Refractory Soil Organic Matter — Formation, Accumulation, Translocation and Transformation

作者: H.-P. Blume , D. M. White , L. Beyer , M. Bölter , D. Kuhn

DOI: 10.1007/978-3-642-56318-8_9

关键词:

摘要: Soil formation in the Antarctic is a recognised process. The occurrence of accumulations organic matter despite hostile climate, and soils by debris mosses, lichens algae widespread (Campbell Claridge 1987; Beyer et al. 1999). This leads to mineral which may contain large amounts soil maritime (Blume 1996). In contrast, patches are associated locally with shallow coastal regions East Antarctica (Beyer

参考文章(52)
Bernhard Post, Reinhold Hempfling, Horst Klamberg, Hans-Rolf Schulten, Zur Charakterisierung von Boden-Huminstoffen Fresenius Journal of Analytical Chemistry. ,vol. 331, pp. 273- 281 ,(1988) , 10.1007/BF00481896
N. E. Smeck, G. F. Hall, Larry P. Wilding, The soil orders Elsevier , Distributors for the U.S. and Canada, Elsevier Science Pub. Co.. ,(1983)
J.A. McKeague, F. DeConinck, D.P. Franzmeier, Chapter 6 Spodosols1 Developments in soil science. ,vol. 11, pp. 217- 252 ,(1983) , 10.1016/S0166-2481(08)70617-2
Clarence E. Koeppe, George C. De Long, Weather and climate ,(1935)
David W.H. Walton, J. Miles, Primary succession on land Blackwell Scientific Publications. ,(1993)
G. G. C. Claridge, I. B. Campbell, Antarctica: Soils, weathering processes and environment Elsevier Science Pub. Co. Inc.,New York, NY. ,(1987)
M. SCHNITZER, C. TARNOCAI, P. SCHUPPLI, H. -R. SCHULTEN, Nature of the organic matter in Tertiary paleosols in the Canadian Arctic. Soil Science. ,vol. 149, pp. 257- 267 ,(1990) , 10.1097/00010694-199005000-00002