The largest database of trusted experimental protocols

2400 2 chn elemental analyzer

Manufactured by PerkinElmer
Sourced in United States

The 2400 II CHN Elemental Analyzer is a laboratory instrument designed to determine the carbon, hydrogen, and nitrogen content in a wide range of organic and inorganic samples. It utilizes a combustion process to analyze the elemental composition of the sample.

Automatically generated - may contain errors

5 protocols using 2400 2 chn elemental analyzer

1

Elemental Composition Analysis

Check if the same lab product or an alternative is used in the 5 most similar protocols
Elemental CHN composition data were obtained using a PerkinElmer 2,400 II CHN Elemental Analyzer.
+ Open protocol
+ Expand
2

Comprehensive food composition analysis

Check if the same lab product or an alternative is used in the 5 most similar protocols
Sample moisture contents were measured by heating at 105°C and cooling in a desiccator to a constant weight. The ash content was measured at 600°C. Crude fat was extracted by Soxhlet extraction with diethyl ether, with reference to an AOAC Standard Method (1980, 7.056). Crude protein and crude fiber contents were measured using a facility service at the Japan Food Research Laboratory. The crude protein content was determined using the Kjeldahl method with a conversion factor of 6.25. Crude fiber was calculated using the ceramic fiber filter method based on the report of Sawaya, Al‐Shalhat, AlSogair, and Al‐Mohammad (1985). Crude protein, crude fat, crude fiber, and ash contents were each measured at least twice to obtain analytical results within the experimental error range of 5% and average values. Elemental CHN composition data were obtained using a PerkinElmer 2400 II CHN Elemental Analyzer.
+ Open protocol
+ Expand
3

Soil and Climate Influence on Ecosystem

Check if the same lab product or an alternative is used in the 5 most similar protocols
The environmental parameters were geographic variables (latitude, longitude, and elevation) and meteorological data [mean annual precipitation (MAP) and mean annual temperature (MAT)] at each sampling site and soil properties [pH, electrical conductivity (EC), total carbon (TC), total nitrogen (TN), and the TC/TN ratio] for each sample. The meteorological data (MAP and MAT) were collected from the Chinese Meteorological Agency Database1. Soil pH was measured by using an E20-FiveEasy pH meter (Mettler Toledo, Giessen, Germany), and the soil EC was calculated by using an electric conductometer. Both soil measurements used a soil water suspension (a 5:1 vol/vol mixture of deionized water and soil) after shaking for 30 min. Soil TC and TN were determined with a carbon–hydrogen–nitrogen elemental analyzer (2400 II CHN Elemental Analyzer; PerkinElmer, Boston, MA, United States). Meteorological data and soil properties are shown in Supplementary Tables 1, 2, respectively.
+ Open protocol
+ Expand
4

Comprehensive Soil Characterization and Analysis

Check if the same lab product or an alternative is used in the 5 most similar protocols
Total soil carbon and nitrogen were determined by combustion on a CHN elemental analyzer (2400 II CHN elemental analyzer, PerkinElmer, Boston, MA, USA). Total soil phosphorus was determined by the molybdenum blue method with a ultraviolet–visible spectrophotometer (UV-2550, Shimadzu, Kyoto, Japan). Soil CaCO3 was analysed volumetrically on ground subsamples using a Calcimeter (Eijkelkamp, Netherland). Soil organic carbon was calculated as the difference between total soil carbon and carbon bound in soil CaCO3. The density of soil organic carbon, soil nitrogen, soil phosphorus and soil CaCO3 were calculated in the top 0–5 cm. Soil moisture was measured gravimetrically after ∼10-h desiccation at 105 °C. Soil available nitrogen (sum of ammonium, nitrate and dissolved organic nitrogen) were determined using a TOC-TN analyzer (Shimadzu, Kyoto, Japan). Soil pH was determined in a 1:5 ratio of fresh soil to deionised water slurry on a pH meter (Thermo 0rion-868).
+ Open protocol
+ Expand
5

Measuring Terrestrial Carbon Cycling

Check if the same lab product or an alternative is used in the 5 most similar protocols
We installed 10 litter traps (1×1 m 2 ) at each plot in July 2011. Litter was collected monthly during the growing season (April to November) from August 2011 until July 2014. After collection, litter was taken to the laboratory, oven dried at 65°C to a constant weight, weighed, and then annual litter production (Mg C ha 1 a 1 ) was calculated. We estimated dead root production (Mg C ha 1 a 1 ) using eq. ( 4) [14, 25] :
Litter production Root production Root biomass Aboveground biomass  
. (4)
Woody debris production represents the losses from the mortality (that is, death of entire trees) per year. In addition, we measured the stocks of litter and woody debris by harvest and weight in July 2011. Sub-samples of litter and woody debris were air dried for 2 weeks at 25°C, and then ground and sieved (0.15 mm). The C concentrations of both litter and woody debris were determined using an Elemental Analyzer (2400 II CHN Elemental Analyzer; Perkin-Elmer, Boston, USA).
+ Open protocol
+ Expand

About PubCompare

Our mission is to provide scientists with the largest repository of trustworthy protocols and intelligent analytical tools, thereby offering them extensive information to design robust protocols aimed at minimizing the risk of failures.

We believe that the most crucial aspect is to grant scientists access to a wide range of reliable sources and new useful tools that surpass human capabilities.

However, we trust in allowing scientists to determine how to construct their own protocols based on this information, as they are the experts in their field.

Ready to get started?

Sign up for free.
Registration takes 20 seconds.
Available from any computer
No download required

Sign up now

Revolutionizing how scientists
search and build protocols!