Skip to main content

Advertisement

Log in

CLAY MINERALS AS THE KEY TO THE SEQUESTRATION OF CARBON IN SOILS

  • Original Paper
  • Published:
Clays and Clay Minerals

Abstract

Results from earlier laboratory and field experiments were interrogated for the possibilities of sequestration, or long-term accumulation, of carbon from excess greenhouse gases in the atmosphere. In the laboratory study, samples of three (top) soils dominated by kaolinite and illite (together), smectite, and allophane were examined for the adsorption and desorption of dissolved organic carbon (DOC). Adsorption and desorption of DOC were carried out on clay fractions extracted physically and after first native organic matter and then iron oxides were removed chemically. Labeled organic material was added to the soils to assess the priming effect of organic carbon (OC). In the field, changes in OC were measured in sandy soils that had been amended by additions of clay for between 3 and 17 years, both through incorporation of exogenous clay and delving of in situ clay. The laboratory experiments demonstrated that a portion of DOC was held strongly in all soils. The amount of DOC adsorbed depended on clay mineral types, including Fe oxides. Much adsorbed DOC was lost by desorption in water and a substantial amount of native OC was lost on priming with new OC. Addition of clay to soils led to increased OC. Therefore, addition of clay to soil may enhance net sequestration of C. Organic carbon close to mineral surfaces or within microaggregates is held most strongly. Carbon sequestration may occur in subsoils with unsaturated mineral surfaces. However, incorporation of carbon into macroaggregates from enhanced plant growth might be most effective in removing excess carbon from the atmosphere, albeit over the short-term.

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

REFERENCES

  • Bailey, G. & Hughes, B. (2012). An observational study of clay delving and its impact on the A2 horizon in sand over clay soils. Pp 201–210 in: Proceedings of the 5thjoint Australia and New Zealand soil science conference, Hobart. (L.L. Burkitt and L.A. Sparrow, editors). Australian Society of Soil Science Inc.

  • Balesdent, J. (1996). The significance of organic separates to carbon dynamics and its modelling in some cultivated soils. European Journal of Soil Science, 47, 485–493.

    Google Scholar 

  • Balesdent, J., Chenu, C., & Balabane, M. (2000). Relationship of soil organic matter dynamics to physical protection and tillage. Soil & Tillage Research, 53, 215–230.

    Google Scholar 

  • Batjes, N. H. (1996). Total carbon and nitrogen in the soils of the world. European Journal of Soil Science, 47, 151–163.

    Google Scholar 

  • Beare, M. H., Hendrix, P. F., & Coleman, D. C. (1994). Water-stable aggregates and organic matter fractions in conventional and no-tillage soils. Soil Science Society of America Journal, 58, 777–786.

    Google Scholar 

  • Betti, G., Grant, C., Churchman, G., & Murray, R. (2015). Increased profile wettability in texture-contrast soils from clay delving: case studies in South Australia. Soil Research, 53, 125–136.

    Google Scholar 

  • Blakemore, L.C., Searle, P.L., & Daly, B.K. (1987). Methods for chemical analysis of soils. N.Z. Soil Bureau Scientific Report 80.

  • Bolan, N. S., Kunhikrishnan, A., Choppala, G. K., Thangarajan, R., & Chung, J. W. (2012). Stabilization of carbon in composts and biochars in relation to carbon sequestration and soil fertility. Science of the Total Environment, 424, 264–270.

    Google Scholar 

  • Cann, M. A. (2000). Clay spreading on water repellent sands in the south east of South Australia--promoting sustainable agriculture. Journal of Hydrology, 231–232, 333–341.

    Google Scholar 

  • Chabbi, A., Kögel-Knabner, I., & Rumpel, C. (2009). Stabilised carbon in subsoil horizons is located in spatially distinct parts of the soil profile. Soil Biology and Biochemistry, 41, 256–261.

    Google Scholar 

  • Chenu, C., & Plante, A. F. (2006). Clay-sized organo-mineral complexes in a cultivation chronosequence: revisiting the concept of the ‘primary organo-mineral complex’. European Journal of Soil Science, 57, 596–607.

    Google Scholar 

  • Churchman, G. J. (2010). Is the geological concept of clay minerals appropriate for soil science? A literature–based and philosophical analysis. Physics and Chemistry of the Earth, 35, 927–940.

    Google Scholar 

  • Churchman, G.J. (2018). Game changer in soil science. functional role of clay minerals in soil. Journal of Plant Nutrition and Soil Science, 181, 99–103.

  • Churchman, G.J. & Lowe, D.J. (2012). Alteration, formation and occurrence of minerals in soils. Pp. 1–20 in: Handbook of Soil Sciences. Properties and Processes, 2nd edition. (P.M. Huang, Y. Li, and M.E. Sumner, editors). CRC Press, Boca Raton, Florida, USA.

  • Churchman, G. J., & Velde, B. (2019). Soil Clays, Linking Geology, Biology, Agriculture, and the Environment. Boca Raton, Florida, USA: CRC Press.

  • Churchman, G. J., Foster, R. C., D’Acqui, L. P., Janik, L. J., Skjemstad, J. O., Merry, R. H., & Weissmann, D. A. (2010). Effect of land-use history on the potential for carbon sequestration in an Alfisol. Soil & Tillage Research, 109, 23–35.

    Google Scholar 

  • Churchman, J., Hesterberg, D., & Singh, B. (2012). Soil clays (Editorial). Applied Clay Science, 64, 1–3.

    Google Scholar 

  • Churchman, G. J., Noble, A., Bailey, G., Chittleborough, D., & Harper, R. (2014). Clay addition and redistribution to enhance carbon sequestration in soils. In A. E. Hartemink & K. McSweeney (Eds.), Soil Carbon, Progress in Soil Science (pp. 327–335). Switzerland: Springer.

    Google Scholar 

  • Crossley, P. (2001). Clear opportunities for bleaching and clarifying clays. Industrial Minerals, 2001, 69–75.

    Google Scholar 

  • Denef, K., Six, J., Merckx, R., & Paustian, K. (2004). Carbon sequestration in microaggregates of no-tillage soils with different clay mineralogy. Soil Science Society of America Journal, 68, 1935–1944.

    Google Scholar 

  • Dictionary.com (2019). – accessed 12 August 2019

  • Eusterhues, K., Rumpel, C., Kleber, M., & Kőgel-Knabner, I. (2003). Stabilisation of organic matter by interactions with minerals as revealed by mineral dissolution and oxidative degradation. Organic Geochemistry, 34, 1591–1600.

    Google Scholar 

  • Eusterhues, K., Rumpel, C., & Kőgel-Knabner, I. (2005). Stabilization of soil organic matter isolated via oxidative degradation. Organic Geochemistry, 36, 1567–1575.

    Google Scholar 

  • FAO/UNESCO. (1995). Digital soil map of the world and derived properties. Italy: Rome.

    Google Scholar 

  • Finley, B. K., Dijkstra, P., Rasmussen, C., Schwartz, E., Mau, R. L., Liu, X.-J. A., van Gestel, N., & Hungate, B. A. (2018). Soil mineral assemblage and substrate quality effects on microbial priming. Geoderma, 322, 38–47.

    Google Scholar 

  • Golchin, A., Oades, J. M., Skjemstad, J. O., & Clarke, P. (1994). Soil structure and carbon cycling. Australian Journal of Soil Research, 32, 1043–1068.

    Google Scholar 

  • Hall, D. J., Jones, H. R., Crabtree, W. L., & Daniels, T. L. (2010). Claying and deep ripping can increase crop yields and profits on water repellent sands with marginal fertility in southern Western Australia. Australian Journal of Soil Research, 48, 178–187.

    Google Scholar 

  • Harper, R.J., Sochacki, S.J., Bell, R.W., & 7 others (2012). Increasing soil carbon storage in sandy soils with clay amendments. P. 75 in: The CCRSPI (Climate Change Research Strategy for the Primary Industries) conference, Melbourne, 27–29 Nov., 2012

  • Hassink, J. (1997). The capacity of soils to preserve organic C and N by their association with clay and silt particles. Plant and Soil, 191, 77–87.

    Google Scholar 

  • Hinsinger, P., Bengouh, A. G., Vetterlin, D., & Young, I. M. (2009). Rhizosphere: biophysics, biogeochemistry and ecological relevance. Plant and Soil, 321, 117–152.

    Google Scholar 

  • Janzen, H. H. (2006). The soil carbon dilemma: Shall we hoard it or use it? Soil Biology and Biochemistry, 38, 419–424.

    Google Scholar 

  • Kahle, M., Kleber, M., & Jahn, R. (2003). Retention of dissolved organic matter by illitic soils and clay fractions: influence of mineral phase properties. Journal of Plant Nutrition and Soil Science, 166, 737–741.

    Google Scholar 

  • Kahle, M., Kleber, M., & Jahn, R. (2004). Retention of dissolved organic matter by phyllosilicate and soil clay fractions in relation to mineral properties. Organic Geochemistry, 35, 269–276.

    Google Scholar 

  • Kaiser, K., & Guggenberger, G. (2003). Mineral surfaces and soil organic matter. European Journal of Soil Science, 54, 219–236.

    Google Scholar 

  • Kleber, M., Sollins, P., & Sutton, R. (2007). A conceptual model of organo-mineral interactions in soils: self-assembly of organic molecular fragments into zonal structures on mineral surfaces. Biogeochemistry, 85, 9–24.

    Google Scholar 

  • Kleber, M., Eusterhues, K., Keiluweit, M., Mikutta, C., Mikutta, R., & Nico, P. S. (2015). Mineral-organic associations: formation, properties, and relevance in soil environments. Advances in Agronomy, 130, 1–140.

    Google Scholar 

  • Lal, R. (2004). Soil carbon sequestration impacts on global climate change and food security. Science, 304, 1623–1627.

    Google Scholar 

  • Lal, R. (2014). Soil carbon management and climate change. In A. E. Hartemink & K. McSweeney (Eds.), Soil Carbon, Progress in Soil Science (pp. 339–361). Switzerland: Springer.

    Google Scholar 

  • Le Quéré, C., Raupach, M. R., Canadell, J. G., et al. (2009). Trends in the sources and sinks of carbon dioxide. Nature Geoscience, 2, 831–836.

    Google Scholar 

  • Liefeld, J., & Kögel-Knabner, I. (2003). Microaggregates in agricultural soils and their size distribution determined by X-ray attenuation. European Journal of Soil Science, 54, 167–174.

    Google Scholar 

  • Lorenz, K., & Lal, R. (2005). The depth distribution of soil organic carbon in relation to land use and management and the potential of carbon sequestration in subsoil horizons. Advances in Agronomy, 88, 35–66.

    Google Scholar 

  • Luo, Z., Wang, E., & Sun, O. J. (2010). Can no-tillage stimulate carbon sequestration in agricultural soils? A meta-analysis of paired experiments. Agriculture, Ecosystems and Environment, 139, 224–231.

    Google Scholar 

  • Mayer, L. M., & Xing, B. (2001). Organic matter-surface area relationships in acid soils. Soil Science Society of America Journal, 65, 250–258.

    Google Scholar 

  • McCarthy, J. F., Ilavsky, J., Jastrow, J. D., Mayer, L. M., Perfect, E., & Zhuang, J. (2008). Protection of organic carbon in soil microaggregates via restructuring of aggregate porosity and filling of pores with accumulating organic matter. Geochimica et Cosmochimica Acta, 72, 4725–4744.

    Google Scholar 

  • McKissock, I., Gilkes, R. J., & Walker, E. L. (1998). The reduction of water repellency by added clay is influenced by clay and soil properties. Applied Clay Science, 20, 225–239.

    Google Scholar 

  • Michéli, E. & Spaargaren, O.C. (2012). Other systems of soil classification. Pp. 32–1–32-34 in: Handbook of Soil Sciences. Properties and Processes, 2nd edition (P.M. Huang, Y. Li and M.E. Sumner, editors). CRC Press, Boca Raton, Florida.

  • Mikutta, R., Kleber, M., & Jahn, R. (2005). Poorly crystalline minerals protect organic carbon in clay subfractions from acid subsoil horizons. Geoderma, 128, 106–115.

    Google Scholar 

  • Mikutta, R., Mikutta, C., Kalbitz, K., Scheel, T., Kaiser, K., & Jahn, R. (2007). Biodegradation of forest floor organic matter bound to minerals via different binding mechanisms. Geochimica et Cosmochimica Acta, 71, 2569–2590.

    Google Scholar 

  • Minasny, B., Malone, B. P., McBratney, A. B., et al. (2017). Soil carbon 4 per mille. Geoderma, 292, 59–86.

    Google Scholar 

  • Noble, A. D., Gillman, G. P., Nath, S., & Srivastava, R. J. (2001). Changes in the surface charge characteristics of degraded soils in the wet tropics through the addition of beneficiated bentonite. Australian Journal of Soil Research, 39, 991–1001.

    Google Scholar 

  • Oades, J. M. (1984). Soil organic matter and structural stability: mechanisms and implications for management. Plant and Soil, 76, 319–337.

    Google Scholar 

  • Oades, J.M. (1989). Introduction to organic matter in mineral soils. Pp. 89–159 in: Minerals in Soil Environments (J.B. Dixon and S.B. Weed, editors). 2nd edition, Soil Science Society of America Inc., Madison, Wisconsin, USA.

  • Paradelo, R., van Oort, F., Barré, P., Billiou, D., & Chenu, C. (2016). Soil organic matter stabilization at the pluri-decadal scale: Insight from bare fallow soils with contrasting physicochemical properties and macrostructures. Geoderma, 275, 48–54.

    Google Scholar 

  • Percival, H. J., Parfitt, R. L., & Scott, N. A. (2000). Factors controlling soil carbon levels in New Zealand grasslands: Is clay content important? Soil Science Society of America Journal, 64, 1623–1630.

    Google Scholar 

  • Powlson, D. S., Whitmore, A. P., & Goulding, K. W. T. (2011). Soil carbon sequestration to mitigate climate change: a critical re-examination to identify the true and the false. European Journal of Soil Science, 62, 42–55.

    Google Scholar 

  • Puget, P., Chenu, C., & Balesdent, J. (2000). Dynamics of soil organic matter associated with particle-size fractions of water-stable aggregates. European Journal of Soil Science, 51, 595–605.

    Google Scholar 

  • Rasmussen, C., Matsuyama, N., Dahlgren, R. A., Southard, R. J., & Brauer, N. (2007). Soil genesis and mineral transformation across and environmental gradient on andesitic lahar. Soil Science Society of America Journal, 71, 225–237.

    Google Scholar 

  • Rowley, M. C., Grand, S., & Verrecchia, E. P. (2018). Calcium-mediated stabilization of soil organic carbon. Biogeochemistry, 137, 27–49.

    Google Scholar 

  • Saggar, S., Parshotam, A., Sparling, G. P., Feltham, C. W., & Hart, P. B. S. (1996). 14C-labelled ryegrass turnover and residence times in soils varying in clay content and mineralogy. Soil Biology and Biochemistry, 28, 1677–1686.

    Google Scholar 

  • Saidy, A. R., Smernik, R. J., Baldock, J. A., Kaiser, K., Sanderman, J., & Macdonald, L. M. (2012). Effects of clay mineralogy and hydrous iron oxides on labile organic carbon stabilisation. Geoderma, 173, 104–110.

    Google Scholar 

  • Saidy, A. R., Smernik, R. J., Baldock, J. A., Kaiser, K., & Sanderman, J. (2013). The sorption of organic carbon onto differing clay minerals in the presence and absence of hydrous iron oxide. Geoderma, 209, 15–21.

    Google Scholar 

  • Salomé, C., Nunan, N., Pouteau, V., Lerch, T. Z., & Chenu, C. (2010). Carbon dynamics in topsoil and in subsoil may be controlled by different regulatory mechanisms. Global Change Biology, 16, 416–426.

    Google Scholar 

  • Sarkar, B., Singh, M., Mandal, S., Churchman, G.J., & Bolan, N.S. (2018). Clay minerals—organic matter interactions in relation to carbon stabilization in soils. Pp. 71–86 in: The Future of Soil Carbon: Its Conservation and Formation (C. Garcia, P. Nannipieri, and T. Hernandez, editors). New York: Academic Press.

  • Schapel, A., Marschner, P., & Churchman, J. (2018). Clay amount and distribution influence organic carbon content in sand with subsoil clay addition. Soil & Tillage Research, 184, 253–260.

    Google Scholar 

  • Schöning, I., Knicker, H., & Kőgel-Knabner, I. (2005). Intimate association between O/N-alkyl carbon and iron oxides in clay fractions of forest soils. Organic Geochemistry, 36, 1378–1390.

    Google Scholar 

  • Schuur, E. A. G., & Abbott, B. W. (2011). High risk of permafrost thaw. Nature, 480, 32–33.

    Google Scholar 

  • Singh, M. (2016). Role of clay minerals in carbon stabilisation in soils. Unpublished PhD Thesis, University of South Australia.

  • Singh, M., Sarkar, B., Biswas, B., Churchman, J., & Bolan, N. S. (2016). Adsorption-desorption behavior of dissolved organic carbon by soil clay fractions of varying mineralogy. Geoderma, 280, 47–56.

    Google Scholar 

  • Singh, M., Sarkar, B., Biswas, B., Bolan, N. S., & Churchman, G. J. (2017a). Relationship between soil clay mineralogy and carbon protection capacity as influenced by temperature and moisture. Soil Biology and Biochemistry, 109, 95–106.

    Google Scholar 

  • Singh, M., Sarkar, B., Hussain, S., Ok, Y. S., Bolan, N. S., & Churchman, G. J. (2017b). Influence of physico-chemical properties of soil clay fractions on the retention of dissolved organic carbon. Environmental Geochemistry and Health, 39, 1335–1350.

    Google Scholar 

  • Singh, M., Sarkar, B., Sarkar, S., Churchman, J., Bolan, N., Mandal, S., Menon, M., Purakayastha, T. J., & Beerling, D. J. (2018). Stabilization of soil organic carbon as influenced by clay mineralogy. Advances in Agronomy, 148, 33–84.

    Google Scholar 

  • Singh, M., Sarkar, B., Bolan, N. S., Ok, Y. S., & Churchman, G. J. (2019). Decomposition of soil organic matter as affected by clay types, pedogenic oxides and plant residue addition rates. Journal of Hazardous Materials, 374, 11–19.

    Google Scholar 

  • Six, J., Elliott, E. T., & Paustian, K. (1999). Aggregate and soil organic dynamics under conventional and no-tillage systems. Soil Science Society of America Journal, 63, 1350–1359.

    Google Scholar 

  • Six, J., Conant, R. T., Paul, E. A., & Paustian, K. (2002). Stabilization mechanisms of soil organic matter: implications for C-saturation of soils. Plant and Soil, 241, 155–176.

    Google Scholar 

  • Six, J., Bossuyt, H., Degryze, S., & Denef, K. (2004). A history of research on the link between (micro)aggregates, soil biota, and soil organic matter dynamics. Soil & Tillage Research,79, 7–31.

  • Smith, P., Martino, D., Cai, Z., et al. (2008). Greenhouse gas mitigation in agriculture. Philosophical Transactions of the Royal Society B, 363, 789–813.

    Google Scholar 

  • Soda, W., Noble, A. D., Suzuki, S., Simmons, R., Sindhusen, L., & Bhuthornharaj, S. (2006). Composting of acid waste bentonites and their effects on soil properties and crop biomass. Journal of Environmental Quality, 35, 2293–2301.

    Google Scholar 

  • Soil Survey Staff (1975). Soil taxonomy: A basic system of soil classification for making and interpreting soil surveys. U.S. Dept. of Agriculture Soil Conservation Service, Washington, D.C.

  • Spain, A. V. (1990). Influence of environmental conditions and some soil chemical properties on the carbon and nitrogen contents of some typical Australian rainforest soils. Australian Journal of Soil Research, 28, 825–839.

    Google Scholar 

  • Stewart, C. E., Paustian, K., Conant, R. T., Plante, A. F., & Six, J. (2007). Soil carbon saturation: concept, evidence and evaluation. Biogeochemistry, 86, 19–31.

    Google Scholar 

  • Stewart, C. E., Plante, A. F., Paustian, K., Conant, R. T., & Six, J. (2008). Soil carbon saturation: linking concept and measurable carbon pools. Soil Science Society of America Journal, 72, 379–392.

    Google Scholar 

  • Stockmann, U., Adams, M. A., Crawford, J. W., et al. (2013). The knowns, known unknowns and unknowns of sequestration of soil organic carbon. Agriculture, Ecosystems and Environment, 164, 80–99.

    Google Scholar 

  • Tisdall, J. M., & Oades, J. M. (1982). Organic matter and water-stable aggregates in soils. Journal of Soil Science, 33, 141–163.

    Google Scholar 

  • Totsche, K. U., Amelung, W., Gerzabeck, M. H., et al. (2018). Microaggregates in soils. Journal of Plant Nutrition and Soil Science, 181, 104–136.

    Google Scholar 

  • Virto, I., Moni, C., Swanston, C., & Chenu, C. (2010). Turnover of intra- and extra-aggregates organic matter at the silt scale. Geoderma, 156, 1–10.

    Google Scholar 

  • Vogel, C., Mueller, C. W., Hőschen, C., et al. (2014). Submicron structures provide preferential spots for carbon and nitrogen sequestration in soils. Nature Communications, 5, 2947.

    Google Scholar 

  • West, T. O., & Six, J. (2007). Considering the influence of sequestration duration and carbon saturation on estimates of soil carbon capacity. Climatic Change, 80, 25–41.

    Google Scholar 

Download references

CONFLICTS OF INTEREST

On behalf of all authors, the corresponding author states that there is no conflict of interest.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Gordon Jock Churchman.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Churchman, G.J., Singh, M., Schapel, A. et al. CLAY MINERALS AS THE KEY TO THE SEQUESTRATION OF CARBON IN SOILS. Clays Clay Miner. 68, 135–143 (2020). https://doi.org/10.1007/s42860-020-00071-z

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s42860-020-00071-z

Keywords

Navigation