and organic matter (Pₒ). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10‐year field N addition experiment and a 3700‐km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile Pᵢ (mainly Ca‐bound recalcitrant P) to more available forms of Pᵢ (including Al‐ and Fe‐bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect Pₒ. Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg⁻¹, whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg⁻¹ after the 10‐year N addition, associated with an increase in Pᵢ mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile Pᵢ and immobile Pᵢ. Our results provide a new mechanistic understanding of the important role of soil Pᵢ mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. Phosphorus (P) limitation is expected to increase due to nitrogen (N)-induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pi ) and organic matter (Po ). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10-year field N addition experiment and a 3700-km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile Pi (mainly Ca-bound recalcitrant P) to more available forms of Pi (including Al- and Fe-bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect Po . Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg-1 , whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg-1 after the 10-year N addition, associated with an increase in Pi mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile Pi and immobile Pi . Our results provide a new mechanistic understanding of the important role of soil Pi mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run.Phosphorus (P) limitation is expected to increase due to nitrogen (N)-induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pi ) and organic matter (Po ). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10-year field N addition experiment and a 3700-km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile Pi (mainly Ca-bound recalcitrant P) to more available forms of Pi (including Al- and Fe-bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect Po . Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg-1 , whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg-1 after the 10-year N addition, associated with an increase in Pi mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile Pi and immobile Pi . Our results provide a new mechanistic understanding of the important role of soil Pi mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. Phosphorus (P) limitation is expected to increase due to nitrogen (N)‐induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pi) and organic matter (Po). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10‐year field N addition experiment and a 3700‐km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile Pi (mainly Ca‐bound recalcitrant P) to more available forms of Pi (including Al‐ and Fe‐bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect Po. Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg−1, whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg−1 after the 10‐year N addition, associated with an increase in Pi mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile Pi and immobile Pi. Our results provide a new mechanistic understanding of the important role of soil Pi mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. Phosphorus (P) limitation is expected to increase due to nitrogen (N)‐induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pi) and organic matter (Po). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10‐year field N addition experiment and a 3700‐km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile Pi (mainly Ca‐bound recalcitrant P) to more available forms of Pi (including Al‐ and Fe‐bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect Po. Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg−1, whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg−1 after the 10‐year N addition, associated with an increase in Pi mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile Pi and immobile Pi. Our results provide a new mechanistic understanding of the important role of soil Pi mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. Phosphorus (P) limitation is expected to increase due to nitrogen (N)‐induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (P i ) and organic matter (P o ). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10‐year field N addition experiment and a 3700‐km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile P i (mainly Ca‐bound recalcitrant P) to more available forms of P i (including Al‐ and Fe‐bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect P o . Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg −1 , whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg −1 after the 10‐year N addition, associated with an increase in P i mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile P i and immobile P i . Our results provide a new mechanistic understanding of the important role of soil P i mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. Phosphorus (P) limitation is expected to increase due to nitrogen (N)-induced terrestrial eutrophication, although most soils contain large P pools immobilized in minerals (Pi) and organic matter (Pₒ). Here we assessed whether transformations of these P pools could increase plant available pools alleviating P limitation under enhanced N availability. The mechanisms underlying these possible transformations were explored by combining results from a 10-year field N addition experiment and a 3700-km transect covering wide ranges in soil pH, soil N, aridity, leaching, and weathering that could affect soil P status in grasslands. Nitrogen addition promoted the dissolution of immobile Pi (mainly Ca-bound recalcitrant P) to more available forms of Pi (including Al- and Fe-bound P fractions and Olsen P) by decreasing soil pH from 7.6 to 4.7, but did not affect Pₒ. Soil total P declined by 10% from 385 ± 6.8 to 346 ± 9.5 mg kg−1, whereas available P increased by 546% from 3.5 ± 0.3 to 22.6 ± 2.4 mg kg−1 after the 10-year N addition, associated with an increase in Pi mobilization, plant uptake, and leaching. Similar to the N addition experiment, the drop in soil pH from 7.5 to 5.6 and increase in soil N concentration along the grassland transect were associated with an increased ratio between relatively mobile Pi and immobile Pi. Our results provide a new mechanistic understanding of the important role of soil Pi mobilization in maintaining plant P supply and accelerating biogeochemical P cycles under anthropogenic N enrichment. This mobilization process temporarily buffers ecosystem P limitation or even causes P eutrophication, but will extensively deplete soil P pools in the long run. |
| Author | Jiang, Yong Wang, Ruzhen Liu, Heyong Zhang, Yunhai Peñuelas, Josep Wang, Xiaobo Lü, Xiaotao Han, Xingguo Dijkstra, Feike A. Sardans, Jordi Wei, Cunzheng Yang, Junjie |
| Author_xml | – sequence: 1 givenname: Ruzhen surname: Wang fullname: Wang, Ruzhen – sequence: 2 givenname: Junjie surname: Yang fullname: Yang, Junjie – sequence: 3 givenname: Heyong surname: Liu fullname: Liu, Heyong – sequence: 4 givenname: Jordi surname: Sardans fullname: Sardans, Jordi – sequence: 5 givenname: Yunhai surname: Zhang fullname: Zhang, Yunhai – sequence: 6 givenname: Xiaobo surname: Wang fullname: Wang, Xiaobo – sequence: 7 givenname: Cunzheng surname: Wei fullname: Wei, Cunzheng – sequence: 8 givenname: Xiaotao surname: Lü fullname: Lü, Xiaotao – sequence: 9 givenname: Feike A. surname: Dijkstra fullname: Dijkstra, Feike A. – sequence: 10 givenname: Yong surname: Jiang fullname: Jiang, Yong – sequence: 11 givenname: Xingguo surname: Han fullname: Han, Xingguo – sequence: 12 givenname: Josep surname: Peñuelas fullname: Peñuelas, Josep |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/34923633$$D View this record in MEDLINE/PubMed |
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| ContentType | Journal Article |
| Copyright | 2021 The Ecological Society of America 2021 The Ecological Society of America. 2022 Ecological Society of America |
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| ISSN | 0012-9658 1939-9170 |
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| Issue | 3 |
| Keywords | phosphorus mobilization mineral-bound phosphorus phosphorus limitation precipitation gradient nitrogen deposition climosequence |
| Language | English |
| License | 2021 The Ecological Society of America. |
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| Notes | Funding information Ruzhen Wang, Junjie Yang, and Heyong Liu contributed equally to this work. European Research Council Synergy grant, Grant/Award Number: ERC‐SyG‐2013‐610028 IMBALANCE‐P; National Key Research and Development Program of China, Grant/Award Number: 2016YFC0500707; National Natural Science Foundation of China, Grant/Award Numbers: 31430016, 31770525, 31870441; Spanish government grant, Grant/Award Number: PID2019‐110521GB‐I00 Handling Editor Hugh Henry ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
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| PublicationDate | 20220301 March 2022 2022-03-00 |
| PublicationDateYYYYMMDD | 2022-03-01 |
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| PublicationPlace | Hoboken, USA |
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| PublicationTitle | Ecology (Durham) |
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| Publisher | John Wiley and Sons, Inc John Wiley & Sons, Inc Ecological Society of America |
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| Snippet | Phosphorus (P) limitation is expected to increase due to nitrogen (N)-induced terrestrial eutrophication, although most soils contain large P pools immobilized... Phosphorus (P) limitation is expected to increase due to nitrogen (N)‐induced terrestrial eutrophication, although most soils contain large P pools immobilized... |
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| SubjectTerms | Anthropogenic factors Aridity Biogeochemical cycles Buffers climosequence dry environmental conditions Ecosystem ecosystems Eutrophication Fractions Grassland Grasslands Iron Leaching Minerals mineral‐bound phosphorus Nitrogen Nitrogen - analysis nitrogen content nitrogen deposition Nitrogen enrichment Organic matter pH effects Phosphorus phosphorus limitation phosphorus mobilization precipitation gradient Soil Soil chemistry Soil pH Soils |
| Title | Nitrogen enrichment buffers phosphorus limitation by mobilizing mineral-bound soil phosphorus in grasslands |
| URI | https://www.jstor.org/stable/27121091 https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fecy.3616 https://www.ncbi.nlm.nih.gov/pubmed/34923633 https://www.proquest.com/docview/2634391522 https://www.proquest.com/docview/2612037669 https://www.proquest.com/docview/2661033522 |
| Volume | 103 |
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