Skip to main content
Log in

Properties of humic substances from the baltic sea and lake ermistu mud

  • Research Article
  • Published:
Journal of Soils and Sediments Aims and scope Submit manuscript

Abstract

Scope and Goal

Humic substances (HSs) are the product of microbial degradation, chemical polymerisation and oxidation of organic matter. HSs can be divided into different fractions: humic acid (HA), hymatomelanic acid (HMA), fulvic acid (FA) and humin. HSs play a fundamental role in accumulation and exchange processes of chemical compounds (metals and organic pollutants) in the environment. HSs can form soluble complexes that migrate long distances or precipitate, carrying bound cations with them. The migration/precipitation abilities depend on the metal ion, the ion charge, the degree of ionisation of the organic molecule, the ionic strength of the media, and the location of the metal ion.

Objective

Estonia is rich in the Baltic Sea and lake sediments. Historically, mud has been used in human treatment as a curative mud. High-molecular HSs are an important part of curative mud and they have a strong effect on its properties. The curative mud which is used in human therapy may not be polluted with different organic and inorganic contaminants. The aim of this work is to characterise and compare HSs isolated from the Baltic Sea mud (Haapsalu Bay) and from the sediments of Lake Ermistu (Estonia).

Results and Conclusions

We determined the yield of basic extraction of different HSs components from mud in the course of separation. We found that acid pre-treatment of mud increased the amount of extracted HSs more in the sea mud than in the lake mud. These results show that HSs are bound to the inorganic/organic structure of mud and are released during prolonged treatment with an acid.

We performed elemental analysis of the different fractions of HS extracts. HMA fractions had the highest carbon content and the lowest nitrogen content. HMA contains more polysaccharides than amino acid residues. These subunits may cause a better solubility of HMA in water as compared to HA. Acid pre-treatment of the natural sea and the lake mud diminished the content of carbon in most of the HS fractions. The content of nitrogen in the sea and in lake FA diminished by about two times.

We determined the metal content in the mud and its HS fractions. We found that the concentration of heavy metals Pb and Cr is lower than <0.08 mg/kg. As expected, the total metal concentration is considerably lower in the lake than in the sea mud. Acid pre-treatment of mud shows that the sea HA forms more stable Fe and Mg complexes, while the sea HMA contains more stable Zn and Cu complexes. The lake HSs result in more stable Mg complexes with HA and HMA fractions. Sea FA binds Cu and Mg better, but lake FA is more effective in binding Zn. To compare the amount of metals extracted from HA, HMA, FA (with that, remains in HS fractions), the metal concentration in the alkaline full extract of the sea mud was determined. Alkaline treatment removed 0.8% Mg, 7.9% Cu, 5.2% Zn and 3.8% Fe together with HSs from the sea mud, the rest remained in humin and in the mineral part of the mud. The following work-up was additionally carried out for most of the metals. So, we found that there was only 1.7% of Fe, 2.1 % of Mg, 23.2% of Zn and 45.2% of Cu left in HA, HMA and the FA fraction (as a sum) from the total amount of those metals in HSs. This means that Cu is the metal most strongly bound to HSs. On the bases of HS separation data we found that the order of stability of the metal-humate complexes is Cu>Zn>Mg>Fe.

The ultraviolet spectra of HA, HMA and FA revealed that HMA had the biggest molar absorption and calculated aromaticity. Recommendations and Outlook. The characteristics of HSs, isolated from the Baltic Sea and Lake Ermistu mud reveal the difference of HSs from the sea and the lake mud. Also, different properties of HS fractions are observed. Metals are concentrated variously in different HS fractions. In all cases the content of Pb and Cr was low, meaning that the mud preparations are nontoxic in respect to these metals. The order of stability of metal-humate complexes is Cu>Zn>Mg>Fe. The order of affinity of metals to HS fractions obtained have to be extended to other metals of environmental interest. The ability of HSs to bind metals may make them a candidate for natural, environmentally safe substances to concentrate hazardous metals and to remove them from natural water reservoirs.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

Abbreviations

HS:

humic substance

HA:

humic acid

HMA:

hymatomelanic acid

FA:

fulvic acid

SM:

mud of the Baltic Sea

LM:

mud of Lake Ermistu

Sea HA:

humic acid from the mud of the Baltic Sea

Sea HMA:

hymatomelanic acid from the mud of the Baltic Sea

Sea FA:

fulvic acid from the mud of the Baltic Sea

Ac.sea HA:

humic acid from the acid pre-treated mud of the Baltic Sea

Ac.sea HMA:

hymatomelanic acid from the acid pre-treated mud of the Baltic Sea

Ac.sea FA:

fulvic acid from the acid pre-treated mud of the Baltic Sea

Lake HA:

humic acid from the mud of Lake Ermistu

Lake HMA:

hymatomelanic acid from the mud of Lake Ermistu

Lake FA:

fulvic acid from the mud of Lake Ermistu

Ac.lake HA:

humic acid from the acid pre-treated mud of Lake Ermistu

Ac.lake HMA:

hymatomelanic acid from the acid pre-treated mud of Lake Ermistu

Ac.lake FA:

fulvic acid from the acid pre-treated mud of Lake Ermistu

References

  1. Hayes MHB (1998): Humic substances: progress towards more realistic concepts of structures. In: Davis G, Ghabbour EA, Eds, Humic substances: structures, properties and uses. Royal Society of Chemistry, Cambridge, pp. 1–28

    Google Scholar 

  2. Cardellicchio N, Palma A, Montemurro N, Ragone P (1994): Humic and fulvic acid in marine sediments in the Ionian sea (Italy). In: Senesi N, Miano TM, Eds, Humic substances in the global environment and implications for human health. Elsevier, Amsterdam, pp. 819–824

    Google Scholar 

  3. Novák J, Kozler J, Janoš P, Čežiková J, Tokarová V, Madronová L (2001): Humic acids from coals of the North-Bohemian coal field I. Preparation and characterisation. React Funct Polym 47, 101–109

    Article  Google Scholar 

  4. Orlov DS (1990): Soil humic acids and general humification theory. Moskva (In Russian)

  5. Stevenson FJ (1994): Humus chemistry: genesis, composition, reactions, 2nd Edition. Wiley, New York

    Google Scholar 

  6. Hornets T, Koorits A, Peil S, Pärn A, Salm S, Utsal K, Utsal V, Veermäe I (1993): A comparative study of Estonian curative muds. Acta Comm Univ Tartuensis, Publ Chem XXI, 214-229

  7. Shulgin A, Shapovalov A, Putsykin Y, Bobovnikov C, Pleskachevski G, Eckles III AJ (1999): Using activated humic acids in the detoxification of soils contaminated with polychlorinated biphenyls. Tests conducted in the city of Serpukhov, Russia. In: Ghabbour EA, Davies G, Eds, Understanding humic substances: advanced methods, properties and applications. Royal Society of Chemistry, Cambridge, pp.265–270

    Google Scholar 

  8. Peuravuori J, Paaso N, Pihlaja K (2001): Sorption behaviour of some chlorophenols in lake aquatic humic matter. Talanta 56, 523–538

    Article  Google Scholar 

  9. Paciolla MD, Davies G, Jansen SA (1999): Generation of hydroxyl radicals from metal-loaded humic acids. Environ Sci Technol 33, 1814–1818

    Article  CAS  Google Scholar 

  10. Gaffney JS, Marley NA, Clark SB (1996): Humic and fulvic acids and organic colloidal materials in the environment. In: Gaffney JS, Marley NA, Clark SB, Eds, Humic and fulvic acids: isolation, structure and environmental role. American Chemical Society, Washington DC, pp. 2–16

    Google Scholar 

  11. Peuravuori J, Pihlaja K (1997): Molecular size distribution and spectroscopic properties of aquatic humic substances. Anal Chim Acta 337, 133–149

    Article  CAS  Google Scholar 

  12. Goh KM, Reid MR (1975): Molecular weight distribution of soil organic matter as affected by acid pre-treatment and fractionation into humic and fulvic acids. J Soil Sci 26, 207–222

    Article  CAS  Google Scholar 

  13. Klavins M (1997): Aquatic humic substances: characterization, structure and genesis. Riga

  14. Glebova GI (1985): Hymatomelanic acids in soils. Moskva (In Russian)

  15. Belzile N, Joly HA, Li H (1997): Characterization of humic substances extracted from Canadian lake sediments. Can J Chem 75, 14–27

    Article  CAS  Google Scholar 

  16. Abate G, Masini JC (2001): Acid-base and complexation properties of a sedimentary humic acid. A study on the Barra Bonita reservoir of Tietê River, São Paulo State, Brazil. J Braz Chem Soc 12, 109–116

    Article  CAS  Google Scholar 

  17. Ishiwatari R (1985): Geochemistry of humic substances in lake sediments. In: Aiken GR, McKnight DM, Wershaw RL, Maccarthy P, Eds, Humic substances in soil, sediment and water geochemistry, isolation and characterization. Wiley, New York, pp. 147–180

    Google Scholar 

  18. Čežiková J, Kozler J, Madronová L, Novák J, Janoš P (2001): Humic acids from coals of the North-Bohemian coal field II. Metal-binding capacity under static conditions. React Funct Polym 47, 111–118

    Article  Google Scholar 

  19. Chin YP, Aiken G, O’Loughlin E (1994): Molecular weight, poly-dispersity and spectroscopic properties of aquatic humic substances. Environ Sci Technol 28, 1853–1858

    Article  CAS  Google Scholar 

  20. Klavins M, Serzne J, Supe A (1999): Properties of soil and peat humic substances from Latvia. Proc Latvian Acad Sci Section B 53, 249–255

    CAS  Google Scholar 

  21. Jurcsik I (1994) Investigations in the mechanism of electron transmission and active oxygen generating humic acids supported by redoxindicator. In: Senesi N, Miano TM, Eds, Humic substances in the global environment and implications for human health. Elsevier, Amsterdam, pp. 311–316

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Margus Lopp.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Übner, M., Treuman, M., Viitak, A. et al. Properties of humic substances from the baltic sea and lake ermistu mud. J Soils & Sediments 4, 24–29 (2004). https://doi.org/10.1007/BF02990825

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02990825

Keywords

Navigation