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

Springer Science and Business Media LLC - Tập 20 - Trang 1558-1570 - 2019
Zhan Yu1, Yangzhu Zhang1, Hao Sheng1, Liang Zhang1, Qing Zhou1, Xiong Yan2
1College of Resources and Environment, Hunan Agricultural University, Changsha, China
2College of Resources and Environment, Zunyi Normal University, Zunyi, China

Tóm tắt

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. 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 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. 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.

Tài liệu tham khảo

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 149:66–75 Brinkman R (1970) Ferrolysis, a hydromorphic soil forming process. Geoderma 3:199–206 Chang SN (1961) Clay minerals of some representative paddy soils of China. Acta Pedol Sin 9:81–102 (in Chinese) 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 75:1807–1820 Churchman GJ (1980) Clay minerals formed from micas and chlorites in some New Zealand soils. Clay Miner 15:59–76 Churchman GJ (2010) Is the geological concept of clay minerals appropriate for soil science? A literature-based and philosophical analysis. Phys Chem Earth 35:927–940 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 20.1–20.72 CRGCST (Cooperative Research Group on Chinese Soil Taxonomy) (2003) Chinese Soil Taxonomy. Science Press, Beijing and New York Gong ZT (1986) Origin, evolution and classification of paddy soils in China. Adv Soil Sci 5:174–200 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) Gong ZT, Zhang GL, Chen ZC (2007) Pedogenesis and soil taxonomy. Science Press, Beijing (in Chinese) 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 64:435–444 Han W, Hong HL, Yin K et al (2014) Pedogenic alteration of illite in subtropical China. Clay Miner 49:379–390 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 15:423–435 Hong HL (2010) A review on paleoclimate interpretation of clay minerals. Geol Sci Technol Inf 29:1–8 (in Chinese) Hong H, Churchman GJ, Gu Y et al (2012) Kaolinite–smectite mixed-layer clays in the Jiujiang red soils and their climate significance. Geoderma 173–174:75–83 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 214-215:42–49 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 100:1883–1891 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 63:119–131 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 159:0–334 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) 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 76:2078–2088 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 Hunan Agriculture Department (1987) Hunan Soil Species. China Agriculture Press, Beijing (in Chinese) Hunan Agriculture Department (1989) Hunan soil. China Agriculture Press, Beijing (in Chinese) 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) 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 22:3342–3360 Ismail FT (1970) Biotite weathering and clay formation in arid and humid regions, California. Soil Sci 109:257–261 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) Jenny H (1941) Factors of Soil Formation. McGraw-Hill, New York 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 157:1–14 Kyuma K (1978) Mineral composition of rice soils. In: Soils and Rice. IRRI, Los Bafios, pp 219–235 Li QK (1992) Paddy soils of China. Science Press, Beijing (in Chinese) 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 29:813–822 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 12:694–710 Lin CW, Hseu ZY, Chen ZS (2002) Clay mineralogy of Spodosols with high clay contents in the subalpine forests of Taiwan. Clay Clay Miner 50:726–735 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 72:1580–1590 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 Masanori M (1974) Chloritization in lowland paddy soils. Soil Sci Plant Nutr 20:107–116 Pai CW, Wang MK, Chiu CY (2007) Clay mineralogical characterization of a toposequence of perhumid subalpine forest soils in northeastern Taiwan. Geoderma 138:177–184 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 10:79–92 Ponnamperuma FN (1972) The Chemistry of Submerged Soils. Adv Agron 24:29–96 Prakongkep N, Suddhiprakarn A, Kheoruenromne I et al (2010) SEM image analysis for characterization of sand grains in Thai paddy. Geoderma 156:20–31 State Soil Survey Office of Agricultural Ministry (1992) Techniques for Soil Survey of China. China Agriculture Press, Beijing (in Chinese) 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 278:40–48 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 136:51–63 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 81:124–137 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 63:762–772 Wilson MJ (2004) Weathering of the primary rock-forming minerals: processes, products and rates. Clay Miner 39:233–266 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) 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 74:20–27 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 510:140–151 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 157–166 Zhang GL, Gong ZT (2003) Pedogenic evolution of paddy soils in different soil landscapes. Geoderma 115:15–29 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)