Reverse microdialysis: A window into root exudation hotspots
Plant roots release a variety of low-molecular weight compounds, such as sugars, amino acids or organic acids into the soil, impacting microbial activities and physico-chemical soil processes in their surroundings. These compounds are a source of easily available Carbon (C) and energy for soil micro...
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description | Plant roots release a variety of low-molecular weight compounds, such as sugars, amino acids or organic acids into the soil, impacting microbial activities and physico-chemical soil processes in their surroundings. These compounds are a source of easily available Carbon (C) and energy for soil microbes, potentially accelerating microbial decomposition of soil organic matter in the immediate vicinity of roots. However, knowledge about processes in root exudation hotspots remains limited due to experimental difficulties in investigating such hotspots in soil.
Microdialysis, a passive sampling technique based on diffusion, has been successfully used to collect soil solutes at small spatial scales. Reverse microdialysis, also termed retrodialysis, can be used to introduce solutes into the soil, mimicking passive root exudation. However, little is known about the dynamics of substances released by passive diffusion into intact soil, a crucial prerequisite for applying reverse microdialysis to study root exudation hotspots in undisturbed soils.
Here, we used reverse microdialysis to investigate the spatial and temporal dynamics of thirteen different organic compounds passively introduced into two different intact soils. Diffusion of compounds into soils was substantially lower than into water, and was not – as in water – determined by molecular size. Interestingly, butyrate, oxalate and propionate showed the highest diffusive fluxes into soil combined with the lowest rate of back retrieval after input, indicating that they were quickly removed from the soil solution by biotic or abiotic processes. In contrast, glucose and fructose unexpectedly accumulated around the membrane after input without removal. Furthermore, diffusive fluxes of compounds into soils showed a fluctuating temporal pattern, which may be explained by an observed 2-h delay of microbial respiration of added 13C-labelled compounds. During the course of 12 days, approximately one third of 13C-labelled compounds introduced into soil was respired while 8% ended up in microbial biomass.
Our results demonstrate that introducing compounds into intact soil triggers complex biotic and abiotic responses at the time scale of hours. Reverse microdialysis proved to be an excellent tool to investigate such responses as well as the dynamics and metabolic consequences of passively released compounds into intact soil, and – in combination with 13C labelled substrate and respiration measurements - to shed light |
doi_str_mv | 10.1016/j.soilbio.2022.108829 |
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Microdialysis, a passive sampling technique based on diffusion, has been successfully used to collect soil solutes at small spatial scales. Reverse microdialysis, also termed retrodialysis, can be used to introduce solutes into the soil, mimicking passive root exudation. However, little is known about the dynamics of substances released by passive diffusion into intact soil, a crucial prerequisite for applying reverse microdialysis to study root exudation hotspots in undisturbed soils.
Here, we used reverse microdialysis to investigate the spatial and temporal dynamics of thirteen different organic compounds passively introduced into two different intact soils. Diffusion of compounds into soils was substantially lower than into water, and was not – as in water – determined by molecular size. Interestingly, butyrate, oxalate and propionate showed the highest diffusive fluxes into soil combined with the lowest rate of back retrieval after input, indicating that they were quickly removed from the soil solution by biotic or abiotic processes. In contrast, glucose and fructose unexpectedly accumulated around the membrane after input without removal. Furthermore, diffusive fluxes of compounds into soils showed a fluctuating temporal pattern, which may be explained by an observed 2-h delay of microbial respiration of added 13C-labelled compounds. During the course of 12 days, approximately one third of 13C-labelled compounds introduced into soil was respired while 8% ended up in microbial biomass.
Our results demonstrate that introducing compounds into intact soil triggers complex biotic and abiotic responses at the time scale of hours. Reverse microdialysis proved to be an excellent tool to investigate such responses as well as the dynamics and metabolic consequences of passively released compounds into intact soil, and – in combination with 13C labelled substrate and respiration measurements - to shed light on potential priming effects that may be triggered by them.
•We evaluated reverse microdialysis as a tool to simulate passive root exudation.•Release of compounds differs between soils, and is slower into soil than into water.•Diffusion of compounds into soil show a fluctuating temporal pattern.•In contrast to organic acids, sugars accumulated around the membrane in the soil.•Within 11 days–40% of introduced C was respired, and ∼8% ended up in microbial biomass.</description><identifier>ISSN: 0038-0717</identifier><identifier>EISSN: 1879-3428</identifier><identifier>DOI: 10.1016/j.soilbio.2022.108829</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>biodegradation ; butyrates ; energy ; exudation ; fructose ; glucose ; microbial biomass ; microdialysis ; molecular weight ; oxalates ; Priming effect ; propionic acid ; Reverse microdialysis ; Rhizosphere ; Root exudation ; soil ; Soil microscale ; soil organic matter ; soil solution ; temporal variation</subject><ispartof>Soil biology & biochemistry, 2022-11, Vol.174, p.108829, Article 108829</ispartof><rights>2022 The Author(s)</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-f6dd0aa80950b491bf052e5ffdb84bb033b805e1a27260722ad93af8b5b339163</citedby><cites>FETCH-LOGICAL-c319t-f6dd0aa80950b491bf052e5ffdb84bb033b805e1a27260722ad93af8b5b339163</cites><orcidid>0000-0002-1617-9186 ; 0000-0002-0539-8842 ; 0000-0003-2046-7567 ; 0000-0001-5181-1581 ; 0000-0002-2005-1820 ; 0000-0001-5490-8768</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0038071722002863$$EHTML$$P50$$Gelsevier$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids></links><search><creatorcontrib>König, Alexander</creatorcontrib><creatorcontrib>Wiesenbauer, Julia</creatorcontrib><creatorcontrib>Gorka, Stefan</creatorcontrib><creatorcontrib>Marchand, Lilian</creatorcontrib><creatorcontrib>Kitzler, Barbara</creatorcontrib><creatorcontrib>Inselsbacher, Erich</creatorcontrib><creatorcontrib>Kaiser, Christina</creatorcontrib><title>Reverse microdialysis: A window into root exudation hotspots</title><title>Soil biology & biochemistry</title><description>Plant roots release a variety of low-molecular weight compounds, such as sugars, amino acids or organic acids into the soil, impacting microbial activities and physico-chemical soil processes in their surroundings. These compounds are a source of easily available Carbon (C) and energy for soil microbes, potentially accelerating microbial decomposition of soil organic matter in the immediate vicinity of roots. However, knowledge about processes in root exudation hotspots remains limited due to experimental difficulties in investigating such hotspots in soil.
Microdialysis, a passive sampling technique based on diffusion, has been successfully used to collect soil solutes at small spatial scales. Reverse microdialysis, also termed retrodialysis, can be used to introduce solutes into the soil, mimicking passive root exudation. However, little is known about the dynamics of substances released by passive diffusion into intact soil, a crucial prerequisite for applying reverse microdialysis to study root exudation hotspots in undisturbed soils.
Here, we used reverse microdialysis to investigate the spatial and temporal dynamics of thirteen different organic compounds passively introduced into two different intact soils. Diffusion of compounds into soils was substantially lower than into water, and was not – as in water – determined by molecular size. Interestingly, butyrate, oxalate and propionate showed the highest diffusive fluxes into soil combined with the lowest rate of back retrieval after input, indicating that they were quickly removed from the soil solution by biotic or abiotic processes. In contrast, glucose and fructose unexpectedly accumulated around the membrane after input without removal. Furthermore, diffusive fluxes of compounds into soils showed a fluctuating temporal pattern, which may be explained by an observed 2-h delay of microbial respiration of added 13C-labelled compounds. During the course of 12 days, approximately one third of 13C-labelled compounds introduced into soil was respired while 8% ended up in microbial biomass.
Our results demonstrate that introducing compounds into intact soil triggers complex biotic and abiotic responses at the time scale of hours. Reverse microdialysis proved to be an excellent tool to investigate such responses as well as the dynamics and metabolic consequences of passively released compounds into intact soil, and – in combination with 13C labelled substrate and respiration measurements - to shed light on potential priming effects that may be triggered by them.
•We evaluated reverse microdialysis as a tool to simulate passive root exudation.•Release of compounds differs between soils, and is slower into soil than into water.•Diffusion of compounds into soil show a fluctuating temporal pattern.•In contrast to organic acids, sugars accumulated around the membrane in the soil.•Within 11 days–40% of introduced C was respired, and ∼8% ended up in microbial biomass.</description><subject>biodegradation</subject><subject>butyrates</subject><subject>energy</subject><subject>exudation</subject><subject>fructose</subject><subject>glucose</subject><subject>microbial biomass</subject><subject>microdialysis</subject><subject>molecular weight</subject><subject>oxalates</subject><subject>Priming effect</subject><subject>propionic acid</subject><subject>Reverse microdialysis</subject><subject>Rhizosphere</subject><subject>Root exudation</subject><subject>soil</subject><subject>Soil microscale</subject><subject>soil organic matter</subject><subject>soil solution</subject><subject>temporal variation</subject><issn>0038-0717</issn><issn>1879-3428</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNqFkF9LwzAUxYMoOKcfQeijL503ydomIsgY8w8MBNHnkDS3mNE1M-k29-3N6N59uBy4nHPg_Ai5pTChQMv71SR61xrnJwwYSz8hmDwjIyoqmfMpE-dkBMBFDhWtLslVjCsAYAXlI_L4gTsMEbO1q4O3TreH6OJDNsv2rrN-n7mu91nwvs_wd2t173yXffs-btJdk4tGtxFvTjomX8-Lz_lrvnx_eZvPlnnNqezzprQWtBYgCzBTSU0DBcOiaawRU2OAcyOgQKpZxUqoGNNWct0IUxjOJS35mNwNvZvgf7YYe7V2sca21R36bVQpxxOJispkLQZrWhNjwEZtglvrcFAU1JGWWqkTLXWkpQZaKfc05DDt2DkMKtYOuxqtC1j3ynr3T8MfDoN1xA</recordid><startdate>202211</startdate><enddate>202211</enddate><creator>König, Alexander</creator><creator>Wiesenbauer, Julia</creator><creator>Gorka, Stefan</creator><creator>Marchand, Lilian</creator><creator>Kitzler, Barbara</creator><creator>Inselsbacher, Erich</creator><creator>Kaiser, Christina</creator><general>Elsevier Ltd</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7S9</scope><scope>L.6</scope><orcidid>https://orcid.org/0000-0002-1617-9186</orcidid><orcidid>https://orcid.org/0000-0002-0539-8842</orcidid><orcidid>https://orcid.org/0000-0003-2046-7567</orcidid><orcidid>https://orcid.org/0000-0001-5181-1581</orcidid><orcidid>https://orcid.org/0000-0002-2005-1820</orcidid><orcidid>https://orcid.org/0000-0001-5490-8768</orcidid></search><sort><creationdate>202211</creationdate><title>Reverse microdialysis: A window into root exudation hotspots</title><author>König, Alexander ; Wiesenbauer, Julia ; Gorka, Stefan ; Marchand, Lilian ; Kitzler, Barbara ; Inselsbacher, Erich ; Kaiser, Christina</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-f6dd0aa80950b491bf052e5ffdb84bb033b805e1a27260722ad93af8b5b339163</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>biodegradation</topic><topic>butyrates</topic><topic>energy</topic><topic>exudation</topic><topic>fructose</topic><topic>glucose</topic><topic>microbial biomass</topic><topic>microdialysis</topic><topic>molecular weight</topic><topic>oxalates</topic><topic>Priming effect</topic><topic>propionic acid</topic><topic>Reverse microdialysis</topic><topic>Rhizosphere</topic><topic>Root exudation</topic><topic>soil</topic><topic>Soil microscale</topic><topic>soil organic matter</topic><topic>soil solution</topic><topic>temporal variation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>König, Alexander</creatorcontrib><creatorcontrib>Wiesenbauer, Julia</creatorcontrib><creatorcontrib>Gorka, Stefan</creatorcontrib><creatorcontrib>Marchand, Lilian</creatorcontrib><creatorcontrib>Kitzler, Barbara</creatorcontrib><creatorcontrib>Inselsbacher, Erich</creatorcontrib><creatorcontrib>Kaiser, Christina</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>CrossRef</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><jtitle>Soil biology & biochemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>König, Alexander</au><au>Wiesenbauer, Julia</au><au>Gorka, Stefan</au><au>Marchand, Lilian</au><au>Kitzler, Barbara</au><au>Inselsbacher, Erich</au><au>Kaiser, Christina</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Reverse microdialysis: A window into root exudation hotspots</atitle><jtitle>Soil biology & biochemistry</jtitle><date>2022-11</date><risdate>2022</risdate><volume>174</volume><spage>108829</spage><pages>108829-</pages><artnum>108829</artnum><issn>0038-0717</issn><eissn>1879-3428</eissn><abstract>Plant roots release a variety of low-molecular weight compounds, such as sugars, amino acids or organic acids into the soil, impacting microbial activities and physico-chemical soil processes in their surroundings. These compounds are a source of easily available Carbon (C) and energy for soil microbes, potentially accelerating microbial decomposition of soil organic matter in the immediate vicinity of roots. However, knowledge about processes in root exudation hotspots remains limited due to experimental difficulties in investigating such hotspots in soil.
Microdialysis, a passive sampling technique based on diffusion, has been successfully used to collect soil solutes at small spatial scales. Reverse microdialysis, also termed retrodialysis, can be used to introduce solutes into the soil, mimicking passive root exudation. However, little is known about the dynamics of substances released by passive diffusion into intact soil, a crucial prerequisite for applying reverse microdialysis to study root exudation hotspots in undisturbed soils.
Here, we used reverse microdialysis to investigate the spatial and temporal dynamics of thirteen different organic compounds passively introduced into two different intact soils. Diffusion of compounds into soils was substantially lower than into water, and was not – as in water – determined by molecular size. Interestingly, butyrate, oxalate and propionate showed the highest diffusive fluxes into soil combined with the lowest rate of back retrieval after input, indicating that they were quickly removed from the soil solution by biotic or abiotic processes. In contrast, glucose and fructose unexpectedly accumulated around the membrane after input without removal. Furthermore, diffusive fluxes of compounds into soils showed a fluctuating temporal pattern, which may be explained by an observed 2-h delay of microbial respiration of added 13C-labelled compounds. During the course of 12 days, approximately one third of 13C-labelled compounds introduced into soil was respired while 8% ended up in microbial biomass.
Our results demonstrate that introducing compounds into intact soil triggers complex biotic and abiotic responses at the time scale of hours. Reverse microdialysis proved to be an excellent tool to investigate such responses as well as the dynamics and metabolic consequences of passively released compounds into intact soil, and – in combination with 13C labelled substrate and respiration measurements - to shed light on potential priming effects that may be triggered by them.
•We evaluated reverse microdialysis as a tool to simulate passive root exudation.•Release of compounds differs between soils, and is slower into soil than into water.•Diffusion of compounds into soil show a fluctuating temporal pattern.•In contrast to organic acids, sugars accumulated around the membrane in the soil.•Within 11 days–40% of introduced C was respired, and ∼8% ended up in microbial biomass.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.soilbio.2022.108829</doi><orcidid>https://orcid.org/0000-0002-1617-9186</orcidid><orcidid>https://orcid.org/0000-0002-0539-8842</orcidid><orcidid>https://orcid.org/0000-0003-2046-7567</orcidid><orcidid>https://orcid.org/0000-0001-5181-1581</orcidid><orcidid>https://orcid.org/0000-0002-2005-1820</orcidid><orcidid>https://orcid.org/0000-0001-5490-8768</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | biodegradation butyrates energy exudation fructose glucose microbial biomass microdialysis molecular weight oxalates Priming effect propionic acid Reverse microdialysis Rhizosphere Root exudation soil Soil microscale soil organic matter soil solution temporal variation |
title | Reverse microdialysis: A window into root exudation hotspots |
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