Forest harvesting alters the biogeochemical character and protection of mineral associated carbon in a Podzolic soil.

Discover soil Pub Date : 2026-01-01 Epub Date: 2026-07-14 DOI:10.1007/s44378-026-00261-6
S MacIntyre, L Kellman, C E Gabriel, A Diochon
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Abstract

Forest harvesting can alter the biogeochemical processes that determine the quantity and chemical nature of stored soil organic carbon (SOC). This SOC is distributed amongst organic compounds in soils of varying biological and physical complexity, with a large fraction of this SOC associated with metals and minerals. The objective of this study was to investigate changes in fractions of SOC associated with metals and minerals and their chemical character through depth and time for Podzolic soils of a harvested temperate red spruce (Picea rubens Sarg.) forest chronosequence to understand biogeochemical changes in SOC and its sensitivity to forest harvesting disturbance. A standard analytical approach was used to sequentially extract C from mineral pools of increasing SOC retention strength through depth (0-5, 5-10, 10-15, 15-20, 20-35, 35-50 cm) and time (1, 15, 45, 80, and 125+-yr) following forest harvesting. The biogeochemical character of the largest pool was assessed using aromaticity (specific UV absorbance: SUVA254) and stable C-isotopes (δ13C). Results show that the organo-metal complexed fraction accounted for the largest pool examined (~ 59-85% of mineral associated SOC) and was most susceptible to harvesting losses, particularly in the deeper mineral soil. Biogeochemical patterns of SOC within this pool through depth showed distinct changes including: i) a lower aromaticity with lower C content across all sites within the deep mineral soil (20-50 cm), and ii), a correlation between decreases in aromaticity and increases in δ13C across all sites. This pattern of lower aromaticity and enriched δ13C can be interpreted as a shift towards more microbially processed and/or simpler compounds. Overall, the observed patterns support the conceptual hypothesis that forest harvesting alters the biogeochemical character and protection of the mineral associated fraction of SOC in soils of this region.

森林采伐改变了灰化土的生物地球化学特征和矿物伴生碳的保护。
森林采伐可以改变决定土壤有机碳储量和化学性质的生物地球化学过程。这种有机碳分布在不同生物和物理复杂性的土壤中的有机化合物中,其中很大一部分与金属和矿物有关。本研究旨在研究温带红杉林采伐后灰化土中金属矿物有机碳组分及其化学特征随深度和时间的变化,以了解土壤有机碳的生物地球化学变化及其对森林采伐干扰的敏感性。采用标准分析方法,从采伐后不同深度(0-5、5-10、10-15、15-20、20-35、35-50 cm)和时间(1、15、45、80和125+-yr)的矿池中依次提取碳。利用芳香性(特定紫外吸光度:SUVA254)和稳定c同位素(δ13C)评价了最大池的生物地球化学特征。结果表明,有机-金属络合组分占矿物相关有机碳的最大池(约59-85%),并且最容易受到收获损失,特别是在较深的矿物土壤中。深层矿质土(20 ~ 50 cm)土壤有机碳的生物地球化学模式表现出明显的变化:1)深层矿质土(20 ~ 50 cm)各点芳香性降低,δ13C升高;2)各点芳香性降低,δ13C升高。这种较低芳香性和富集δ13C的模式可以解释为向更多微生物处理和/或更简单的化合物的转变。总体而言,观察到的模式支持了森林采伐改变了该地区土壤有机碳矿物相关组分的生物地球化学特征和保护的概念假设。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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