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GB/T 30740-2014 English PDF

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GB/T 30740-2014: Determination of total organic carbon in marine sediment -- Nondispersive infrared absorption
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PDF similar to GB/T 30740-2014


Standard similar to GB/T 30740-2014

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Basic data

Standard ID GB/T 30740-2014 (GB/T30740-2014)
Description (Translated English) Determination of total organic carbon in marine sediment -- Nondispersive infrared absorption
Sector / Industry National Standard (Recommended)
Classification of Chinese Standard Z17
Classification of International Standard 07.060; 13.060
Word Count Estimation 9,995
Date of Issue 6/9/2014
Date of Implementation 10/1/2014
Quoted Standard GB 17378.5-2007
Regulation (derived from) National Standards Bulletin No. 11 of 2014
Issuing agency(ies) General Administration of Quality Supervision, Inspection and Quarantine of the People's Republic of China, Standardization Administration of the People's Republic of China
Summary This Standard specifies the method for the determination of total organic carbon in marine sediments with a non-dispersive infrared absorption. This Standard applies to the determination of estuaries, bays, coastal and ocean sediments TOC.

GB/T 30740-2014: Determination of total organic carbon in marine sediment -- Nondispersive infrared absorption


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Determination of total organic carbon in marine sediment. Nondispersive infrared absorption ICS 07.060; 13.060 Z17 National Standards of People's Republic of China Determination of total organic carbon in marine sediments Non-dispersive infrared absorption method Issued on. 2014-06-09 2014-10-01 implementation Administration of Quality Supervision, Inspection and Quarantine of People's Republic of China Standardization Administration of China released

Foreword

This standard was drafted in accordance with GB/T 1.1-2009 given rules. This standard was proposed by the State Oceanic Administration. This standard by the National Standardization Technical Commission for Oceanography (SAC/TC283) centralized. This standard was drafted. State Oceanic Administration, the South China Sea Environmental Monitoring Center. The main drafters of this standard. Xinhai Hong, Huang Chuguang, Liujing Qin, Ni Zhixin, Guo Juan, Chang Chao, He Xiaoyuan, forest side, side HTC, Cai Syria, Qu EASTERN Chen Jiahui, blue Saint welcome. Determination of total organic carbon in marine sediments Non-dispersive infrared absorption method

1 Scope

This standard specifies the method for the determination of total organic carbon in marine sediments with a non-dispersive infrared absorption. This standard applies to the determination of estuaries, bays, coastal and ocean sediments TOC.

2 Normative references

The following documents for the application of this document is essential. For dated references, only the dated version suitable for use herein Member. For undated references, the latest edition (including any amendments) applies to this document. GB 17378.5-2007 marine monitoring Part 5. Sediment analysis

3 Terms and Definitions

The following terms and definitions apply to this document. 3.1 Marine sediments marinesediment General term for various marine seabed sediment formed by deposition. 3.2 Total carbon totalcarbon; TC Carbon in general, including organic carbon and inorganic carbon. 3.3 Total inorganic carbon totalinorganiccarbon; TIC Inorganic carbon in general, including the carbonate or bicarbonate of carbon present in the form. 3.4 TOC totalorganiccarbon; TOC Organic general form of the element carbon.

4 principle of the method

The samples were high temperature combustion or acid treatment, the appropriate form of carbon is converted to carbon dioxide, generated by the sample and the sample of Proportional to the carbon content. An oxygen carrier, the content of carbon dioxide to form carbon content is calculated corresponding measured by an infrared detector. TOC can be used directly or subtraction method was measured. 4.1 Determination of total organic carbon subtraction 4.1.1 Determination of total carbon Samples from the injector into the combustion temperature, which leads to high purity oxygen in the sample of all carbonaceous material is oxidized to carbon dioxide, produced by

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