Change in soil carbon, nitrogen, and phosphorus after timber harvesting in northern hardwood forests

Joshua J Puhlick, Ivan J. Fernandez
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Abstract

Quantifying changes in soil carbon (C) and nutrient stocks after timber harvesting is needed to inform C management and to ensure that forest productivity is sustained over time. Our objective was to assess changes in soil C, nitrogen (N), and phosphorus (P) 1 year after timber harvesting in temperate northern hardwood forests. We established permanent plots in forest stands for measuring forest attributes before and after harvesting. We collected soils from quantitative soil pits, which were associated with permanent plots, to determine total C, total N, and extractable P stocks and concentrations. Mean post-harvest fine fraction organic (O) horizon C was less than the pre-harvest stock, but we did not detect a statistically significant change in total O horizon or mineral soil C stocks. For the fine fractions of the O horizon and mineral soil from the 0–5 and 5–30 cm depth increments of the B horizon, total N and extractable P stocks were positively correlated with total C stocks. For all of these soil components, extractable P stocks and concentrations declined over time, which could be related to post-harvest stand conditions that favored microbial activity and immobilization of available P. These findings indicate that P availability could be a concern in these forests and that long-term monitoring is needed to consider potential management actions for ensuring that forest productivity is sustained.

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北方阔叶林采伐木材后土壤碳、氮、磷的变化
需要量化木材采伐后土壤碳(C)和养分储量的变化,以便为碳管理提供信息,并确保森林生产力长期持续。我们的目的是评估温带北方阔叶林木材采伐后1年土壤C、氮和磷的变化。我们在林场中建立永久性样地,测量采伐前后的森林属性。我们从与永久地块相关的定量土壤坑中收集土壤,以确定总碳、总氮和可提取磷的储量和浓度。平均采后细粒有机(O)层储量低于采前储量,但总O层储量和矿质土C储量变化不显著。在0-5 cm和5-30 cm深度增量的O层和矿质土中,总氮和可提取磷储量与总碳储量呈正相关。对于所有这些土壤成分,可提取磷储量和浓度随着时间的推移而下降,这可能与采后有利于微生物活动和有效磷固定的林分条件有关。这些研究结果表明,磷有效性可能是这些森林关注的问题,需要长期监测,以考虑潜在的管理行动,以确保森林生产力的持续。
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