Correlation of soil organic carbon and nutrients (NPK) to soil mineralogy, texture, aggregation, and land use pattern

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• 作者：Gopi Adhikari ; Krishna G. Bhattacharyya
• 关键词：Soil mineralogy ; Soil organic carbon ; Soil nutrients ; Soil aggregation ; Land use pattern
• 刊名：Environmental Monitoring and Assessment
• 出版年：2015
• 出版时间：November 2015
• 年：2015
• 卷：187
• 期：11
• 全文大小：1,442 KB
• 参考文献：Almond, C. (2004). Basic research on the origin and molecular structure of forms stable organic matter relating to the process of abduction soil organic carbon. Edaphology, 11(2), 229–248.
  Anderson, D. W. (1988). The effect of parent material and soil development on nutrient cycling in temperature ecosystems. Biogeochemistry, 5, 71–97.CrossRef
  Baruah, T. C., & Barthakur, H. P. (1997). A textbook of soil analysis, vikash publishing house Pvt. Ltd: New Delhi ISBN 978–81-259-0366-6.
  Bruun, T. B., Elberling, B., & Christensen, B. T. (2010). Lability of soil organic carbon in tropical soils with different clay minerals. Soil Biology & Biochemistry, 42, 888–895.CrossRef
  Cheshire, M. V., Fraser, A. R., Hillier, S., Dumat, C., & Staunton, S. (2000). The interactions between soil organic matter and soil clay minerals by selective removal and controlled addition of organic matter. European Journal of Soil Science, 51, 497–509 Online. doi:10.​1111/​j.​13652389.​2000.​00325.​x .CrossRef
  Chorover, J., & Amistadi, M. K. (2001). Reaction of forest floor organic matter at goethite, birnessite and smectite surfaces. Geochimica et Cosmochimica Acta, 65, 95–109.CrossRef
  Conceição, P. C., Dieckow, J., & Bayer, C. (2013). Combined role of no-tillage and cropping systems in soil carbon stocks and stabilization. Soil & Tillage Research, 129, 40–47.CrossRef
  Davarcioglu, B. (2011). Spectral characterization of non-clay minerals found in the clays (Central Anatolian-Turkey). International Journal of the Physical Sciences, 6(3), 511–522 Available online at http://www.​academicjournals​.​org/​IJPS , ISSN 1992 - 1950 ©2011 Academic Journals.
  Diko, M. L., & Ekosse, G. E. (2012). Physicochemical and mineralogical considerations of Ediki sandstone-hosted kaolin occurrence, South West Cameroon. International Journal of the Physical Sciences, 7(3), 501–507.
  Feller, C., & Beare, M. H. (1997). Physical control of soil organic matter dynamics in the tropics. Geoderma, 79, 69–116.CrossRef
  Franzluebbers, A. J., Haney, R. L., Hongs, F. M., & Zuberer, D. A. (1996). Active fractions of organic matter in soils with different texture. Soil Biololgy & Biochemhemistry, 28, 1367–1372.CrossRef
  Galantini, J. A., Senesi, N., Brunetti, G., & Rosell, R. (2004). Influence of texture on organic matter distribution and quality and nitrogen and sulphur status in semiarid Pampean grassland soils of Argentina. Geoderma, 123, 143–152.CrossRef
  Golchin, A., Oades, J. M., Skjemstad, J. O., & Clarke, P. (1994). Soil structure and carbon cycling. Australian Journal of Soil Research, 32, 1043–1068.CrossRef
  Harris, W., & White, G. N. (2008). Methods of Soil Analysis Part 5—Mineralogical Methods, Chapter 4 (pp.81–116). In A. L. Ulery, & L. R. Drees (Eds.), X-ray diffraction techniques for soil mineral identification. Madison, Wisconsin, USA: Soil Science Society of America, Inc.CrossRef
  Hasse, P. R. (1994). A textbook of soil analysis, 1st Indian reprint, CBS Publishers and Distributors Pvt. New Delhi: Ltd ISBN 978–81-239-1833-4.
  Hassink, J., Neutel, J., & deRuiter, P. C. (1994). C and N mineralization in sandy and loamy grassland soils: the role of microbes and microfauna. SoilBiology & Biochemistry, 26, 1565–1571.CrossRef
  Heine, K., & Völkel, J. (2010). Soil Clay minerals in Namibia and their significance for the terrestrial and marine past global change research. African Study Monographs Suppl, 40, 31–50 URL: jambo.africa.kyoto-u.ac.jp/kiroku/asm_suppl/abstracts/pdf/.../Heine.pdf. Accessed on 6 th November, 2014.
  Hua, K., Wang, D., Guo, X., & Guo, Z. (2014). Carbon sequestration efficiency of organic ammendments in a long-term experiment on a vertisol in Huang-HaiHai Plain in China. PloS One. doi:10.​1371/​journal.​pone.​0108594 .
  Huang, P.-M., Wang, M.-K., & Chiu, C.-Y. (2005). Soil mineral–organic matter–microbe interactions: impacts on biogeochemical processes and biodiversity in soils. Pedobiologia, 49, 609–635.CrossRef
  Igwe, C. A., Zarei, M., & Stahr, K. (2013). Stability of aggregates of some weathered soils in south-eastern Nigeria in relation to their geochemical properties. Journal of Earth System Science, 122(5), 1283–1294.CrossRef
  Kaiser, K., Eusterhues, K., Rumpel, C., Guggenberger, G., & Kögel-Knabner, I. (2002). Stabilization of organic matter by soil minerals-investigations of density and particle-size fractions from two acid forest soils. Journal of Plant Nutrition & Soil Science, 165, 451–459.CrossRef
  Kirkby, C. A., Richardson, A. E., Wade, L. J., Passioura, J. B., Batten, G. D., Blanchard, C., et al. (2014). Nutrient availability limits carbon sequestration in arable soils. Soil Biology & Biochemistry., 68, 402–409. doi:10.​1016/​j.​soilbio.​2013.​09.​032 .CrossRef
  Kögel-Knabner, I., Guggenberger, G., Kleber, M., Kandeler, E., Kalbitz, K., Scheu, S., et al. (2008). Review article, organo-mineral associations in temperate soils:integrating biology, mineralogy, and organic matter chemistry. Journal of Plant Nutrition & Soil Science, 171, 61–82.CrossRef
  Ladd, J. N., Foster, R. C., & Skjemstad, J. O. (1993). Soil structure: carbon and nitrogen metabolism. In: L. Brussaard, L. & Kooistra, M.J.(Ed.) Int. Workshop on methods of research on soil structure/soil biota interrelationships. Geoderma, 56, 401–434.CrossRef
  Madejovà, J. N., & Komadel, P. (2001). Baseline studies of the clay minerals society source clays: infrared methods. Clays and Clay Minerals, 49, 410–432.CrossRef
  Nayak, P. S., & Singh, B. K. (2007). Instrumental characterisation of clay by XRF, XRD and FTIR. Bulletin Mater Science, 30(3), 235–238.CrossRef
  Oades, J. (1988). The retention of organic matter in soils. Biogeochemistry, 5, 35–70.CrossRef
  Olphen, V. H., & Fripiat, J. J. (1979). Data handbook for clay materials and other non-metallic minerals, 1st edition, pergamon press. Oxford: UK.
  Peng, X., Yan, X., Zhou, H., Zhang, Y. Z., & Sun, H. (2015). Assessing the contributions of sesquioxides and soil organic matter to aggregation in an ultisol under long-term fertilization. Soil & Tillage Research, 146, 89–98.CrossRef
  Pironon, J., Pelletier, M., Donato, P. D., & Mosser-Ruck, R. (2003). Characterization of smectite and illite by FTIR spectroscopy of interlayer NH4+ cations. Clay Minerals, 38, 201–211.CrossRef
  Rabbi, S.M.F., Lockwood, P.V., Daniel, H. (2010). How do microaggregates stabilize soil organic matter? © 2010 19th World Congress of Soil Science, Soil Solutions for a Changing World 1–6 August 2010, Brisbane, Australia. pp 109–112, Published on DVD. URL:http://​www.​iuss.​org/​ 19th%20WCSS/Symposium/pdf/1617. Accessed on 26 March, 2014.
  Ravisankar, R., Senthikumar, G., Kiruba, S., Chandrasekaran, A., & Jebakumar, P. P. (2010). Mineral analysis of costal sediments of Tuna, Gujrat, India. Indian Journal of Science and Technology, 3(7), 774–780.
  Sarkar, D., & Halder, A. (2010). Physical and chemical methods in soil analysis (2nd ed., ). New Age International Publishers: New Delhi ISBN 978–81-224-2725-7.
  Schraenbroch, B. C., Lloyd, J. E., & Maynard, J. L. J. (2005). Distinguishing urban soils with physical, chemical and biological properties. Pedobiologia, 49, 283–296.CrossRef
  Schroeder, P. A. (2002). Infrared spectroscopy in clay science. In A. Rule, & S. Guggenheim (Eds.), CMS Workshop Lectures, Teaching Clay Science (vol. 11, pp. 181–206). The Clay Mineral Society: Aurora, CO.
  Shoval, S., Yartiv, S., Michaelian, K. H., Boudeulle, M., & Panczer, G. (1999). Hydroxyl stretching Raman and infrared bands ‘A’ and ‘Z’ in spectra of kaolinites. Clay Minerals, 34, 551–563.CrossRef
  Six, J., & Paustian, K. (2014). Aggregate-associated soil organic matter as an ecosystem property and a measurement tool. Soil Biology & Biochemistry, 68, A4–A9.CrossRef
  Spaccini, R., Piccolo, A., Conte, P., Haberhauer, G., & Gerzabek, M. H. (2002). Increased soil organic carbon sequestration through hydrophobic protection by humic substances. Soil Biology & Biochemistry, 34, 1839–1851.CrossRef
  Sparks, D. L. (2003). Environmental soil chemistry (2nd ed., ). Academic Press: Boston.
  Stewart, C. E., Paustian, K., Conant, R. T., Plante, A. F., & Six, J. (2009). Soil carbon saturation: implications for measurable carbon pool dynamics in long-term incubations. Soil Biology and Biochemistry, 41, 357–366.CrossRef
  Vaculikova, L., & Plevova, E. (2005). Identification of clay minerals and micas in sedimentary rocks. Acta Geodamica et Geomaterialia, 2(138), 167–175.
  Wang, W., Sardans, J., Zeng, C., Zhong, C., Li, Y., & Peñuelas, J. (2014a). Responses of soil nutrient concentrations and stoichiometry to different human land uses in a subtropical tidal wetland. Geoderma, 232–234, 459–470.CrossRef
  Wang, H., Guan, D., Zhang, R., Chen, Y., Hu, Y., & Xiao, L. (2014b). Soil aggregates and organic carbon affected by the land use change from rice paddy to vegetable field. Ecological Engineering, 70, 206–211.CrossRef
  Wiseman, C. L. S., & Püttmann, W. (2006). Interactions between mineral phases in preservation of soil organic matter. Geoderma, 134, 109–118.CrossRef
  Zotarelli, L., Alves, B. J. R., Urquiaga, S., Boddey, R. M., & Six, J. (2007). Impact of tillage and crop rotation on light fraction and intra-aggregate soil organic matter in two oxisols. Soil & Tillage Research, 95, 196–206.CrossRef
  
• 作者单位：Gopi Adhikari (1)
  Krishna G. Bhattacharyya (2)
  
  1. Department of Chemistry, Jagiroad College, Jagiroad, 782410, India
  2. Department of Chemistry, Gauhati University, Guwahati, 781014, India
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Environment
  Monitoring, Environmental Analysis and Environmental Ecotoxicology
  Ecology
  Atmospheric Protection, Air Quality Control and Air Pollution
  Environmental Management
  
• 出版者：Springer Netherlands
• ISSN：1573-2959

文摘

This work investigates the correlations existing among soil organic carbon (C), nitrogen (N), phosphorous (P), potassium (K), and physicochemical properties like clay mineralogy, textural components, soil aggregation, and land use pattern. Seven different locations were chosen in the tropical rainforest climate region of Assam, India, for the work. The soil texture classifications were clay, sandy clay loam, and sandy loam with mixed clay mineralogy consisting of tectosilicates and phylosilicates. Two distinct compositions of total Fe/Al oxides ≥11.5 and <10.8 % were observed along with two distinct groups of water stable soil aggregates of mean weight diameter ≈6.42 and ≤3.26 mm. The soil clay and sand had positive and negative contributions respectively to the soil organic carbon (SOC) protection, which was observed to be dependent on lesser sand content, higher silt + clay content, and the presence of higher percentages of total Fe/Al oxides. Soil clay mineralogy suggested that the mineral, chlorite, favored retention of higher SOC content in a particular site. Under similar climatic and mineralogical conditions, both natural and anthropogenic soil disturbances destabilized SOC protection through SOM mineralization and soil aggregate destabilization as indicated by SOC protective capacity studies. Urbanization resulting in soil compaction contributed to enhanced SOC level through increased contact between the occluded organic carbon and the soil mineralogical constituents.