Climate change increasing calcium and magnesium leaching from granitic alpine catchments

0479732 - BC 2018 RIV US eng J - Článek v odborném periodiku
Kopáček, Jiří - Kaňa, Jiří - Bičárová, S. - Fernandez, I.J. - Hejzlar, Josef - Kahounová, M. - Norton, S. A. - Stuchlík, Evžen
Climate change increasing calcium and magnesium leaching from granitic alpine catchments.
Environmental Science and Technology. Roč. 51, č. 1 (2017), s. 159-166. ISSN 0013-936X. E-ISSN 1520-5851
Grant CEP: GA ČR(CZ) GA14-09231S
Institucionální podpora: RVO:60077344
Klíčová slova: chemical-weathering rates * tatra mountain lakes * water chemistry * acid deposition * surface-water
Obor OECD: Water resources
Impakt faktor: 6.653, rok: 2017

Climate change can reverse trends of decreasing calcium and magnesium [Ca + Mg] leaching to surface waters in granitic alpine regions recovering from acidification. Despite decreasing concentrations of strong acid anions (-1.4 mu eq L-1 yr(-1)) during 2004-2016 in nonacidic alpine lakes in the Tatra Mountains (Central Europe), the average [Ca + Mg] concentrations increased (2.5 mu eq L-1 yr(-1)), together with elevated terrestrial export of bicarbonate (HCO3-, 3.6 mu eq L-1 yr(-1)). The percent increase in [Ca + Mg] concentrations in nonacidic lakes (0.3-3.2% yr(-1)) was significantly and positively correlated with scree proportion in the catchment area and negatively correlated with the extent of soil cover. Leaching experiments with freshly crushed granodiorite, the dominant bedrock,showed that accessory calcite and (to a lesser extent) apatite were important sources of Ca. We hypothesize that elevated terrestrial export of [Ca + Mg] :and HCO3- resulted from increased weathering caused by accelerated physical erosion of rocks due to elevated climate-related mechanical forces (an increasing frequency of days with high precipitation amounts and air temperatures fluctuating around 0 degrees C) during the last 2-3 decades. These climatic effects on water chemistry are especially strong in catchments where fragmented rocks are more exposed to weathering, and their position is less stable than in soil.
Trvalý link: http://hdl.handle.net/11104/0275680