BS ISO 21226:2019
Soil quality. Guideline for the screening of soil polluted with toxic elements using soil magnetometry
Standard number: | BS ISO 21226:2019 |
Pages: | 36 |
Released: | 2019-12-17 |
ISBN: | 978 0 580 97554 7 |
Status: | Standard |
BS ISO 21226:2019 - Soil Quality Guideline for Screening Polluted Soil
Discover the comprehensive guideline designed to enhance the quality of soil assessment with the BS ISO 21226:2019 standard. This essential document provides a detailed framework for the screening of soil polluted with toxic elements using advanced soil magnetometry techniques. Released on December 17, 2019, this standard is a crucial tool for environmental scientists, soil quality experts, and regulatory bodies aiming to maintain and improve soil health.
Overview of BS ISO 21226:2019
The BS ISO 21226:2019 standard is a pivotal document that outlines the procedures and methodologies for detecting and analyzing toxic elements in soil. With a total of 36 pages, this guideline offers a thorough exploration of soil magnetometry, a non-invasive and efficient method for identifying soil contamination. The standard is recognized globally and is an invaluable resource for ensuring soil quality and safety.
Key Features
- Standard Number: BS ISO 21226:2019
- Pages: 36
- Release Date: December 17, 2019
- ISBN: 978 0 580 97554 7
- Status: Standard
Why Choose Soil Magnetometry?
Soil magnetometry is a cutting-edge technique that offers several advantages over traditional soil testing methods. It is a rapid, cost-effective, and non-destructive approach that allows for the detection of magnetic anomalies associated with toxic elements. This method is particularly useful in large-scale environmental assessments where quick and reliable data is essential.
Benefits of Using BS ISO 21226:2019
Implementing the guidelines set forth in the BS ISO 21226:2019 standard can lead to numerous benefits, including:
- Enhanced Accuracy: Provides precise detection of toxic elements, ensuring accurate soil quality assessments.
- Efficiency: Streamlines the screening process, saving time and resources.
- Environmental Protection: Helps in identifying and mitigating soil pollution, contributing to environmental conservation.
- Compliance: Assists organizations in meeting regulatory requirements and standards for soil quality.
Applications of BS ISO 21226:2019
This standard is applicable across various sectors, including:
- Agriculture: Ensures soil used for farming is free from harmful contaminants, promoting healthy crop production.
- Construction: Assesses soil quality for safe and sustainable building practices.
- Environmental Management: Aids in the monitoring and remediation of polluted sites.
- Research: Provides a reliable framework for scientific studies on soil contamination.
Understanding the Importance of Soil Quality
Soil quality is a critical component of environmental health, influencing everything from agricultural productivity to ecosystem stability. Contaminated soil can have far-reaching impacts, affecting plant growth, water quality, and human health. The BS ISO 21226:2019 standard plays a vital role in safeguarding soil quality by providing a robust methodology for detecting and addressing soil pollution.
Conclusion
The BS ISO 21226:2019 standard is an indispensable resource for anyone involved in soil quality assessment and management. By adopting this guideline, organizations can ensure they are using the most effective and reliable methods for detecting toxic elements in soil. This not only helps in maintaining compliance with environmental regulations but also supports the broader goal of sustainable environmental stewardship.
Invest in the future of our planet by utilizing the BS ISO 21226:2019 standard to enhance soil quality and protect our natural resources.
BS ISO 21226:2019
This standard BS ISO 21226:2019 Soil quality. Guideline for the screening of soil polluted with toxic elements using soil magnetometry is classified in these ICS categories:
- 13.080.10 Chemical characteristics of soils
This document specifies methods for the measurements of magnetic susceptibility of soils (?) as an indicator of potential soil pollution/contamination with trace elements associated with technogenic magnetic particles (TMPs) and describes related procedures, protocols and guidelines to be applied as a screening geophysical method of determination of soil pollution with trace elements. The results of measurements are used for preparing the maps of magnetic susceptibility of soils in the area of interest. From these maps, the areas of elevated and high magnetic susceptibility indicating high trace element total pollution load are discriminated for further identification of pollutants by geochemical methods.
This document is applicable to screening all TMPs-related anthropogenic emission sources including long-range transport of airborne elements, of which TMPs are carriers and indicators. Such emission sources comprise the majority of high-temperature industrial processes, where iron is present in any mineralogical form in raw materials, additives or fuels, is transformed into ferrimagnetic iron oxides (e.g. fossil solid and liquid fuels combustion, metallurgy, cement and ceramics industry, coke production, industrial waste landfills, land transport). This document is not applicable to screening anthropogenic emissions not associated with TMPs, e.g. organic pollutants or emissions from agricultural sources.
Copper, zinc and other non-ferrous metal ores also contain iron (in many sulfides) as this element is abundant in almost all environments. During smelting, the iron occurring in sulfides is transformed into ferrimagnetic oxides (TMPs). However, in such cases, the proportion of TMPs and related PTEs is usually less than at coal combustion or iron metallurgy, for example, and not all PTEs are physically associated and transported by TMPs. Non-airborne elements are deposited in the close proximity of the emission source, while TMPs can be used in these cases as indicators of airborne elements and of the spatial distribution of the total element deposition from a smelter in the area.
In rare cases, some soils are developed on bedrock exhibiting geogenically high magnetism, which can cause false-positive results. This influence can, however, be easily indicated by measurements of magnetic susceptibility along soil profiles. This method is not applicable when the bedrock exhibits extremely high magnetic signals.
Such cases are rare.