Journals / Mediterranean Agricultural Sciences / 1995 / Volume: 8 Issue: 1

Properties of Transported Soil Material

Taşınmış Toprak Materyallerinin Özellikleri

Pages
197–205
Publication Date
1995-12-01
DOI
—
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

It is possible to get valuable information not only on the origin but also on the mode of formation of the transported material by field (macromorphology) and laboratory (analytical and micromorphological) investigations.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:Three alternating types of periods may be recognized in the development of landscape; 1) period of landscape stability; 2) period of landscape instability in which transported deposits are formed; and 3) period in which both case can be seen.
📊
Key Findings & Data:Therefore transported material can provide valuable information on the conditions and developments of the unstable periods.
💡
Conclusion & Impact:It is possible to get valuable information not only on the origin but also on the mode of formation of the transported material by field (macromorphology) and laboratory (analytical and micromorphological) investigations.
🔬Design:Derleme
📍Scope:Comprehensive Sample
⚙️Variables:Toprak Materyali · makromorfolojik · topografya

Abstract

Three alternating types of periods may be recognized in the development of landscape; 1) period of landscape stability; 2) period of landscape instability in which transported deposits are formed; and 3) period in which both case can be seen. Therefore transported material can provide valuable information on the conditions and developments of the unstable periods. It is possible to get valuable information not only on the origin but also on the mode of formation of the transported material by field (macromorphology) and laboratory (analytical and micromorphological) investigations.

Özet

Yeryüzündeki topografyanın gelişmesinde birbirini takıp eden üç ayrı periyod gözlemlenebilir; 1) durağan period; 2) taşınmış materyalin ouştuğu durağan olmayan period; ve 3) her iki periyodun görüldüğü durum. Bu nedenle taşınmış materyaller oluşmuş oldukları periyod hakkında değerli bilgiler sağlarlar. Arazi (makromorfolojik) ve laboratuvar (analitik ve mikromorfolojik) çalışmaları ile yalnızca taşman materyallerin kaynağı hakkında değil, aynı zamanda onların nasıl oluştuklarını da içeren bilgiler elde etmek mümkündür.

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Cite This Article

Alagöz, Z. (1995). Properties of Transported Soil Material. Mediterranean Agricultural Sciences, Volume: 8 Issue: 1, 197–205. https://ajindex.com/articles/1170886

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References (23)

  1. Butler, B. E. Periodic phenomena in landscapes as a basis for soil studies. Soil Publication No: 14. Commonwealth Scientific and Industrial Research Organisation, Australia Melbourne. 1959.
  2. Mucher, H. J. Micromorphology of slope deposits: the necessity of classification, 553-566. In. Rutherford, G. K. (Eds.) Soil Microscopy. Proceedings of the 4th International Working-Meeting on Soil Micromorphology. Department of Geography, Quens University. Kingston, Ontario, Canada. 1974.
  3. Foster, G. R. and Mayer, L. D. Mathematical simulation of upland erosion by fundamental erosion mechanics, 190-207. In: Present and perspective technology of predicting sediment yield and sources, ARS-40, USDA, Washington. 1975.
  4. Monke, E. J., Marelli, H. J., Meyer, L. D. and De Jong, J. F. Runoff, Erosion, and Nutrient movement from interrill areas. Trans. ASAE. 58-61. 1977.
  5. Meyer, L. D., Harmon, W. C. and McDowell, L. L. Sediment sizes eroded from crop row sideslopes. Transection of the ASAE, 23(4): 891-898. 1980.
  6. Bolt, A. J., Mucher, H. J., Sevink, J. and Verstraten, J. M. A study on loess-derived colluvia in southern Limburg (The Netherlands). Net. J. Agric. Sci. 28: 110-126. 1980.
  7. Avery, B. W. Soils of the British Isles. CAB International. 1990.
  8. Courty, M. A. and Fedoroff, N. Micromorphology of a Holocene dwelling. PACT, 7: 257-277. 1985.
  9. Valentine, K. W. G. and Dalrymple, J. B. The identification, lateral variation, and chronology of two buried palaecatenas at Woodhall Spa and West Runton, England. Quat. Res. 5: 551-590. 1975.
  10. Kemp, R A. Soil micromorphology and the Quaternary: Q.R.A. Tecnical guide No 2. Cambridge. 1985.
  11. Mucher, H. J. and De Ploey J. Experimental and micromorphologycal investigation of erosion and redeposition of loess by water. Earth Surface Processes, 2,117-124. 1977.
  12. Green, P. Recognition of sedimentary characteristics in soils by size-shape analysis. Geoderma, 11: 181-193. 1974.
  13. Brewer, R. Fabrics and Mineral Analysis of Soils. John Wiley and Sons. Inc. 1964.
  14. Brewer, R. Use of macro and micromorphological data in soil stratigraphy to elucidate surficial geology and soil genesis. J. Geo. Soc. Australia, 19: (3) 331-344. 1972.
  15. Brewer, R. and Sleeman, J. R. Soil structure and fabric, their definition and description. J. Soil Scı. 11 (1): 173-185. 1960.
  16. Goudie, A. and Bull, P. A. Slope process change and colluvium deposition in Swaziland: SEM analysis. Earth Surface Process and Landforms, 9: 289-299. 1984.
  17. FitzPatrick, E. A. Micromorphology of soils. Chapman and Hall, London. 1984.
  18. Mucher, H. J. and Vreeken, W. J. (Re)deposition of loess in Southern Limbourg, the Netherlands, 2. Micromorphology of the lower silt loam complex and comparison with deposits produced under laboratory conditions. Earth Surface Processes and Landforms, 6: 355-363. 1981.
  19. Bullock, P. and Murphy, C. P. Evolution of a Paleo-Argillic Brown Earth (Paleudalf) from Oxfordshire, England. Geoderma, 22: 225- 252. 1979.
  20. Birkeland, P. W. Soils and geomorphology. Oxford University Press 1984.
  21. Mucher, H. J., Carballas, T., Guitian Ojea, F., Jungerius, P. D, Kroonenberg, S. B. and Villar, M. C. Micromorphological analysis of effects of alternating phases of landscape stability and instability on two soil profiles in Galicia, N. W. Spain. Geoderma, 8: 241-266. 1972.
  22. Mucher, H. J. and Morozova, T. D. The application of soil micromorphology in Quaternary geology and geomorphology, (1): 151-194. In: Bullock, P. and Murphy, C. P. (Ed) Soil Micromorphology. Proceeding 6th International Working Meeting on Soil Micromorpholgy, 1981, London. A.B. Academic Publishers, Berkhamsted England. 1983.
  23. Mucher, H. J., Carballas, T., Guitian Ojea, F., Jungerius, P. D, Kroonenberg, S. B. and Villar, M. C. Micromorphological analysis of effects of alternating phases of landscape stability and instability on two soil profiles in Galicia, N. W. Spain. Geoderma, 8: 241-266. 1972.