Title: Microhydrological Niches in Soils: How Mucilage and EPS Alter the Biophysical Properties of the Rhizosphere and Other Biological Hotspots

Abstract

Core Ideas Plant mucilage and bacterial extracellular polymeric substances (EPS) prevent the breakup of the soil liquid phase. Formation of continuous structures buffers soil hydraulic properties. The release of viscous polymeric substances represents a universal strategy. Plant roots and bacteria are capable of buffering erratic fluctuations of water content in their local soil environment by releasing a diverse, highly polymeric blend of substances (e.g. extracellular polymeric substances [EPS] and mucilage). Although this concept is well accepted, the physical mechanisms by which EPS and mucilage interact with the soil matrix and determine the soil water dynamics remain unclear. High‐resolution X‐ray computed tomography revealed that upon drying in porous media, mucilage (from maize [ Zea mays L.] roots) and EPS (from intact biocrusts) form filaments and two‐dimensional interconnected structures spanning across multiple pores. Unlike water, these mucilage and EPS structures connecting soil particles did not break up upon drying, which is explained by the high viscosity and low surface tension of EPS and mucilage. Measurements of water retention and evaporation with soils mixed with seed mucilage show how these one‐ and two‐dimensional pore‐scale structures affect macroscopic hydraulic properties (i.e., they enhance water retention, preserve the continuity of the liquid phase in dryingmore » soils, and decrease vapor diffusivity and local drying rates). In conclusion, we propose that the release of viscous polymeric substances and the consequent creation of a network bridging the soil pore space represent a universal strategy of plants and bacteria to engineer their own soil microhydrological niches where stable conditions for life are preserved.« less

Authors:

Benard, Pascal ^[1]; Zarebanadkouki, Mohsen ^[2]; Brax, Mathilde ^[3]; Kaltenbach, Robin ^[3]; Jerjen, Iwan ^[4]; Marone, Federica ^[4]; Couradeau, Estelle ^[5]; Felde, Vincent J. M. N. L. ^[6]; Kaestner, Anders ^[7]; Carminati, Andrea ^[2]

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+ Show Author Affiliations

1. Faculty for Biology, Chemistry, and Earth Sciences, Chair of Soil Physics Univ. of Bayreuth Universitätsstraße 30, 95447 Bayreuth Bavaria Germany, Faculty of Agricultural Sciences, Group of Soil Hydrology Univ. of Göttingen Büsgenweg 2, 37077 Göttingen Lower Saxony Germany
2. Faculty for Biology, Chemistry, and Earth Sciences, Chair of Soil Physics Univ. of Bayreuth Universitätsstraße 30, 95447 Bayreuth Bavaria Germany
3. Institute for Environmental Sciences Group of Environmental and Soil Chemistry Univ. Koblenz‐Landau Fortstraße 7, 76829 Landau Rhineland‐Palatinate Germany
4. Paul Scherrer Institute Swiss Light Source Forschungsstrasse 111 5232 Villigen Switzerland
5. Arizona State Univ. School of Life Sciences 427 E. Tyler Mall Tempe AZ85281, Lawrence Berkeley National Lab. Environmental Genomics and Systems Biology 1 Cyclotron Rd. Berkeley CA 94720
6. Dep. of Soil Science Univ. of Kassel Mönchebergstraße 19 34125 Witzenhausen Hesse Germany
7. Paul Scherrer Institute Lab. for Neutron Scattering and Imaging Forschungsstrasse 111 5232 Villigen Switzerland

Publication Date:

2019-06-27

Sponsoring Org.:

USDOE

OSTI Identifier:

1602291

Alternate Identifier(s):

OSTI ID: 1604258

Resource Type:

Published Article

Journal Name:

Vadose Zone Journal

Additional Journal Information:

Journal Name: Vadose Zone Journal Journal Volume: 18 Journal Issue: 1; Journal ID: ISSN 1539-1663

Publisher:

Wiley Blackwell (John Wiley & Sons)

Country of Publication:

United States

Language:

English