Quantitative soil zymography: Mechanisms, processes of substrate and enzyme diffusion in porous media

Research output: Contribution to journalArticleResearchpeer review

Authors

  • Andrey Guber
  • Alexandra Kraychenko
  • Bahar S. Razavi
  • Daniel Uteau
  • Stephan Peth
  • Evgenia Blagodatskaya
  • Yakov Kuzyakov

External Research Organisations

  • Michigan State University (MSU)
  • University of Göttingen
  • Kiel University
  • University of Kassel
  • Institute of Physicochemical and Biological Problems in Soil Science
  • Peoples' Friendship University of Russia (RUDN)
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Details

Original languageEnglish
Pages (from-to)156-167
Number of pages12
JournalSoil biology & biochemistry
Volume127
Early online date28 Sept 2018
Publication statusPublished - Dec 2018
Externally publishedYes

Abstract

Soil membrane zymography enables 2D mapping of enzyme activities on the surface of soil samples. The method is based on diffusion of components of enzymatically-mediated reactions to/from membrane, and, thus, reflects the distribution of enzyme activities at the intact soil surface. Zymography has been already successfully implemented in numerous soil ecology applications. Here we identify two methodological aspects for further improvement and expansion of the method at micro and macro scales: first, accounting for the area of contact between the soil surface and the zymography membranes and, second, accounting for diffusion effects during the zymography procedure. We tested three methods, namely, laser-scanning, staining with a fluorescent product (e.g. MUF: 4-methylumbelliferone), and X-ray computed micro-tomography, for assessing the area of the soil surface in contact with the membranes. We quantified diffusion of MUF, enzymes and substrate between the substrate-saturated membrane and soil as well as diffusion processes during membrane zymography via HP2 software. Diffusion of the substrate from the membrane and of the MUF-product to the membrane was detected, while there were no clear evidence of enzyme diffusion to/in the membrane. According to the model simulations, the enzyme activities detected via 2D zymography probably represent only a small portion, about 20%, of the actual reactions within the soil volume that is in both direct contact and in hydrological contact with zymography membranes. This is a result of omnidirectional diffusion of reaction products. The membrane contact with the soil surface estimated by three methods ranged from 3.4 to 36.5% further signifying that only a fraction of enzymes activity is detectable in a course of 2D soil zymography.

Keywords

    In situ 2D zymography, Soil enzyme activity, Microbial hotspot's localization, Diffusion processes

ASJC Scopus subject areas

Cite this

Quantitative soil zymography: Mechanisms, processes of substrate and enzyme diffusion in porous media. / Guber, Andrey; Kraychenko, Alexandra; Razavi, Bahar S. et al.
In: Soil biology & biochemistry, Vol. 127, 12.2018, p. 156-167.

Research output: Contribution to journalArticleResearchpeer review

Guber A, Kraychenko A, Razavi BS, Uteau D, Peth S, Blagodatskaya E et al. Quantitative soil zymography: Mechanisms, processes of substrate and enzyme diffusion in porous media. Soil biology & biochemistry. 2018 Dec;127:156-167. Epub 2018 Sept 28. doi: 10.1016/j.soilbio.2018.09.030
Guber, Andrey ; Kraychenko, Alexandra ; Razavi, Bahar S. et al. / Quantitative soil zymography : Mechanisms, processes of substrate and enzyme diffusion in porous media. In: Soil biology & biochemistry. 2018 ; Vol. 127. pp. 156-167.
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abstract = "Soil membrane zymography enables 2D mapping of enzyme activities on the surface of soil samples. The method is based on diffusion of components of enzymatically-mediated reactions to/from membrane, and, thus, reflects the distribution of enzyme activities at the intact soil surface. Zymography has been already successfully implemented in numerous soil ecology applications. Here we identify two methodological aspects for further improvement and expansion of the method at micro and macro scales: first, accounting for the area of contact between the soil surface and the zymography membranes and, second, accounting for diffusion effects during the zymography procedure. We tested three methods, namely, laser-scanning, staining with a fluorescent product (e.g. MUF: 4-methylumbelliferone), and X-ray computed micro-tomography, for assessing the area of the soil surface in contact with the membranes. We quantified diffusion of MUF, enzymes and substrate between the substrate-saturated membrane and soil as well as diffusion processes during membrane zymography via HP2 software. Diffusion of the substrate from the membrane and of the MUF-product to the membrane was detected, while there were no clear evidence of enzyme diffusion to/in the membrane. According to the model simulations, the enzyme activities detected via 2D zymography probably represent only a small portion, about 20%, of the actual reactions within the soil volume that is in both direct contact and in hydrological contact with zymography membranes. This is a result of omnidirectional diffusion of reaction products. The membrane contact with the soil surface estimated by three methods ranged from 3.4 to 36.5% further signifying that only a fraction of enzymes activity is detectable in a course of 2D soil zymography.",
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note = "Funding Information: This research was partly funded by the National Science Foundation's Long-Term Ecological Research Program (DEB 1027253), by the National Science Foundation's Geobiology and Low Temperature Geochemistry Program (Award no. 1630399), by the Department of Energy Great Lakes Bioenergy Research Center (DOE O_ce of Science BER DE-FC02-07ER64494), by Michigan State University's AgBioResearch (Project GREEEN), and by Michigan State University's Discretionary Funding Initiative. The work was supported by DAAD- German Academic Exchange Service{\textquoteright} program “Research Stays for University Academics and Scientists, 2017” (57314018) and by the Research Award from Alexander von Humboldt Foundation. Contributions of BSR and EB were motivated and supported within the framework of the priority program 2089, funded by the DFG- Projects Nr. 403670038 and Nr. 403664478, respectively. This work has also been conducted in part as a preparatory study for the recently launched DFG priority program 2089 Rhizosphere spatiotemporal organization—a key to rhizosphere functions PE 1523/10–1. ",
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T1 - Quantitative soil zymography

T2 - Mechanisms, processes of substrate and enzyme diffusion in porous media

AU - Guber, Andrey

AU - Kraychenko, Alexandra

AU - Razavi, Bahar S.

AU - Uteau, Daniel

AU - Peth, Stephan

AU - Blagodatskaya, Evgenia

AU - Kuzyakov, Yakov

N1 - Funding Information: This research was partly funded by the National Science Foundation's Long-Term Ecological Research Program (DEB 1027253), by the National Science Foundation's Geobiology and Low Temperature Geochemistry Program (Award no. 1630399), by the Department of Energy Great Lakes Bioenergy Research Center (DOE O_ce of Science BER DE-FC02-07ER64494), by Michigan State University's AgBioResearch (Project GREEEN), and by Michigan State University's Discretionary Funding Initiative. The work was supported by DAAD- German Academic Exchange Service’ program “Research Stays for University Academics and Scientists, 2017” (57314018) and by the Research Award from Alexander von Humboldt Foundation. Contributions of BSR and EB were motivated and supported within the framework of the priority program 2089, funded by the DFG- Projects Nr. 403670038 and Nr. 403664478, respectively. This work has also been conducted in part as a preparatory study for the recently launched DFG priority program 2089 Rhizosphere spatiotemporal organization—a key to rhizosphere functions PE 1523/10–1.

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