Soil development on basic and ultrabasic rocks in cold environments of Russia traced by mineralogical composition and pore space characteristics

Catena

Volumn 137, Issue , 2016, Pages 596-604

  Lessovaia, Sofia N ^a,d   Dultz, Stefan ^b   Plötze, Michael ^c   Andreeva, Natalia ^d   Polekhovsky, Yury ^a   Filimonov, Alexey ^d   Momotova, Olesya ^e  

^a ST PETERSBURG STATE UNIVERSITY   (Russian Federation)

^b LEIBNIZ UNIVERSITY HANNOVER   (Germany)

^c ETH ZURICH   (Switzerland)

^d PETER THE GREAT ST PETERSBURG POLYTECHNIC UNIVERSITY   (Russian Federation)

^e BELGOROD STATE UNIVERSITY   (Russian Federation)

Author keywords

Amphibolites; Mineral associations; Pore space characteristics; Serpentinous dunite; Silicate weathering; Soil formation

Indexed keywords

AMPHIBOLITE; BOREAL FOREST; CHEMICAL WEATHERING; CLAY MINERAL; CLIMATE; DUNITE; METAGABBRO; MINERALOGY; PEDOGENESIS; PHYLLOSILICATE; PORE SPACE; ROCK PROPERTY; SERPENTINITE; SILICATE; SOIL DYNAMICS;

FENNOSCANDIA; RUSSIAN FEDERATION; URALS;

EID: 84964305255     PISSN: 03418162     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.catena.2014.11.020     Document Type: Article

References (37)

1. Alexander, E.B., DuShey, J., 2011. Topographic and soil differences from peridotite to serpentinite. Geomorphology 135, 271-276.
2. Allen, Ch. E., 2002. The influence of schistocity on soil weathering on large boulder tops, Kärkevagge, Sweden. Catena 49, 157-169.
3. Arnaud, R.J.S.T., Whiteside, E.P., 1963. Physical breakdown in relation to soil development. Eur. J. Soil Sci. 14, 267-281.
4. Bergmann, J., Kleeberg, R., 1998. Rietveld analysis of disordered layer silicates. Mater. Sci. Forum 278-281, 300-305.
5. Bergmann, J., Friedel, P., Kleeberg, R., 1998. BGMN-a new fundamental parameters based Rietveld program for laboratory X-ray sources, it's use in quantitative analysis and structure investigations. CPD Newsletter 20. Commission of Powder Diffraction, International Union of Crystallography, pp. 5-8.
6. Bish, D.L., Plötze, M., 2011. X-ray powder diffraction with emphasis on qualitative and quantitative analysis in industrial mineralogy. In: Christidis, G. (Ed.), Industrial Mineralogy, EMU Notes in Mineralogy vol. 9, pp. 35-76 (Chapter 3).
7. Borden, P.W., Ping, C.-Lu., McCarthy, P.J., Naidu, S., 2010. Clay mineralogy in arctic tundra gelisols, northern Alaska. Soil Sci. Soc. Am. J. 74 (2), 580-592.
8. Caillaud, J., Proust, D., Righi, D., 2006.Weathering sequences of rock-formingminerals in a serpentinite: influence of microsystems on clay mineralogy. Clays Clay Minerals 54 (1), 87-100.
9. Chernyakhovskii, A.G., 1994. Eluvial process and soil formation (Eluvial'nyi prozess e pochvoobrazovanie). Nauka, Moscow (in Russian).
10. Darot, M., Reuschle, T., 1999. Direct assessment of Wood's metal wettability on quartz. Pure Appl. Geophys. 155, 119-129.
11. Dultz, S., Behrens, H., Simonyan, A., Kahr, G., Rath, T., 2006. Determination of porosity and pore connectivity in feldspars from soils of granite and saprolite. Soil Sci. 171, 675-694.
12. Eggleton, R.A., 1984. Formation of iddingsite rims on olivine: a transmission electron microscope study. Clays Clay Minerals 32, 1-11.
13. Hseu, Z.Y., Tsai, H., Hsi, H.C., Chen, Y.C., 2007. Weathering sequences of clay minerals in soils along a serpentinitic toposequence. Clays Clay Minerals 55, 389-401.
14. Jackson, M.L., Lim, C.H., Zelazny, L.W., 1986. Oxides, hydroxides, and aluminosilicates. In: Klute, A. (Ed.), Methods of Soil Analysis. Part 1, 2nd ed., pp. 101-150.
15. Kaufmann, J., 2009. Characterization of pore space of cement-based materials by combined mercury and Wood's Metal intrusion. J. Am. Ceram. Soc. 92, 209-216.
16. Klapetek, P., Ohlidal, I., Franta, D., Montaigne-Ramil, A., Bonanni, A., Stifter, D., Sitter, H., 2003. Atomic force microscopy characterization of ZnTe epitaxial films. Acta Phys. Slovaca 3 (53), 223-230.
17. Lessovaia, S.N., Polekhovsky, Yu. S., 2009. Mineralogical composition of shallow soils on basic and ultrabasic rocks of East Fennoscandia and of the Ural Mountains, Russia. Clays Clay Minerals 57, 476-485.
18. Lessovaia, S., Dultz, S., Polekhovsky, Yu., Krupskaya, V., Vigasina, M., Melchakova, L., 2012. Rock control of pedogenic clay mineral formation in a shallow soil from serpentinous dunite in the Polar Urals, Russia. Appl. Clay Sci. 64, 4-11.
19. Lessovaia, S.N., Goryachkin, S.V., Desyatkin, R.V., Okoneshnikova, M.V., 2013. Pedoweathering and mineralogical change in Cryosols in an ultracontinental climate (Central Yakutia, Russia). Acta Geodyn. Geomater. 10 (172), 465-473 (No. 4).
20. Lloyd, R.R., Provis, J.L., Smeaton, K.J., van Deventer, J.S.J., 2009. Spatial distribution of pores in fly ash-based inorganic polymer gels visualised byWood's metal intrusion. Microporous Mesoporous Mater. 126, 32-39.
21. Mehra, O.P., Jackson, M.L., 1958. Iron oxide removal from soils and clays by a dithionite-citrate system buffered with sodium bicarbonate. Clays Clay Minerals 7, 317-327.
22. Navarre-Sitchler, A., Steefel, C.I., Yang, L., Tomutsa, L., Brantley, S.L., 2009. Evolution of porosity and diffusivity associated with chemical weathering of a basalt clast. J. Geophys. Res. 114, 14. http://dx.doi.org/10.1029/2008JF001060 art. no. F02016.
23. Proust, D., Caillaud, J., Fontaine, C., 2006. Clay minerals in early amphibole weathering: trito dioctahedral sequence as a function of crystallization sites in the amphibole. Clays Clay Minerals 54, 351-362.
24. Putnis, A., 2002. Mineral replacement reactions: frommacroscopic observations tomicroscopic mechanisms. Mineral. Mag. 66, 689-708.
25. Schuessler, J.A., Botcharnikov, R.E., Behrens, H., Misiti, V., Freda, C., 2008. Oxidation state of iron in hydrous phono-tephritic melts. Am. Mineral. 93, 1493-1504.
26. Sedov, S.N., Vaseneva, E.G., Shoba, S.A., 1992. Modern and ancient processes of weathering in soils from basic rocks in Valaam Island (Sovremennye e drevnie prozessy vyvetrivaniya v pochvakh na osnovnykh porodakh ostrova Valaam). Pochvovedenie 7, 83-96 (in Russian).
27. Simas, F.N.B., Schaefer, C.E.G.R., Melo, V.F., Guerra, M.B.B., Saunders, M., Gilkes, R.J., 2006. Clay sized minerals in permafrost-affected soils (Cryosols) from King George Island, Antarctica. Clays Clay Minerals 54, 721-736.
28. Simonyan, A.V., Dultz, S., Behrens, H., 2012. Diffusive transport of water in porous fresh to altered mid-ocean ridge basalts. Chem. Geol. 306-307, 63-77.
29. Smith, K., Milnes, A., Eggleton, R.A., 1987. Weathering of basalt: formation of iddingsite. Clays Clay Minerals 35 (6), 418-428.
30. Tyurin, E.V., 1931. New modification of volume method for determination of humus by chromic acid (Novoe vidoizmenenie ob'emnogo metoda opredeleniya gumusa s pomosh'u khromovoi kisloty). Pochvovedenie 37, 515-524 (in Russian).
31. Velbel, M.A., 1989. Weathering of hornblende to ferruginous products by a dissolution-reprecipitation mechanism: petrography and stoichiometry. Clays Clay Minerals 37, 515-524.
32. Velde, B., Meunier, A., 2008. The Origin of Clay Minerals in Soils and Weathered Rocks. Springer-Verlag, Berlin, Heidelberg, New York.
33. Washburn, E.W., 1921. Note on amethod of determining the distribution of pore sizes in a porous material. Proc. Natl. Acad. Sci. U. S. A. 7, 115-116.
34. Whitney, D.L., Evans, B.W., 2010. Abbreviations for names of rock-forming minerals. Am. Mineral. 95, 185-187.
35. Wilson, M.J., 2004.Weathering of the primary rock-formingminerals: processes, products and rates. Clay Miner. 39, 233-266.
36. Wilson, M.J., Farmer, V.C., 1970. A study of weathering in a soil derived from a biotite-hornblende rock II. The weathering of hornblende. Clay Miner. 8, 435-444.
37. World Reference Base for Soil Resources, 2006. World Soil Resources Reports 103. 2nd edition. FAO, Rome.