Replacement of wildfire by whole-tree harvesting in jack pine forests: Effects on soil fertility and tree nutrition

▶ Organic-horizon C and N are higher and P and base cations lower, following whole-tree harvesting than following wildfire. ▶ Differences in organic horizon nutrient pools are insignificant compared to larger pools in mineral soil which were unaffected by disturbance regime. ▶ Cumulative soil nutrie...

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Veröffentlicht in:Forest ecology and management 2010-08, Vol.260 (7), p.1164-1174
Hauptverfasser: Rothstein, David E., Spaulding, Susan E.
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Sprache:eng
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Zusammenfassung:▶ Organic-horizon C and N are higher and P and base cations lower, following whole-tree harvesting than following wildfire. ▶ Differences in organic horizon nutrient pools are insignificant compared to larger pools in mineral soil which were unaffected by disturbance regime. ▶ Cumulative soil nutrient availability following whole-tree harvest falls within the natural range of variation produced by wildfire in this study area. Large areas of northern coniferous forests once naturally maintained by stand-replacing wildfires have shifted to an anthropogenic disturbance regime of clearcut harvesting followed by natural or artificial regeneration, with unknown consequences for soil biogeochemical processes. We used a comparative approach to investigate the effects of whole-tree harvesting (WTH) vs. stand-replacing wildfire (WF) on soil C and nutrient availability, and nutrition and growth of the succeeding stand, in jack pine ( Pinus banksiana) forests of northern Lower Michigan. We compared total carbon (C), total nitrogen (N), potential N mineralization, and extractable phosphorus (P), potassium (K), calcium (Ca) and magnesium (Mg) among stands regenerated via WTH or WF in two age classes (4–7 years and 12–18 years). We also measured jack pine foliar nutrition and height growth in these same stands, as well as estimating the contribution of legacy dead wood to ecosystem nutrient capital in young stands. We found some evidence in support of our hypothesis that WTH would leave behind greater pools of soil C and N, but lower pools of P and base cations. However, the differences we observed were confined entirely to surface organic horizons, with the two disturbance regimes indistinguishable when viewed cumulatively to our maximum sampling depth of 30 cm. Estimates of nutrient pools in legacy wood inherited by young jack pine stands were also small in comparison to total soil pools (ranging from 1 to 9% depending on the element), suggesting that decomposition and nutrient release from this material is not likely to result in noticeable differences in soil fertility later in stand development. Similar levels of soil nutrients between WTH- and WF-origin stands were reflected in our measures of jack pine foliar nutrition and height growth, which were both unaffected by mode of stand origin. Results from this study suggest that soil nutrient levels following WTH fall within the natural range of variation produced by WF in these jack pine forests; however, comparison
ISSN:0378-1127
1872-7042
DOI:10.1016/j.foreco.2010.07.007