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Czasopismo

2016 | 160 | 09 |

Tytuł artykułu

Rozpuszczanie skały węglanowej w glebach leśnych buczyn i świerczyn w warunkach laboratoryjnych

Treść / Zawartość

Warianty tytułu

EN
Dissolution of carbonate rock in soils under beech and spruce forests in the laboratory conditions

Języki publikacji

PL

Abstrakty

EN
Chemical denudation plays a crucial role in affecting the water chemistry and the development of the relief, therefore the dissolution of carbonate rocks is the subject of numerous research. The aim of the study was to determine the effect of soil material derived from the organic (O) as well as humus (A) horizons of forest soils (common beech and Norway spruce stands) on the dissolution of rock. During one−year laboratory experiment standardized samples of dolomitic limestone placed in the soil material were washed with deionized water. The greatest loss of the sample rocks mass occurred in O material from Norway spruce stand (43.9‰ on average), while in other cases, the loss of rock samples mass was much lower and statistically non−significant. The total masses of calcium (Ca2+) leached from O material under beech and spruce stands were similar, however in the case of spruce most of Ca2+ derives from rock dissolution. Similarly, higher proportion of magnesium (Mg2+) leached from O material under Norway spruce derives from rock dissolution, although the total mass of Mg2+ leached is higher from O material under beech. The total mass of Ca2+ and Mg2+ leached from A material was similar or higher than from O material, however most of those ions derived from the soil material. The results indicate that the replacement of beech by Norway spruce can increase chemical denudation as well as Ca2+ and Mg2+ leaching, wherein Ca2+ leaching would be significantly greater than Mg2+.

Wydawca

-

Czasopismo

Rocznik

Tom

160

Numer

09

Opis fizyczny

s.751-758,rys.,tab.,wykr.,bibliogr.

Twórcy

autor
  • Instytut Geografii i Gospodarki Przestrzennej, Uniwersytet Jagielloński, ul.Gronostajowa 7, 30-387 Kraków
autor
  • Instytut Geografii i Gospodarki Przestrzennej, Uniwersytet Jagielloński, ul.Gronostajowa 7, 30-387 Kraków
autor
  • Instytut Geografii i Gospodarki Przestrzennej, Uniwersytet Jagielloński, ul.Gronostajowa 7, 30-387 Kraków
  • Instytut Geografii i Gospodarki Przestrzennej, Uniwersytet Jagielloński, ul.Gronostajowa 7, 30-387 Kraków

Bibliografia

  • Akiyama S., Hattanji T., Matsushi Y., Matsukura Y. 2015. Dissolution rates of subsoil limestone in a doline on the Akiyoshi-dai Plateau, Japan: An approach from a weathering experiment, hydrological observations, and electrical resistivity tomography. Geomorphology 247: 2-9.
  • Berger T. W., Köllensperger G., Wimmer R. 2004. Plant-soil feedback in spruce (Picea abies) and mixed spruce-beech (Fagus sylvatica) stands as indicated by dendrochemistry. Plant Soil 264: 69-83.
  • Berger T. W., Swoboda S., Prohaska T., Glatzel G. 2006. The role of calcium uptake from deep soils for spruce (Picea abies) and beech (Fagus sylvatica). Forest Ecology Management 229: 234-246.
  • Berger T. W., Untersteiner H., Toplitzer M., Neubauer C. 2009. Nutrient fluxes in pure and mixed stands of spruce (Picea abies) and beech (Fagus sylvatica). Plant and Soil 322 (1): 317-342.
  • Bergkvist B., Folkeson L. 1995. The Influence of Tree Species on Acid Deposition, Proton Budgets and Element Fluxes in South Swedish. Forest Ecosystems Ecological Bulletins 44: 90-99.
  • Crabtree R. W., Trudgill S. T. 1985. Chemical denudation on a magnesian limestone hillslope, field evidence and implications for modelling. Earth Surface Processes and Landforms 10: 331-341.
  • Davis M. R. 1990. Chemical composition of soil solutions extracted from New Zealand beech forests and West German beech and spruce forests. Plant and Soil 126: 237-246.
  • Dixon J. C., Thorn C. E., Darmody R. G., Schlyterd P. 2001. Weathering rates of fine pebbles at the soil surface in Kärkevagge, Swedish Lapland. Catena 45: 273-286.
  • Egli M., Merkli C., Sartorti G., Mirabella A., Plötze M. 2008. Weathering, mineralogical evolution and soil organic matter along a Holocene toposequence developed on carbonate-rich materials. Geomorphology 97: 675-696.
  • Fabijanowski J., Dziewolski J. 1996. Gospodarka leśna. W: Mirek Z. [red.]. Przyroda TPN. TPN-PTPNoZ, Kraków – Zakopane. 675-696.
  • Finzi A. C., Van Breemen N., Canham C. D. 1998. Canopy tree-soil interactions within temperate forests: species effects on soil carbon and nitrogen. Ecological Applications 8: 440-446.
  • Hattanji T., Ueda M., Song W., Ishii N., Hayakawa Y. S., Takaya Y., Matsukura Y. 2014. Field and laboratory experiments on high dissolution rates of limestone in stream flow. Geomorphology 204: 485-492.
  • Inkpen R. 1995. Errors in measuring the percentage dry weight change of stone tablets. Earth Surface Processes and Landforms 20: 783-793.
  • Jin L., Williams E. L., Szramek K. J., Walter L. M., Hamilton S. K. 2008. Silicate and carbonate mineral weathering in soil profiles developed on Pleistocene glacial drift (Michigan, USA): Mass balances based on soil water geochemistry. Geochimica et Cosmochimica Acta 72: 1027-1042.
  • Klimek B., Niklińska M., Jaźwa M., Tarasek A., Takielak I., Musielok Ł. 2015. Covariation of soil bacteria function diversity along an altitudinal climatic gradient in the Western Carpathians. Pedobiologia 58: 105-112.
  • Kotarba A. 1976. Współczesne modelowanie węglanowych stoków wysokogórskich. Prace Geograficzne PAN 120: 1-128.
  • Lindroos A.-J., Brügger T., Derome J., Derome K. 2003. The weathering of mineral soil by natural soil solutions. Water Air and Soil Pollution 149: 269-279.
  • Matsukura Y., Hattanji T., Oguchi C. T., Hirose T. 2007. Ten year measurement of weight-loss of rock tablets due to weathering in a forested hillslope of a humid temperate region. Zeitschrift für Geomorphologie 51 (1): 27-40.
  • Matsukura Y., Hirose T. 1999. Five-year measurement of weight loss of rock tablets due to weathering on a forested hillslope of a humid temperate region. Engineering Geology 55: 69-76.
  • Oh N.-H., Hofmockel M., Levine M., Richter D. D. 2007. Did elevated atmospheric CO2 alter soil mineral weathering? An analysis of 5-year soil water chemistry data at Duke FACE study. Global Change Biology 13: 2626-2641.
  • Raulund-Rassmusen K., Borggaard O. K., Hansen K. C. B., Olsson M. 1998. Effect of natural organic soil solutes on weathering rates of soil minerals. European Journal of Soil Science 49: 397-406.
  • Reimann C., Filzmoser P. 2000. Normal and lognormal data distribution in geochemistry: death of a myth. Consequences for the statistical treatment of geochemical an environmental data. Environmental Geology 39 (9): 1001-1014.
  • Richter D. D., Hofmockel M., Callaham M. A., Powlson D. S., Smith P. 2007. Long-term soil experiments: key to managing Earth’s rapidly changing ecosystem. Soil Science of America Journal 71: 266-279.
  • Rothe A., Huber C., Kreutzer K., Weis W. 2002. Deposition and soil leaching in stands of Norway spruce and European Beech: Results from the Höglwald research in comparison with other European case studies. Plant and Soil 240: 33-45.
  • Stevenson F. J. 1994. Humus Chemistry. Genesis, Composition, Reactions. Wiley and Sons, New York, Chichester, Brisbane, Toronto, Singapore.
  • Thorn C. E., Darmody R. G., Dixon J. C., Schlyter P. 2002. Weathering rates of buried machine-polished rock disks, Kärkevagge, Swedish Lapland. Earth Surface Processes and Landforms 27: 831-845.
  • Thorn C. E., Dixon J. C., Darmody R. G., Allen C. E. 2006. Ten years (1994-2004) of ‘potential’ weathering in Kärkevagge, Swedish Lapland. Earth Surface Processes and Landforms 31: 992-1002.
  • Trudgill S. T., Crabtree R. W., Ferguson R. I., Ball J., Gent R. 1994. Ten year remeasurement of chemical denudation on a magnesian limestone hillslope. Earth Surface Processes and Landforms 19: 109-114.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

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