1 1 2 3 4 5 6 Biology and Fertility of Soils Kinetics of short-term carbon mineralization in roots of biofuel crops in soils 7 Supplemental Information 8 9 10 Authors: F. A. Rivas1 • M. A. Tabatabai1 • D. C. Olk2 • M. L. Thompson1 11 12 13 14 15 16 17 18 19 Corresponding author: Dr. M.L. Thompson Department of Agronomy Iowa State University Ames, Iowa 50011-1010 U.S.A. Email: (mlthomps@iastate.edu) Phone: 515-294- 2415 Fax: 515-294-3163 20 21 22 23 1 Agronomy Department, Iowa State University, Ames, Iowa 50011 USA 24 2 USDA-ARS, National Laboratory for Agriculture and the Environment, Ames, Iowa 50011 25 USA 26 2 27 Supplemental Information 28 To determine lignin in the root samples, the acetyl bromide method was adapted from Hatfield et 29 al. (1999). Approximately 10-15 mg of root samples were weighed into 30-mL glass tubes with 30 screw caps. Then 10 mL of distilled, deionized water were added to each tube. The tubes were 31 capped, mixed, and heated at 65oC on a block digester for one hour. The suspensions were 32 filtered through a 25-mm diameter glass fiber filter and the root residues were washed 33 sequentially with approximately 3-5 mL of water, ethanol, acetone, and diethyl ether to remove 34 the water-soluble and semi-water-soluble carbohydrates. After rinsing, the filter papers and their 35 root residues were transferred into 50-mL tubes and dried overnight at 70oC. The dried roots 36 were then mixed with 2.5 mL of 25% (v/v) acetyl bromide in glacial acetic acid and the samples 37 were heated in 50-mL tubes for 2 hours in block digester at 50oC. After cooling, each digestate 38 was quantitatively transferred into a 50-mL volumetric flask that contained 10 mL of 2 M NaOH 39 and 12 mL of glacial acetic acid and was diluted to volume with glacial acetic acid. The solution 40 was shaken and filtered through a 47-mm glass fiber filter to remove colloidal particles that 41 could interfere in the spectrophotometric analysis. The absorbance of the filtered sample was 42 measured at 280 nm by a UV-Vis spectrophotometer. The results were calculated from 43 calibration graphs prepared by using lignin standards (Sigma-Aldrich, St. Louis, Mo) 44 Monosaccharides (fucose, arabinose, rhamnose, galactose, glucose, xylose, and mannose) 45 were extracted from the root samples by using a procedure adapted from that of Martens and 46 Loeffelmann (2002). Here, 20 mg of root materials were weighed into a 15 x 125-mm labeled 47 culture tube and soaked in 800 μL of 6 M H2SO4 for 30 minutes. The sample was then diluted 48 with 4 mL of deionized water to adjust the concentration of acid to 1 M H2SO4. The diluted 49 solution was autoclaved for 30 minutes at 121oC. The samples were cooled, centrifuged, and 3 50 decanted into Falcon tubes. The sample pellet was rinsed twice, each time by adding 1 mL of 51 deionized water; the washings were centrifuged and transferred to the originally collected 52 supernatant. The pH of the supernatant was then adjusted to pH 5.5 - 6.5 by addition of NaOH 53 solution and monitored by a pH meter. The sample was then diluted with deionized water to 10 54 mL. A 1-mL aliquot of the sample was further diluted to 10 mL, and 500 μL of the diluted 55 sample were pipetted into an auto sampler vial to be analyzed for the monosaccharides noted 56 above by ion chromatography. The sum of these sugars was taken as an index of hemicellulose 57 (HI) for the root samples. The residues left from the first acid extraction were saved and dried 58 overnight at 58 - 60oC. To obtain a cellulose index (CI), the dried residue was soaked for 30 59 minutes in 300 𝜇L of concentrated H2SO4. The concentration of the sample solution was adjusted 60 to 1.5 M by adding 3.3 mL of deionized water. The samples in the culture tubes were autoclaved 61 and glucose was determined by ion chromatography. Monosaccharides comprising both the HI 62 and the CI were determined using a Dionex DX-500 Chromatograph (Dionex Corporation, 63 Sunnyvale, CA) equipped with a CarboPac PA10 column (2 mm i.d.) and using 5 - 80 mM 64 NaOH as the eluent (Martens and Frankenberger, 1990b). 65 Water-holding capacity of the soil was determined by saturating a known mass of air- 66 dried soil material over a 24-h period, allowing the sample to drain freely in a humid atmosphere, 67 and then measuring the wet mass of the sample. 68 References 69 Hatfield R, Grabber J, Ralph J, Brei K (1999) Using the acetyl bromide assay to determine lignin 70 concentrations in herbaceous plants: Some cautionary notes. J Agri Fd Chem 47: 628- 71 632 4 72 73 74 Martens D A, Loeffelmann KL (2002) Improved accounting of carbohydrate carbon from plants and soils. Soil Biol Biochem 34:1393-1399