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Vario el analyser

Manufactured by Elementar

The Vario EL analyser is an elemental analyser designed to determine the total content of carbon, hydrogen, nitrogen, and sulfur in a wide range of organic and inorganic solid and liquid samples. It utilizes combustion and thermal conductivity detection principles to provide accurate and reliable analysis results.

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5 protocols using vario el analyser

1

Synthesis and Characterization of Iminodiethanol Complex

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All chemicals and solvents used for synthesis were obtained from commercial sources and used as received without further purification. All reactions were carried out under aerobic conditions. N-(2-Pyridylmethyl)iminodiethanol was prepared according to the literature procedure.43 (link) The elemental analyses (C, H, and N) were carried out using an Elementar Vario EL analyser. Fourier transform IR spectra (4000 to 400 cm–1) were measured on a PerkinElmer Spectrum GX spectrometer with samples prepared as KBr discs. Powder X-ray diffraction was carried out on a STOE STADI-P diffractometer, using Cu-Kα radiation with λ = 1.5406 Å.
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2

Peatland Carbon and Nitrogen Accumulation

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Long-term mass accumulation rates for N were calculated by Schillereff et al. (2016) for the Migneint during a study of UK ombrotrophic peatlands in 2014. Briefly, cores were extracted in triplicate using both a box corer (for peat shallower than 1 m), and Russian-type corer (peat deeper than 1 m). The core was sliced to 10 cm intervals with samples air dried, manually sieved to 2 mm to exclude large roots and dried at 60 °C before being ball-milled to a homogenous powder. After drying at 105 °C, carbon and nitrogen were determined using an Elementar Vario-EL analyser. Bulk sub-samples of the upper (20-30 cm), mid and base of the core were then submitted to the NERC Radiocarbon Facility at East Kilbride for 14 C analysis. These data were used to estimate down core patterns in accumulation rates utilised in this study.
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3

Plant Tissue C:N Ratio Analysis

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After weighing biomass, belowground and aboveground plant C and N concentrations were measured on ground samples using an automated Dumas procedure on a Vario EL analyser (Elementar). This was used to calculate whole plant mean C: N ratio (the mean of above-and belowground C: N ratios). Since plant tissue C: N ratio is the mass of C relative to the mass of N in plant tissue, it provides a similar measure to tissue %N content, with the advantage of being easily compared to other substrates such as soil. To calculate total N content (g), %N content of above-and belowground biomass components was multiplied by the corresponding biomass (g) and then summed. We also calculated % dead aboveground biomass (of total aboveground biomass) and two allocation patterns: root mass fraction (RMF: belowground biomass/ total biomass) and root nitrogen fraction (RNF: belowground N/ total N).
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4

Soil Sampling and Analysis for Bioassays

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Representative soil samples for the bioassays were taken from each plot by pooling five soil sub-samples (depth 10 cm, diameter 8 cm) collected from the centre of each plot and four orthogonal points 5 m from the centre. Fresh soil was sieved to 4 mm and stored at 4°C prior to analyses. KCl extractable N concentration (NO 3 --N and NH 4 + -N) was determined colorimetrically in a segmented flow stream using an AutoAnalyser (Seal-Analytical). Net N-mineralisation rate was measured as the release of mineral N after incubation of soil samples (5 g) for 14 days at 25°C (Ross 1992 ). Soil moisture content, water-holding capacity (WHC) and pH (1:2.5, soil/water) were also determined for each soil sample. Litter of each of the four grass species (A. capillaris, A. odoratum, C. flavescens subsp. Brevis and P. colensoi) was collected from each plot. For each species, at least 10 g of senesced leaves was collected from at least five individual plants. Due to the timing of collection, the majority of senescent material available from A. odoratum was stem litter and not leaf litter, so stem litter was used for all analyses of this species. All litter was processed in the same way as the standardised litter described above (that is air-dried and homogenised). Litter C and N concentrations were measured on ground samples using an automated Dumas procedure on a Vario EL analyser (Elementar).
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5

Latitudinal Gradient of Upland Peat Bog Cores

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New cores were collected from five upland ombrotrophic blanket bogs selected to represent a latitudinal gradients through Britain (Fig. 1). Triplicate adjacent cores were extracted in 2014 using both a box corer (to recover the surface vegetation and uppermost 1 m of peat) and a Russian-type corer (for peat deeper than 1 m). The sites were: Great Gnat's Head on Dartmoor (DM), Migneint (Mg) in northwest Wales, Moor House (MH) in northern England, Glensaugh (G) near the north eastern Scottish coast and Forsinard Flows (F) in the far north of mainland Scotland. Physiographical information for each site is summarised in Table 1. All cores extended down to the underlying mineral substrate, ranging in length from 95 cm (Glensaugh) to 417 cm (Forsinard).
The new cores were carefully extruded, sliced at 10 cm intervals, airdried for one week, manually sieved to 2 mm to remove large particles and roots, oven-dried at 60 °C to remove residual moisture and ball-milled to a fine, homogenous powder. Bulk densities of all samples were calculated prior to milling by dividing the dry matter mass by the original volume of wet material. Phosphorus content was measured colorimetrically using a Seal Analytical AQ2 discrete analyser after digestion in H 2 SO 4 /H 2 O 2 . After drying at 105 °C, carbon and nitrogen were determined on an Elementar Vario-EL analyser using an ISO17025 accredited method.
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