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APPENDIX A: SUPPLEMENTARY DATA Selective transport and retention of organic matter and bacteria shapes initial pedogenesis in artificial soil - A two-layer column study KATHARINA LEHMANN a* , SABINE SCHAEFER a , DOREEN BABIN b , JOHN MAXIMILIAN KÖHNE c , STEFFEN SCHLÜTER c , KORNELIA SMALLA b , HANS-JÖRG VOGEL c , AND KAI UWE TOTSCHE a a Friedrich Schiller University Jena, Institute of Geosciences, Department of Hydrogeology, Burgweg 11, D-07749 Jena, Germany b Julius Kühn-Institut -Federal Research Centre for Cultivated Plants (JKI), Institute for Epidemiology and Pathogen Diagnostics, Messeweg 11-12, D-38104 Braunschweig, Germany c Helmholtz Centre for Environmental Research - UFZ Halle, Department of Soil System Sciences, Theodor-Lieser-Strasse 4, D-06120 Halle, Germany E-mail addresses: a : [email protected], [email protected] b : [email protected], [email protected] c : [email protected], steff[email protected], [email protected] *Corresponding Author: Katharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of Hydrogeology, Burgweg 11, D-07749 Jena, Germany

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Page 1: ars.els-cdn.com€¦ · Web viewKatharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of. Hydrogeology, Burgweg 11, D-07749 Jena, Germany

APPENDIX A: SUPPLEMENTARY DATA

Selective transport and retention of organic matter and bacteria shapes

initial pedogenesis in artificial soil - A two-layer column study

KATHARINA LEHMANNa*, SABINE SCHAEFERa, DOREEN BABINb, JOHN MAXIMILIAN KÖHNEc, STEFFEN

SCHLÜTER c, KORNELIA SMALLAb, HANS-JÖRG VOGEL c, AND KAI UWE TOTSCHEa

a Friedrich Schiller University Jena, Institute of Geosciences, Department of Hydrogeology, Burgweg 11, D-

07749 Jena, Germany

b Julius Kühn-Institut -Federal Research Centre for Cultivated Plants (JKI), Institute for Epidemiology and

Pathogen Diagnostics, Messeweg 11-12, D-38104 Braunschweig, Germany

c Helmholtz Centre for Environmental Research - UFZ Halle, Department of Soil System Sciences, Theodor-

Lieser-Strasse 4, D-06120 Halle, Germany

E-mail addresses:

a: [email protected], [email protected]

b: [email protected], [email protected]

c: [email protected], [email protected], [email protected]

*Corresponding Author:

Katharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of

Hydrogeology, Burgweg 11, D-07749 Jena, Germany

E-Mail address: [email protected]

Page 2: ars.els-cdn.com€¦ · Web viewKatharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of. Hydrogeology, Burgweg 11, D-07749 Jena, Germany

Tables: Supplementary data

Table S1. Flow scheme separated into the single flow phases and flow interruptions (FI)

including cumulated time intervals, mean cumulative pore volume (PV), mean effective pore

water velocity, and the mean water content.

PhasesCum. time

intervalMean

cum. PV

Mean effective pore water

velocityMean water

content[d]  [-] [cm min-]1 [-]

flow phase 1 3.4 1.1 0.003 0.47FI-1 10.2flow phase 2 15.3 1.9 0.002 0.48FI-2 32.2flow phase 3 48.2 3.6 0.002 0.40FI-3 65.1flow phase 4 75.2 4.5 0.001 0.39

Page 3: ars.els-cdn.com€¦ · Web viewKatharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of. Hydrogeology, Burgweg 11, D-07749 Jena, Germany

Table S2. Calculation of the bacterial contribution to TOC in selected effluent fractions (mean and standard deviation of the four replicate columns)

and at the solid phase (mean and standard-deviation of column C1 and C2, each four quadrants per layer) after the transport experiment according to

Dibbern et al. (2014). Same assumptions as in Dibbern et al. (2014) have been applied for the weighted mean of families (2.96 copies of 16S rRNA

genes per cell) and the amount of 26.27 fg carbon per cell for the calculation of the bacterial biomass carbon.

samples mean cum. pore volumes

16s rRNA gene abundance Bacterial cell numbers Bacterial biomass

carbon Mean TOCBacterial

contribution to TOC

qPCR Copies / copies per cell Cell number x 26.27 fg carbon cell-1

[-] [copies u-1] [cell u-1] [µg C u-1] [µg u-1] [%]

Effluent Fract. 1 0.1 7.96 x 102 ± 1.98 x 102 2.69 x 102 ± 6.68 x 101 7.07 x 10-6 ±1.76 x 10-6 6.04 ± 1.78 1.27 x 10-4 ±

6.65 x 10-5

[u = ml] Fract. 10 0.9 1.02 x 108 ± 4.02 x 107 3.43 x 107 ± 1.36 x 107 0.90 ± 0.36 389.18 ± 118.02 0.26 ± 0.18

Fract. 22*FI-1 1.2 1.68 x 108 ± 3.75 x 107 5.66 x 107 ± 1.27 x 107 1.49 ± 0.33 242.01 ± 43.75 0.63 ± 0.20

Fract. 42 *FI-2 1.9 2.99 x 108 ± 2.39 x 108 1.01 x 108 ± 8.07 x 107 2.65 ± 2.12 91.95 ± 6.82 2.87 ± 2.37

Fract. 53-54 2.3 1.52 x 108 ± 1.16 x 108 5.13 x 107 ± 3.93 x 107 1.35 ± 1.13 65.57 ± 6.92 2.02 ± 1.52Fract. 101-106* FI-3 3.7 4.27 x 107 ± 1.60 x 107 1.44 x 107 ± 5.41 x 106 0.38 ± 0.14 53.01 ± 15.88 0.70 ± 0.07

Fract. 114-118 4.0 4.25 x 107 ± 4.97 x 107 1.44 x 107 ± 1.68 x 107 0.38 ± 0.44 36.18 ± 9.09 0.90 ± 0.82Solid phase SL 1.78 x 1010 ± 4.71 x 109 6.02 x 109 ± 1.59 x 109 158.05 ± 41.79 11.56 ± 0.13 1.37 ± 0.37

[u = g] IL 1.02 x 1010 ± 3.13 x 109 3.44 x 109 ± 1.06 x 109 90.29 ± 27.77 8.28 ± 1.02 1.12± 0.39

RL 5.32 x 107 ± 5.92 x 107 1.80 x 107 ± 2.00 x 107 0.47 ± 0.53 b.d.l.a -* first effluent fraction after a flow interruptiona b.d.l. below detection limit

Page 4: ars.els-cdn.com€¦ · Web viewKatharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of. Hydrogeology, Burgweg 11, D-07749 Jena, Germany

Figures: Supplementary data

Fig. S1. Cumulative pore size distribution (column: C1, C2) of the SL (a) and the RL (b)

before and after the transport experiment. Only pores > 228 µm were considered. The total

porosity was 0.47.

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Figure S2. SEM images of a) the RL mineral mixture with quartz minerals surrounded by

illite and goethite before the transport column experiments, and b) of more chaotic mineral

structures at the end of the experiment. SEM images of c) microbial structures (highlighted in

orange) in the SL at the beginning and d) a single cell in RL1 after the transport experiment.

Page 6: ars.els-cdn.com€¦ · Web viewKatharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of. Hydrogeology, Burgweg 11, D-07749 Jena, Germany

Fig. S3. Course of pH (a). the electric conductivity and chloride(Cl) (b), sulfate (c),

phosphate (d), turbidity and total iron (e), hydrodynamic diameter and zeta potential (f) in the

effluent of all columns (n=4). Markers: mean values of the four replicate columns. Error bars:

standard deviation. Vertical lines: indicate the flow interruptions (FI). The durations of FIs are

shown on top of the figures. Horizontal lines: represent the background concentrations of

artificial rain water (ARW) or manure (estimated from batch experiment).

Page 7: ars.els-cdn.com€¦ · Web viewKatharina Lehmann, Friedrich Schiller University Jena, Institute of Geosciences, Department of. Hydrogeology, Burgweg 11, D-07749 Jena, Germany

Fig. S4. DGGE-fingerprint based on 16S rRNA gene amplicons of total bacterial

communities in selected effluent fractions of all 4 replicate columns. White arrow: marks

band observable in all effluent fractions of all columns. Patterned arrow: marks shift in the

bacterial community structure over time. Frct: fraction. Marker *: fractions after FI. FI-(1-3):

flow interruption. AS-SL-start: artificial SL mixture shortly after mixing with microbial

inoculum. AS-SL-incub: AS SL mixture incubated for 3 days used for packing of columns.

BS: bacterial standard.