Forest growth responds more to air pollution than soil acidification

0571049 - ÚVGZ 2024 RIV US eng J - Článek v odborném periodiku
Hruška, Jakub - Oulehle, Filip - Chuman, Tomáš - Kolář, T. - Rybníček, M. - Trnka, Miroslav - McDowell, W. H.
Forest growth responds more to air pollution than soil acidification.
PLoS ONE. Roč. 18, č. 3 (2023), č. článku e0256976. ISSN 1932-6203. E-ISSN 1932-6203
Grant CEP: GA MŠMT(CZ) EF16_019/0000797; GA ČR(CZ) GC21-22810J
Výzkumná infrastruktura: CzeCOS IV - 90248
Institucionální podpora: RVO:86652079
Klíčová slova: spruce picea -abies * norway spruce * magic model * nitrogen * deposition * carbon * chemistry * turnover * decline * sulfur
Obor OECD: Forestry
Impakt faktor: 3.7, rok: 2022
Způsob publikování: Open access
https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0256976

The forests of central Europe have undergone remarkable transitions in the past 40 years as air quality has improved dramatically. Retrospective analysis of Norway spruce (Picea abies) tree rings in the Czech Republic shows that air pollution (e.g. SO2 concentrations, high acidic deposition to the forest canopy) plays a dominant role in driving forest health. Extensive soil acidification occurred in the highly polluted ,,Black Triangle,, in Central Europe, and upper mineral soils are still acidified. In contrast, acidic atmospheric deposition declined by 80% and atmospheric SO2 concentration by 90% between the late 1980s and 2010s. In this study we oserved that annual tree ring width (TRW) declined in the 1970s and subsequently recovered in the 1990s, tracking SO2 concentrations closely. Furthermore, recovery of TRW was similar in unlimed and limed stands. Despite large increases in soil base saturation, as well as soil pH, as a result of repeated liming starting in 1981, TRW growth was similar in limed and unlimed plots. TRW recovery was interrupted in 1996 when highly acidic rime (originating from more pronounced decline of alkaline dust than SO2 from local power plants) injured the spruce canopy, but recovered soon to the pre-episode growth. Across the long-term site history, changes in soil chemistry (pH, base saturation, Bc/Al soil solution ratio) cannot explain observed changes in TRW at the two study sites where we tracked soil chemistry. Instead, statistically significant recovery in TRW is linked to the trajectory of annual SO2 concentrations or sulfur deposition at all three stands.
Trvalý link: https://hdl.handle.net/11104/0342359