TY - JOUR

T1 - Multiple exchange processes on mineral surfaces control the transport of dissolved organic matter through soil profiles

AU - Leinemann, T.

AU - Preusser, S.

AU - Mikutta, R.

AU - Kalbitz, K.

AU - Cerli, C.

AU - Höschen, C.

AU - Mueller, C. W.

AU - Kandeler, E.

AU - Guggenberger, G.

N1 - Funding Information: Funding of the research was provided by the Deutsche Forschungsgemeinschaft DFG within the research unit FOR 1806 ‘‘The Forgotten Part of Carbon Cycling: Organic Matter Storage and Turnover in Subsoils (SUBSOM)’’. The funding for NanoSIMS analyses was provided by MU 3021/4-1. We would like to thank Dr. Stefanie Heinze and Prof. Dr. Bernd Marschner for project coordination and Petra Kuner and numerous student helpers for support in the laboratory.

PY - 2018/3

Y1 - 2018/3

N2 - Organic topsoil layers are important sources of dissolved organic matter (DOM) transported to deeper soil layers. During passage through the mineral soil, both organic matter (OM) quality and quantity change markedly. Whether these alterations are due to sorption processes alone or to additional stepwise exchange processes of OM on mineral surfaces (“cascade model”) is not fully understood. To test the “cascade model” we conducted a laboratory flow cascade experiment with undisturbed soil columns from three depths of two different soil profiles (Dystric and Eutric Cambisol) using carbon (C) isotope labelling. Each of the connected topsoil and subsoil columns contained a goethite (α-FeOOH) layer either with or without sorbed 13C-labelled OM to assess the importance of OM immobilization/mobilization reactions with reactive soil minerals. By using a multiple method approach including 13C analysis in the solid and solution phases, nanometer scale secondary ion mass spectrometry (NanoSIMS), and quantitative polymerase chain reaction (qPCR), we quantified organic carbon (OC) adsorption and desorption and net OC exchange at goethite surfaces as well as the associated microbial community patterns at every depth step of the column experiment. The gross OC exchange between OM-coated goethite and the soil solution was in the range of 15–32%. This indicates that a considerable proportion of the mineral associated OM was mobilized and replaced by percolating DOM. We showed that specific groups of bacteria play an important role in processing organic carbon compounds in the mineral micro-environment. Whereas bulk soils were dominated by oligotrophic bacteria such as Acidobacteria, the goethite layers were specifically enriched with copiotrophic bacteria such as Betaproteobacteria. This group of microorganisms made use of labile carbon derived either from direct DOM transport or from OM exchange processes at goethite surfaces. Specific microorganisms appear to contribute to the cascade process of OM transport within soils. Our study confirms the validity of the postulated “cascade model” featuring the stepwise transport of OM within the soil profile.

AB - Organic topsoil layers are important sources of dissolved organic matter (DOM) transported to deeper soil layers. During passage through the mineral soil, both organic matter (OM) quality and quantity change markedly. Whether these alterations are due to sorption processes alone or to additional stepwise exchange processes of OM on mineral surfaces (“cascade model”) is not fully understood. To test the “cascade model” we conducted a laboratory flow cascade experiment with undisturbed soil columns from three depths of two different soil profiles (Dystric and Eutric Cambisol) using carbon (C) isotope labelling. Each of the connected topsoil and subsoil columns contained a goethite (α-FeOOH) layer either with or without sorbed 13C-labelled OM to assess the importance of OM immobilization/mobilization reactions with reactive soil minerals. By using a multiple method approach including 13C analysis in the solid and solution phases, nanometer scale secondary ion mass spectrometry (NanoSIMS), and quantitative polymerase chain reaction (qPCR), we quantified organic carbon (OC) adsorption and desorption and net OC exchange at goethite surfaces as well as the associated microbial community patterns at every depth step of the column experiment. The gross OC exchange between OM-coated goethite and the soil solution was in the range of 15–32%. This indicates that a considerable proportion of the mineral associated OM was mobilized and replaced by percolating DOM. We showed that specific groups of bacteria play an important role in processing organic carbon compounds in the mineral micro-environment. Whereas bulk soils were dominated by oligotrophic bacteria such as Acidobacteria, the goethite layers were specifically enriched with copiotrophic bacteria such as Betaproteobacteria. This group of microorganisms made use of labile carbon derived either from direct DOM transport or from OM exchange processes at goethite surfaces. Specific microorganisms appear to contribute to the cascade process of OM transport within soils. Our study confirms the validity of the postulated “cascade model” featuring the stepwise transport of OM within the soil profile.

KW - C

KW - Cascade model

KW - DOM

KW - Microbial community composition

KW - NanoSIMS

KW - Reactive minerals

UR - http://www.scopus.com/inward/record.url?scp=85038076458&partnerID=8YFLogxK

U2 - 10.1016/j.soilbio.2017.12.006

DO - 10.1016/j.soilbio.2017.12.006

M3 - Article

AN - SCOPUS:85038076458

VL - 118

SP - 79

EP - 90

JO - Soil Biology and Biochemistry

JF - Soil Biology and Biochemistry

SN - 0038-0717

ER -