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Composition of clay minerals and their pedogenetic and taxonomic implications for Stagnic Anthrosols derived from different parent materials in Hunan Province, China

  • Zhan Yu
  • Yangzhu ZhangEmail author
  • Hao Sheng
  • Liang Zhang
  • Qing Zhou
  • Xiong Yan
Soils, Sec 5 • Soil and Landscape Ecology • Research Article
  • 12 Downloads

Abstract

Purpose

The aims of this study were to investigate the composition of clay minerals in soils derived from different parent materials and to elucidate how parent materials and pedogenic environment affect the distribution of clay minerals and reveal the implications for pedogenetics and taxonomy in Stagnic Anthrosols.

Materials and methods

Clay mineralogy and physicochemical properties of the Hydragric horizon of Stagnic Anthrosols derived from granite (GR), plate shale (PS), quaternary red clays (QRC), limestone (LS), purple sandy shale (PSS) and fluvial-lacustrine deposit (FLD) located in Hunan Province of China were analysed to explore the relationships between the conditions influencing the formation of the soil and the composition of clay minerals.

Results and discussion

Results indicated that the composition of clay minerals is closely related to both parent material and type of Stagnic Anthrosols: the soils derived from GR, PS and QRC, which are mostly classified as Fe-accumulic-Stagnic Anthrosols, are dominantly 1:1 type kaolinite and vermiculite and illite/vermiculite mixed layer minerals of widespread distribution. However, soils derived from LS, PSS and FLD were mainly classified as Hapli-Stagnic Anthrosols and are mainly composed of 2:1 type illite/smectite mixed layer minerals, where chlorite is commonly found. Illite is widely distributed and its content varies the least among different parent materials. An extremely significant relationship between pH and kaolinite, chlorite and mixed layer minerals was noted, and the two kinds of mixed layer minerals showed highly significant negative correlation.

Conclusions

This study revealed that the types and quantities of clay minerals in the soil are closely related to the types of parent material. This reflected better direction and degree of development in Stagnic Anthrosols, which is related to the physicochemical properties of parent material and can be used as one of the bases for the classification of soil groups and subgroups within the soil family for Stagnic Anthrosols in Chinese Soil Taxonomy.

Keywords

Clay minerals Hydragric horizon Parent materials Pedogenic environment Soil group Stagnic Anthrosols 

Notes

Funding information

This research was supported by the Basic Work of the Ministry of Science and Technology of China (grant no. 2014FY110200), the National Natural Science Foundation of China (grant no. 41571234), and the Project of Key Laboratory of Soil Resources and Environment in Qianbei of Guizhou Province (grant no. Qian Jiao He KY zi[2017]010).

Compliance with ethical standards

Conflict of interest

The authors declare that they have no conflict of interest.

References

  1. Bonifacio E, Falsone G, Simonov G, Sokolova T, Tolpeshta I (2009) Pedogenic processes and clay transformations in bisequal soils of the Southern Taiga zone. Geoderma 149:66–75CrossRefGoogle Scholar
  2. Brinkman R (1970) Ferrolysis, a hydromorphic soil forming process. Geoderma 3:199–206CrossRefGoogle Scholar
  3. Chang SN (1961) Clay minerals of some representative paddy soils of China. Acta Pedol Sin 9:81–102 (in Chinese)Google Scholar
  4. Chen LM, Zhang GL, Effland WR (2011) Soil characteristic response times and pedogenic thresholds during the 1000-year evolution of a paddy soil chronosequence. Soil Sci Soc Am J 75:1807–1820CrossRefGoogle Scholar
  5. Churchman GJ (1980) Clay minerals formed from micas and chlorites in some New Zealand soils. Clay Miner 15:59–76CrossRefGoogle Scholar
  6. Churchman GJ (2010) Is the geological concept of clay minerals appropriate for soil science? A literature-based and philosophical analysis. Phys Chem Earth 35:927–940CrossRefGoogle Scholar
  7. Churchman GJ, Lowe DJ (2012) Alteration, formation, and occurrence of minerals in soils. In: Huang PM, Li Y, Sumner ME (eds) Handbook of Soil Sciences, vol 1, 2nd edn. CRC Press. Properties and Processes, Boca Raton, pp 20.1–20.72Google Scholar
  8. CRGCST (Cooperative Research Group on Chinese Soil Taxonomy) (2003) Chinese Soil Taxonomy. Science Press, Beijing and New YorkGoogle Scholar
  9. Gong ZT (1986) Origin, evolution and classification of paddy soils in China. Adv Soil Sci 5:174–200Google Scholar
  10. Gong ZT, Chen ZC, Shi XZ, Zhang GL, Zhang JM, Zhao WJ et al (1999) Chinese soil taxonomy:theory, methodology and practice. Science Press, Beijing (in Chinese)Google Scholar
  11. Gong ZT, Zhang GL, Chen ZC (2007) Pedogenesis and soil taxonomy. Science Press, Beijing (in Chinese)Google Scholar
  12. Han GZ, Zhang GL (2013) Changes in magnetic properties and their pedogenetic implications for paddy soil chronosequences from different parent materials in South China. Eur J Soil Sci 64:435–444CrossRefGoogle Scholar
  13. Han W, Hong HL, Yin K et al (2014) Pedogenic alteration of illite in subtropical China. Clay Miner 49:379–390CrossRefGoogle Scholar
  14. Han GZ, Zhang GL, Li DC et al (2015) Pedogenetic evolution of clay minerals and agricultural implications in three paddy soil chronosequences of south china derived from different parent materials. J Soils Sediments 15:423–435CrossRefGoogle Scholar
  15. Hong HL (2010) A review on paleoclimate interpretation of clay minerals. Geol Sci Technol Inf 29:1–8 (in Chinese)Google Scholar
  16. Hong H, Churchman GJ, Gu Y et al (2012) Kaolinite–smectite mixed-layer clays in the Jiujiang red soils and their climate significance. Geoderma 173–174:75–83CrossRefGoogle Scholar
  17. Hong H, Churchman GJ, Yin K et al (2014) Randomly interstratified illite–vermiculite from weathering of illite in red earth sediments in Xuancheng, southeastern China. Geoderma 214-215:42–49CrossRefGoogle Scholar
  18. Hong H, Cheng F, Yin K et al (2015) Three-component mixed-layer illite/smectite/kaolinite (I/S/K) minerals in hydromorphic soils, south China. Am Mineral 100:1883–1891CrossRefGoogle Scholar
  19. Hseu ZY, Zehetner F, Ottner F et al (2015) Clay-mineral transformations and heavy-metal release in paddy soils formed on serpentinites in Eastern Taiwan. Clay Clay Miner 63:119–131CrossRefGoogle Scholar
  20. Hu XF, Wei J, Du Y et al (2010) Regional distribution of the Quaternary Red Clay with aeolian dust characteristics in subtropical China and its paleoclimatic implications. Geoderma 159:0–334CrossRefGoogle Scholar
  21. Huang LM (2014) Phosphorus and Iron Geochemistry during Paddy Soil Development on Calcareous and Acid Parent Materials Using a Chronosequence Apporach. Ph.D. thesis, Institute of Soil Science, Chinese Academy of Soil Sciences, Nanjing, China (in Chinese)Google Scholar
  22. Huang LM, Zhang GL, Thompson A et al (2013) Pedogenic transformation of phosphorus during paddy soil development on calcareous and acid parent materials. Soil Sci Soc Am J 76:2078–2088CrossRefGoogle Scholar
  23. Huang LM, Jia X, Shao M et al (2018) Phases and rates of iron and magnetism changes during paddy soil development on calcareous marine sediment and acid Quaternary red-clay. Sci Rep.  https://doi.org/10.1038/s41598-017-18963-x
  24. Hunan Agriculture Department (1987) Hunan Soil Species. China Agriculture Press, Beijing (in Chinese)Google Scholar
  25. Hunan Agriculture Department (1989) Hunan soil. China Agriculture Press, Beijing (in Chinese)Google Scholar
  26. Hunan Provincial Institute of Cultural Relics and Archaeology (2006) Hunan provincial institute of cultural relics and archaeology, Pengtoushan and Bashidang, vol 2 vols. Science Press, Beijing (in Chinese)Google Scholar
  27. Hussain S, Peng S, Fahad S, Khaliq A, Huang J, Cui K, Nie K (2015) Rice management interventions to mitigate greenhouse gas emissions: a review. Environ Sci Pollut Res 22:3342–3360CrossRefGoogle Scholar
  28. Ismail FT (1970) Biotite weathering and clay formation in arid and humid regions, California. Soil Sci 109:257–261CrossRefGoogle Scholar
  29. ISSAS (Institute of Soil Science, Chinese Academy of Sciences) (1978) Methods for soil physical and chemical analysis. Shanghai Science and Technology Press, Shanghai (in Chinese)Google Scholar
  30. Jenny H (1941) Factors of Soil Formation. McGraw-Hill, New YorkCrossRefGoogle Scholar
  31. Kögel-Knabner I, Amelung W, Cao Z, Fiedler S, Frenzel P, Jahn R, Kalbitz K, Kölbl A, Schloter M (2010) Biogeochemistry of paddy soils. Geoderma 157:1–14CrossRefGoogle Scholar
  32. Kyuma K (1978) Mineral composition of rice soils. In: Soils and Rice. IRRI, Los Bafios, pp 219–235Google Scholar
  33. Li QK (1992) Paddy soils of China. Science Press, Beijing (in Chinese)Google Scholar
  34. Li FC, Jin ZD, Xie CR et al (2007) Roles of sorting and chemical weathering in the geochemistry and magnetic susceptibility of Xiashu loess, East China. J Asian Earth Sci 29:813–822CrossRefGoogle Scholar
  35. Liao YL, Zheng SX, Nie J et al (2013) Long-term effect of fertilizer and rice straw on mineral composition and potassium adsorption in a reddish paddy soil. J Integr A Gr 12:694–710CrossRefGoogle Scholar
  36. Lin CW, Hseu ZY, Chen ZS (2002) Clay mineralogy of Spodosols with high clay contents in the subalpine forests of Taiwan. Clay Clay Miner 50:726–735CrossRefGoogle Scholar
  37. Liu YL, Zhang B, Li CL, Hu F, Velde B (2008) Long-term fertilization influences on clay mineral composition and ammonium adsorption in a rice paddy soil. Soil Sci Soc Am J 72:1580–1590CrossRefGoogle Scholar
  38. Martin JD (2004) Using XPowder: A Software Package for Powder X-ray Diffraction Analysis. www.xpowder.com D.L. GR 1001/04.ISBN 84-609-1497-6. 105 p
  39. Masanori M (1974) Chloritization in lowland paddy soils. Soil Sci Plant Nutr 20:107–116CrossRefGoogle Scholar
  40. Pai CW, Wang MK, Chiu CY (2007) Clay mineralogical characterization of a toposequence of perhumid subalpine forest soils in northeastern Taiwan. Geoderma 138:177–184CrossRefGoogle Scholar
  41. Pan G, Li L, Wu L, Zhang X (2004) Storage and sequestration potential of topsoil organic carbon in China’s paddy soils. Global Chang Biol 10:79–92CrossRefGoogle Scholar
  42. Ponnamperuma FN (1972) The Chemistry of Submerged Soils. Adv Agron 24:29–96CrossRefGoogle Scholar
  43. Prakongkep N, Suddhiprakarn A, Kheoruenromne I et al (2010) SEM image analysis for characterization of sand grains in Thai paddy. Geoderma 156:20–31CrossRefGoogle Scholar
  44. State Soil Survey Office of Agricultural Ministry (1992) Techniques for Soil Survey of China. China Agriculture Press, Beijing (in Chinese)Google Scholar
  45. Vogelsang V, Kaiser K, Wagner FE, Jahn R, Fiedler S (2016) Transformation of clay-sized minerals in soils exposed to prolonged regular alternation of redox conditions. Geoderma 278:40–48CrossRefGoogle Scholar
  46. Watanabe T, Funakawa S, Kosaki T (2006) Clay mineralogy and its relationship to soil solution composition in soils from different weathering environments of humid Asia: Japan, Thailand and Indonesia. Geoderma 136:51–63CrossRefGoogle Scholar
  47. Watanabe T, Hasenaka Y, Hartono A, Sabiham S, Nakao A, Funakawa S (2017) Parent materials and climate control secondary mineral distributions in soils of Kalimantan, Indonesia. Soil Sci Soc Am J 81:124–137CrossRefGoogle Scholar
  48. Weber J, Tyszka R, Kocowicz A et al (2012) Mineralogical composition of the clay fraction of soils derived from granitoids of the Sudetes and Fore-Sudetic Block, southwest Poland. Eur J Soil Sci 63:762–772CrossRefGoogle Scholar
  49. Wilson MJ (2004) Weathering of the primary rock-forming minerals: processes, products and rates. Clay Miner 39:233–266CrossRefGoogle Scholar
  50. Xu XM, Qin LH, Yang H (2014) Clay mineral composition of diagnostic horizons in stagnic anthrosols: Implications for soil taxonomic classification. Chin J Soil Sci 45:265–271 (in Chinese)Google Scholar
  51. Yin K, Hong H, Churchman GJ et al (2013) Hydroxy-interlayered vermiculite genesis in Jiujiang late-Pleistocene red earth sediments and significance to climate. Appl Clay Sci 74:20–27CrossRefGoogle Scholar
  52. Yin K, Hong H, Churchman GJ et al (2018) Mixed-layer illite-vermiculite as a paleoclimatic indicator in the Pleistocene red soil sediments in Jiujiang, southern China. Palaeogeogr Palaeocl 510:140–151CrossRefGoogle Scholar
  53. Yuan J (2002) Rice and pottery 10 000 yrs. BP at Yuchanyan, Dao county, Hunan province. In: Yasuda Y (ed) The origins of pottery and agriculture. Roli Books, New Delhi, pp 157–166Google Scholar
  54. Zhang GL, Gong ZT (2003) Pedogenic evolution of paddy soils in different soil landscapes. Geoderma 115:15–29CrossRefGoogle Scholar
  55. Zhang GL, Wang QB, Zhang FR et al (2013) Criteria for establishment of soil family and soil series in Chinese Soil Taxonomy. Acta Pedol Sin 50:826–834 (in Chinese)Google Scholar

Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  1. 1.College of Resources and EnvironmentHunan Agricultural UniversityChangshaChina
  2. 2.College of Resources and EnvironmentZunyi Normal UniversityZunyiChina

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