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Ea1110

Manufactured by Carlo Erba
Sourced in Italy

The EA1110 is a laboratory instrument designed for elemental analysis. It is capable of determining the elemental composition of various samples.

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6 protocols using ea1110

1

Soil Characterization Protocol

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Soil texture was obtained by the pipette method (Day, 1965) after the specimens were submerged in NaClO (pH 9) for 24 h to destroy the organic cements. Soil pH was measured in a suspension (solid:liquid ratio 1:2.5) by a combined glass-calomel electrode. Soil mineralogy was assessed by x-ray diffraction with a Philips PW 1830 diffractometer (Fe-filtered Co K1 radiation, 35 kV and 25 mA). A semi-quantitative estimation was obtained after identification of the minerals on the basis of their characteristic peaks. Separates of 0.5-2 mm diameter, recovered from the extraction residue of the organic matter fractionation protocol prior the 0.5 M HCl solution treatment (see below), were observed under an optical microscope. Total C and N were determined by a Carlo Erba EA1110 dry combustion analyzer. The amount of total organic C (TOC) was measured by dichromate digestion, heating the suspension at 180°C for 30 min (Allison, 1965) . As the Walkley-Black method without application of heat is considered not able to oxidize the coarse particulate organic matter, it was used to estimate the amount of the most oxidizable organic matter (e.g., Frink, 1995) , here called organic C (OC). The content of inorganic C was obtained from the difference between total C and TOC.
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2

Elemental Composition Analysis of Compost

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Samples dried at 40 0 C (about 1kg each) were ground, passed through a 2 mm sieve, and used to measure pH and total C and N content. The pH was determined potentiometrically in H2O (1:8 w/v). Total C and N were determined by dry combustion method using a CHNS analyzer (EA-1110, Carlo Erba Instruments, Milan, Italy) . Total solid content (TS) was estimated as the fraction of the dry mass after samples were dried at 105 0 C for 24 h. Organic matter (OM) was determined as the loss on ignition (Heiri et al., 2001) at 550 0 C until constant weight was obtained. Water extractable Al, Ca, Ba, Cd, Cu, Fe, Mg, Mn, Na, Ni, P, Pb, S, and Zn were determined by using 10 g of ground compost samples that were added to 100 ml of distilled water (1:10 w/v) and shaken for about 1 h at 10 rpm. The suspension was then centrifuged for 10 minutes at 300 g and the solution filtered using Whatman 42 filter. The extract was used to determine the concentration of the elements on an ICP-MS (Pröfrock and Prange, 2012) (link).
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3

Characterization of Malt Residue and Anaerobic Sludge for Biogas Production

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Malt residue (substrate) and anaerobic sludge (inoculum) were characterized through the analysis of volatile solids (VS), the samples were placed in a muffle EDG model Thermo-3000; pH measurements were performed in a Digimed DM23 pH-meter. Electrical conductivity of the samples was acquired by conductimetric method through the DM23 pH-meter. Finally, elemental analysis (Carbon, nitrogen, sulfur and hydrogen) was carried out in a Carlo-Erba-Instruments model EA 1110. For the substrate, volatile acidity, alkalinity, chemical oxygen demand (COD, in mg O2/L) and biochemical oxygen demand (BOD, in mg O2/L) analyzes were performed with the objective to investigate the conversion of organic matter into biogas. Three analyzes were carried out: one for the sludge used in the biodigester; one for the malt bagasse before biodigestion; and for the malt bagasse after the experiment of the biodigestion process.
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4

Soil Physicochemical Characterization Protocol

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The soil pH was determined potentiometrically in water (solid:liquid ratio of 1:2.5) after one night of equilibration using a Thermo Scientific™ Orion™ 2-Star Benchtop pH-meter. The total organic C (TOC) was estimated by K-dichromate digestion method, heating the suspension at 180 °C for 30 min [27 ]. The water extractable organic C (WEOC) was extracted by mixing 1 g of soil with 10 mL of water. The mixture was shaken overnight with an orbital shaker (140 rpm), centrifuged at 1400 g for 10 min and filtrated through a 0.45 μm membrane filter [28 (link)], and its organic C content was analyzed by K-dichromate digestion method, as reported above. The total N (TN) was measured by a dry combustion analyzer (EA-1110, Carlo Erba Instruments, Milan, Italy). The inorganic N forms (NH4+-N and NO3-N) were determined, after processing the samples with 2 M KCl solution (solid:liquid ratio 1:10), by a FOSS Fiastar™ 5000 system (Hillerod, Denmark). The difference between the total N and inorganic N content was considered as organic N.
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5

Leaf Nitrogen Content Analysis

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For dry matter nitrogen content, oven‐dried leaves were ground to a consistent powder and the percentage nitrogen was calculated by combustion of samples in an elemental analyser (EA1110, Carlo Erba, Cornaredo, Italy).
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6

Isotopic Analysis of Plant Roots

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Total C and the 13C/12C ratios of the roots were determined by isotope ratio mass spectrometry (IRMS) using an elemental analyzer (EA 1110; Carlo Erba, Italy) coupled with a mass spectrometer (Delta S; Thermo Finnigan, Germany). The δ13C value was expressed relative to the international V-PDB standard and the analytical precision, which is the standard deviation (SD) of the measured results of the working standard (plant biomass), was 0.2‰.
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