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Czasopismo

2001 | 50 |

Tytuł artykułu

Quantity and quality of organic matter in forest and arable soils developed from sand and loess

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Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
Eight sandy and three loess forest and arable soils taken from the S-E region of Poland were used in the study. The following fractions of C were determined: total organic carbon, fraction soluble in 0.5 mol NaOH dm-3 (humic acids + fulvic acids), humic acids, fulvic acids, fraction soluble in 0.5 mol H2SO4 dm-3 (hemicelluloses) and residue. Quantity and quality of organic matter depended on horizon and soil use. The highest content was shown by fraction of humus acids and residue, whereas the lowest - hemicelluloses fraction. In most soils C ratio of humic to fulvic acids exceeded 1.0. On average, in humus horizons, it was higher in arable than in forest soils and in loess as against sandy soils. In sandy soils, a slightly higher content of humus fraction and lower residue one than in loess soils was found.

Wydawca

-

Czasopismo

Rocznik

Tom

50

Opis fizyczny

p.225-234

Twórcy

autor
  • Agricultural University, Leszczynskiego 7, 20-069 Lublin, Poland
autor
autor

Bibliografia

  • 1.Arinuskina E.B.: Methods of sail chemical analysis, Izdatielstvo Moskovskogo Universileta, 130-139, 1931.
  • 2. Borowiec S., Wybieralska A.: Differentiation of humus composition depending on type and utilization of soils. Roczn. Glebozn., 20, 67-79, 1969.
  • 3. Czerwiński Z.: Content of humus, nitrogen and clay minerals in separate mechanical fractions of podzolic sandy soil. Zesz, Probl. Post. Nauk Roln.. 40a, 1-13, 1961.
  • 4. Flis-Bujak M.: Transformations of humus compounds in soils developed from loess as influenced by crop rotation with various share of cereals. Rozpr. hab. AR Lublin. Rozpr. Nauk., 56, 1- 50, 1978.
  • 5. Gonet S.: Properties of humus in soils with differentiated fertilization. Organic fertilizers (PI). AR Szczecin, I, 288-293, 1992.
  • 6. Griffith S.M., Schnitzer M.: Analytical characteristics of humic and ful vie acids extracted from tropical volcanic soils. Soil Sci. Soc. Am. Proc., 39, 861-867, 1975.
  • 7. Maciejewska A.: The content of humus and sorption properties of light lextured soils, Zesz. Probl. Post. Nauk Roln., 41 1,319-324, 1993.
  • 8. Musierowicz A., Sytek .J.: Fractions of humus compounds in typical brown and grey-brown podzolic arable soils formed of loess. Roczn. Nauk Roln,, 91, 97-1 11,1966.
  • 9. Pisarek I.: Properties of humus substances extracted from grey-brown podzolic soils. Zesz. Probl. Post. Nauk Roln., 411, 177-181, 1993.
  • 10.Skłodowski P.: Transformations of organic matter in rusty and acid brown soils. Roczn. Glebozn., 37, 2/3, 127-137, 1986.
  • 11.Skłodowski P.: Influence of soil use on transformation of organic matter. Roczn. Glebozn., 45, 3/4, 77-84, 1994.
  • 12.Słowińska-Jurkiewicz A.: Studies on structure and physical properties of loess soils in Lublin region, Rozpr. habil., AR Lublin, 1984.
  • 13. Turski R.: Humic compounds in Polish soils. Roczn. Nauk Roln., Ser. D., Monografie, 212, 1- 69, 1988.
  • 14. Turski R., Słowińska-Jurkiewicz A.: Soils developed from loess. LTN-Lublin, 1994.
  • 15. Turski R., Uziak S,, Zawadzki S.: The natural environment of the Lublin District. Soils. LTN - Lublin, 1993.
  • 16. Wójcikowska-Kapusta A.: The effect of anthropogenic factor on chemical properties and content of some micronutrients in soils developed from loess. Rozpr. habil, Rozpr. Nauk. AR Lublin (209), Wyd. AR Lublin, 1998,

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Bibliografia

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