Organic Acids Regulation of Chemical–Microbial Phosphorus Transformations in Soils
We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantl...
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| Published in | Environmental science & technology Vol. 50; no. 21; pp. 11521 - 11531 |
|---|---|
| Main Authors | , , , , , , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
United States
American Chemical Society
01.11.2016
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| Subjects | |
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| Abstract | We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg–1. However, low organic acid doses (<2 mmol kg–1) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (K d) and desorption rate constants (k –1) decreased whereas an increase in the response time of solution P equilibration (T c) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical–microbial soil phosphorus transformations. |
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| AbstractList | We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg^sup -1^. However, low organic acid doses (<2 mmol kg^sup -1^) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (K^sub d^) and desorption rate constants (k^sub -1^) decreased whereas an increase in the response time of solution P equilibration (T^sub c^) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical-microbial soil phosphorus transformations. We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg super( -1). However, low organic acid doses (<2 mmol kg super( -1)) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (K sub( d)) and desorption rate constants (k sub( -1)) decreased whereas an increase in the response time of solution P equilibration (T sub( c)) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical-microbial soil phosphorus transformations. We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg–¹. However, low organic acid doses (<2 mmol kg–¹) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (Kd) and desorption rate constants (k–₁) decreased whereas an increase in the response time of solution P equilibration (Tc) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical–microbial soil phosphorus transformations. We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg–1. However, low organic acid doses (<2 mmol kg–1) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (K d) and desorption rate constants (k –1) decreased whereas an increase in the response time of solution P equilibration (T c) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical–microbial soil phosphorus transformations. We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg-1. However, low organic acid doses (<2 mmol kg-1) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (Kd) and desorption rate constants (k-1) decreased whereas an increase in the response time of solution P equilibration (Tc) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical-microbial soil phosphorus transformations.We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg-1. However, low organic acid doses (<2 mmol kg-1) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (Kd) and desorption rate constants (k-1) decreased whereas an increase in the response time of solution P equilibration (Tc) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical-microbial soil phosphorus transformations. We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration at increasing doses of citric and oxalic acid in two different soils with contrasting agronomic P status. Citric or oxalic acids significantly increased soil solution P concentrations for doses over 2 mmol kg . However, low organic acid doses (<2 mmol kg ) were associated with a steep increase in microbial biomass P, which was not seen for higher doses. In both soils, treatment with the tribasic citric acid led to a greater increase in soil solution P than the dibasic oxalic acid, likely due to the rapid degrading of oxalic acids in soils. After equilibration of soils with citric or oxalic acids, the adsorbed-to-solution distribution coefficient (K ) and desorption rate constants (k ) decreased whereas an increase in the response time of solution P equilibration (T ) was observed. The extent of this effect was shown to be both soil and organic acid specific. Our results illustrate the critical thresholds of organic acid concentration necessary to mobilize sorbed and precipitated P, bringing new insight on how the exudation of organic acids regulate chemical-microbial soil phosphorus transformations. |
| Author | George, Timothy S Cooper, Patricia Brown, Lawrie Haygarth, Philip M Giles, Courtney D Paredes, Cecilia Blackwell, Martin Zhang, Hao Darch, Tegan Wearing, Catherine Shand, Charles Stutter, Marc Menezes-Blackburn, Daniel Lumsdon, David Wendler, Renate |
| AuthorAffiliation | Scientific and Technological Bioresource Nucleus (BIOREN) James Hutton Institute The James Hutton Institute Lancaster Environment Centre Universidad de La Frontera Lancaster University |
| AuthorAffiliation_xml | – name: Scientific and Technological Bioresource Nucleus (BIOREN) – name: James Hutton Institute – name: Lancaster Environment Centre – name: Lancaster University – name: Universidad de La Frontera – name: The James Hutton Institute |
| Author_xml | – sequence: 1 givenname: Daniel surname: Menezes-Blackburn fullname: Menezes-Blackburn, Daniel email: d.blackburn@lancaster.ac.uk – sequence: 2 givenname: Cecilia surname: Paredes fullname: Paredes, Cecilia – sequence: 3 givenname: Hao surname: Zhang fullname: Zhang, Hao email: h.zhang@lancaster.ac.uk – sequence: 4 givenname: Courtney D surname: Giles fullname: Giles, Courtney D – sequence: 5 givenname: Tegan surname: Darch fullname: Darch, Tegan – sequence: 6 givenname: Marc surname: Stutter fullname: Stutter, Marc – sequence: 7 givenname: Timothy S surname: George fullname: George, Timothy S – sequence: 8 givenname: Charles surname: Shand fullname: Shand, Charles – sequence: 9 givenname: David surname: Lumsdon fullname: Lumsdon, David – sequence: 10 givenname: Patricia surname: Cooper fullname: Cooper, Patricia – sequence: 11 givenname: Renate surname: Wendler fullname: Wendler, Renate – sequence: 12 givenname: Lawrie surname: Brown fullname: Brown, Lawrie – sequence: 13 givenname: Martin surname: Blackwell fullname: Blackwell, Martin – sequence: 14 givenname: Catherine surname: Wearing fullname: Wearing, Catherine – sequence: 15 givenname: Philip M surname: Haygarth fullname: Haygarth, Philip M |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/27700099$$D View this record in MEDLINE/PubMed |
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| References_xml | – volume: 8 start-page: 233 issue: 3 year: 2008 ident: ref9/cit9 publication-title: J. Soil Sci. Plant Nutr. – ident: ref12/cit12 doi: 10.1002/jpln.201500047 – ident: ref6/cit6 doi: 10.1104/pp.112.207142 – ident: ref23/cit23 doi: 10.1021/es9704388 – ident: ref28/cit28 doi: 10.1016/0038-0717(89)90157-0 – ident: ref13/cit13 doi: 10.1021/acs.est.5b05395 – ident: ref27/cit27 doi: 10.1128/AEM.69.6.3593-3599.2003 – ident: ref31/cit31 doi: 10.1371/journal.pone.0055731 – ident: ref41/cit41 doi: 10.1111/j.1365-3040.1989.tb01942.x – ident: ref30/cit30 doi: 10.2136/sssaj1982.03615995004600050017x – ident: ref1/cit1 doi: 10.1046/j.1469-8137.2003.00695.x – ident: ref14/cit14 doi: 10.1023/A:1022304332313 – ident: ref5/cit5 doi: 10.1038/74531 – ident: ref25/cit25 doi: 10.1016/j.geoderma.2015.03.020 – ident: ref15/cit15 doi: 10.1071/EN09010 – ident: ref19/cit19 doi: 10.1016/S0016-7037(98)00186-0 – ident: ref11/cit11 doi: 10.1097/SS.0b013e318272f83f – ident: ref18/cit18 doi: 10.1021/ac101450j – ident: ref36/cit36 doi: 10.1002/jpln.19941570104 – ident: ref26/cit26 doi: 10.1016/0038-0717(86)90050-7 – ident: ref2/cit2 doi: 10.1023/A:1013351617532 – ident: ref40/cit40 doi: 10.1007/s11104-013-1594-3 – ident: ref10/cit10 doi: 10.1002/(SICI)1522-2624(200004)163:2<207::AID-JPLN207>3.0.CO;2-P – ident: ref20/cit20 doi: 10.1021/ac00115a005 – ident: ref7/cit7 doi: 10.1111/ppl.12150 – ident: ref35/cit35 doi: 10.1080/00103620600623558 – start-page: 20 year: 2000 ident: ref24/cit24 publication-title: Methods of Phosphorus Analysis for Soils, Sediments, Residuals, and Waters – ident: ref39/cit39 doi: 10.1016/j.envexpbot.2010.08.010 – ident: ref16/cit16 doi: 10.1016/S0003-2670(00)88444-5 – ident: ref21/cit21 doi: 10.1021/es0352597 – ident: ref32/cit32 doi: 10.1104/pp.109.147462 – ident: ref8/cit8 doi: 10.1016/j.soilbio.2015.02.019 – ident: ref29/cit29 doi: 10.1186/1472-6750-10-2 – ident: ref17/cit17 doi: 10.1021/ac00115a005 – ident: ref34/cit34 doi: 10.1007/BF00570634 – ident: ref33/cit33 doi: 10.1074/jbc.M112.433300 – ident: ref3/cit3 doi: 10.1023/A:1004356007312 – ident: ref22/cit22 doi: 10.1016/S1364-8152(99)00027-4 – volume: 1 start-page: 19 volume-title: Soil Fertility Improvement and Integrated Nutrient Management: A Global Perspective year: 2011 ident: ref37/cit37 – ident: ref4/cit4 doi: 10.1071/CP07125 – ident: ref38/cit38 doi: 10.1094/MPMI-19-0250 |
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| Snippet | We have used an integrated approach to study the mobility of inorganic phosphorus (P) from soil solid phase as well as the microbial biomass P and respiration... |
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| SubjectTerms | Acids Biomass citric acid Desorption exudation inorganic phosphorus Integrated approach microbial biomass Organic Chemicals oxalic acid Phosphorus Soil Soil microorganisms Soil Pollutants soil solution |
| Title | Organic Acids Regulation of Chemical–Microbial Phosphorus Transformations in Soils |
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