ISSN 0137-0944
eISSN 2949-6144
En Ru
ISSN 0137-0944
eISSN 2949-6144
Laboratory determination of the solid phase composition of technogenic salted peat bog: possibilities and limitations

Laboratory determination of the solid phase composition of technogenic salted peat bog: possibilities and limitations

Abstract

The laboratory study of the solid phase of salted peat by X-ray fluorescence analysis revealed the presence of some halogen-organic compounds. Cl-organic compounds were formed in one third of peat samples, while their share is small: 14-15% of the total Cl. On the contrary, Br-organic compounds are formed more often and Brorg proportion is higher: from 12 to 23% of total Br. Relatively weak development of halogenisation of the organic matter in salted peat bog is explained by the recovery conditions that prevent the synthesis of halogen-organic compounds. In X-ray diffraction analysis of peat ash, errors are possible, both due to the growth of minerals, and due to incomplete identification of the number of phases in high-ash peat samples. The second type of error can be corrected using data on the content of chlorine in peat by X-ray fluorescence analysis. In the characteristic of peat bog contamination, in addition to salt profiles in the solution, it is necessary to determine the number and composition of halogen-organic compounds, some of which have herbicide properties.

References

  1. Biester И., Keppler F., Putschew A. et al. Halogen retention, organohalogen and the role of organic matter decomposition on halogen enrichment in two Chilean peat bogs // Environ. Sci. Technol. 2004. Vol. 38.

  2. Johansson E., Krantz-Rulcker C., Zhang B.X., Oberg G. Chlorination and biodegradation of lignin // Soil Biol. Biochem. 2000. Vol. 32.

  3. Kabata-Pendias A. Trace elements in soils and plants. CRC Press, 2011.

  4. Kotte K., Low F., Huber S.G. et al. Organohalogen emissions from saline environments — spatial extrapolation using remote sensing as most promising tool // Biogeoscience. 2012. Vol. 9.

  5. Leri A., Myneni S.C.B. Natural organobromine in terrestrial ecosystems // Geochim. Cosmochim. Acta. 2012. Vol. 77.

  6. Oberg G., Johansen C., Gron C. Organic halogens in spruce forest through fall // Chemosphere. 1998. Vol. 36.

  7. Oberg G.y Nordlund E., Berg B. In situ formation of organically bound halogens during decomposition of Norway spruce needles: effects of fertilization // Can. J. For. Res. 1996. Vol. 26.

  8. Oberg G., Sanden P. Retention of chloride in soil and cycling of organic matter-bond chlorine // Hydrol. Proc. 2005. Vol. 19.

  9. Svensson T, Sanden P., Bastviken D., Oberg G. Chlorine transport in a small catchment in southeast Sweden during two years // Biogeochemistry. 2007. Vol. 82.

  10. Vodyanitskii Yu., Minkina T, Zamulina I. Methodological aspects in the analysis of the content of mobile compounds of heavy metals in hydromorphic soils // Appl. Geochem. 2020. Vol. 113.

  11. Winterton N. Chlorine: the only green element — towards a wider acceptance of its role in natural cycles // Green Chem. 2000. Vol. 2.
PDF, ru

Received: 02/11/2020

Accepted: 03/13/2020

Accepted date: 09/30/2020

Keywords: X-ray fluorescence soil analysis; soil analysis; X-ray diffractometric soil analysis; halogens; Cl-organic compounds; Br-organic compounds

Available in the on-line version with: 30.09.2020

  • To cite this article:
Issue 3, 2020