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Vario macro cube elemental analyzer

Manufactured by Elementar
Sourced in Germany

The Vario MACRO cube elemental analyzer is a laboratory equipment designed for the determination of carbon, hydrogen, nitrogen, sulfur, and oxygen in a wide range of solid and liquid samples. It utilizes combustion and state-of-the-art detection technologies to provide accurate and reliable analytical results.

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8 protocols using vario macro cube elemental analyzer

1

Surface Composition of Modified Celluloses

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Surface
composition of pure CEL and modified cellulose (H-CEL, V-CEL,
and S-CEL) were recorded with monochromatic A1 Kα irradiation
at 100 W and effectively charged to neutralization with slow thermal
electrons, using AXIS Ultra instrument (Kyoto, Japan). C–C/C–H
assigned to the C 1s signal was set at 285.0 keV. XPS PEAK 41 program
was used for the spectrum decomposition for C 1s, with the subtraction
of a Shirley background before Gaussian functions. The degree of surface
substitution (DSS) was calculated from eq 1(23 (link)) where C(O–C=O)
is the percentage of O–C=O groups from the grafted acids
and Ccellulose is the percentage of the
C–O and O–C–O groups.
The DS in the bulk
was also calculated from elemental analysis by using a Vario Macro
cube elemental analyzer (Elementar, Fulda, German) which was used
to determine the carbon, hydrogen, nitrogen, and oxygen content in
the unmodified and modified celluloses (H-CEL, V-CEL, and S-CEL).
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2

Soil Nutrient Analysis Protocol

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Soil samples were extracted with 2M potassium chloride solution for the detection of NH4+-N and NO3-N (Maharjan and Venterea, 2013 ). The soil organic matter (SOM) and total nitrogen (TN) were determined by an Element Vario MACRO cube elemental analyzer (Elementar, Germany). The total phosphorus (TP) and available phosphorus (AP) were determined by the molybdenum blue colorimetric method with a spectrophotometer. The total potassium (TK) and available potassium (AK) were determined by a BWB-XP flame photometer (BWB Technologies, UK). Soil mineral N was extracted with 2 M KCl solution in a 1:5 soil-solution ratio, and the NH4+-N and NO3-N concentrations were determined by a Skalar San++ continuous flow analyzer (Skalar, Netherlands). The cellulose and lignin contents were determined as described in a previous study (Chen et al., 2019 (link)).
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3

Elemental Composition Analysis of Thraustochytrid Biomass

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The elemental composition (C, N, H, and S) of the biomass of thraustochytrid isolates was analyzed for the exponential (24 h) and stationary (96 h) growth phases. The time points 24 h and 96 h were chosen as exponential and stationary phases, respectively, based on the growth curves of the isolates (Figure S4). The isolates were cultivated in 50 mL of sterilized M4 medium inoculated with respective seed cultures (5% v/v) for 7 days at 28 ℃ and 170 rpm. Seed cultures (5% v/v) were prepared as described in Section 4.1. Samples were collected from the culture broth and a subsample of about 8 mL was used for cell harvesting by centrifugation (20 min, 8000 rpm, 20 ℃). The resulting cell pellet was washed several times with 5 mL of sterile deionized water and pre-frozen at −80 ℃ and then lyophilized in a freeze dryer (CHRIST ALPHA 1-2 LD Plus, Germany) for 48 h. The freeze-dried cells were weighed to obtain their dry cell weight. The elemental composition of the freeze-dried cells (2 mg) was determined on a vario MACRO cube elemental analyzer (Elementar Analysensysteme GmbH, Germany) following the manufacturer’s instructions.
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4

Moss Tissue Elemental Analysis

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Carbon and N concentrations in moss tissue were assessed with a Vario Macro Cube Elemental Analyzer (Elementar, Germany). Total phenols were measured in moss tissue that had been ground into fine powder and then suspended in 10 mL ethanol. Samples were shaken for 120 min and then centrifuged at 3600 g for 10 min. The supernatant was analysed for phenols using the Folin–Ciocalteu reagent. The absorbance was measured at 725 nm using a spectrophotometer. The pH of mosses was measured in 3 g fresh moss tissue that was submerged in 15 mL ddH2O and then shaken for 60 min. The pH of the extracts was determined with a pH electrode.
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5

Sediment Geochemical Analysis

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After digestion with aqua regia, sediment total iron content was determined using an inductively coupled-plasma mass spectrometer (ICP-MS, ELAN DRC II, Perkin Elmer, Waltham, MA, USA) [17 (link)]. Carbonates of sediment samples were removed by immersion in 1 M HCl, then the total organic carbon (TOC) and total nitrogen (TN) of the sediment were measured by a Vario MACRO cube elemental analyzer (Elementar Analysensysteme GmbH, Langenselbold, BAV, Germany). χlf of the sediment soil was determined by a MS2B magnetic susceptibility meter (Bartington Instruments Ltd., Witney, Oxon, UK).
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6

Comprehensive Plant and Soil Analysis

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For plant nutrients, LN was determined by combustion on a Vario MACRO cube elemental analyzer (Elementar Analysensysteme Gmb H, Germany; Lu et al., 2015 (link)). LP was measured with the molybdate colorimetric test (Sommers and Nelson, 1972 (link)). For soil properties, soil water content (SWC) and soil bulk density (SBD) were tested using a drying method (Yao, 2006 ); soil organic carbon content (SOC) and soil total nitrogen content (STN) were determined by combustion on a Vario MACRO cube elemental analyzer (Lu et al., 2015 (link)); and soil total phosphorus content (STP) was measured with the molybdate colorimetric test after perchloric acid digestion (Sommers and Nelson, 1972 (link)). Soil available nitrogen content (SAN) was determined from the alkali hydrolyzable fraction, and soil available phosphorus content (SAP) was measured by the Olsen method (Sun et al., 2018 (link)). For soil microbial factors, the determination of microbial biomass carbon content (MBC) and nitrogen content (MBN) was performed with the chloroform–K2SO4 extraction method (Vance et al., 1987 (link)).
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7

Elemental Analysis of Plant Samples

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After sampling, the leaves were mixed to form composite samples from ten to fifteen different individuals. The materials were crushed, sieved through an 80-mesh screen, and then dried at 70°C for 24 hours before being packed in plastic bags for measurement. A Vario Macro Cube Elemental analyzer (Elementar, Hanau, Germany) was used to assess total contents of carbon and nitrogen. Total phosphorus contents were measured using a molybdenum antimony resistance colorimetric method. For each species, the measurements were repeated three times.
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8

Physicochemical Characterization of Soils

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Soil samples were freeze-dried, thoroughly grounded, and passed through a 200 mesh sieve prior to physicochemical characterization. Parameters of pH, sulfate, and nitrate were measured according to the standard methods, which were narrated previously (Sun et al., 2015) (link). SOC was directly determined with a vario MACRO cube elemental analyzer (Elementar, Hanau, Germany). For measuring the concentrations of metal(loid)s including Cr, Cu, Cd, Pb, Zn, As, and Sb and their acid-soluble fractions, the dried soil samples were completely digested with HNO 3 /HF at a volume ratio of 5:1 (Sun et al., 2018a) and 0.11 M acetic acid (Zhai et al., 2018) (link), respectively, then determined using an Agilent 7700x inductively coupled plasma mass spectrometer (ICP-MS).
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