Wei Jiabin, Li Youqing, Li Juan, Yan Wei, Yin Qi, Jiang Hongwei, Li Zongling, Jiang Jinyu, Li Yu, Yao Yu, Zhang Lang
School of Landscape Architecture, Hunan Polytechnic of Environment and Biology, Hengyang, 421005, Hunan, China.
Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, the CAS Engineering Laboratory for Ecological Restoration of Island and Coastal Ecosystems, South China Botanical Garden, Xiaoliang Research Station for Tropical Coastal Ecosystems, Chinese Academy of Sciences, Guangzhou, 510650, China.
Sci Rep. 2024 Dec 3;14(1):30122. doi: 10.1038/s41598-024-81232-1.
The enhancement of soil aggregate size and stability is crucial for mitigating climate change and improving carbon sequestration in forest ecosystems. Biochar, derived from rice husks, has been suggested as an effective mean to increase soil carbon storage. However, isolating biochar's specific effects on soil aggregate formation and carbon sink capacity can be complex due to the overlapping influences of fertilization and understory vegetation cultivation. Our study circumvented these variables by incorporating different amounts of biochar into plantation soil without any additional cultivation or fertilization, conducting a detailed two-year field experiment. The findings revealed that biochar significantly increased the organic carbon content and density in the uncultivated under-forest Ferralsols, thus enhancing its carbon sink function. Intriguingly, while biochar raised the proportion of small soil aggregates (< 0.25 mm) and their organic carbon levels, it decreased the fraction of larger aggregates (> 0.25 mm), adversely affecting soil aggregate stability. These results suggest that biochar may compromise soil aggregate structure and stability in the absence of plant growth. The positive impact of biochar on soil carbon storage was found to depend more on its inherent inert carbon content than on soil type. Moreover, biochar alone was insufficient to increase the quantity of soil macroaggregates without the binding action of plant root exudates. Biochar's key function appears to be in enhancing the soil aggregate-forming processes facilitated by plant roots and microorganisms. Therefore, for optimal carbon sequestration in forest soils, integrating biochar application with appropriate agricultural practices is advisable.
提高土壤团聚体大小和稳定性对于缓解气候变化以及改善森林生态系统中的碳固存至关重要。源自稻壳的生物炭被认为是增加土壤碳储量的有效手段。然而,由于施肥和林下植被种植的重叠影响,分离生物炭对土壤团聚体形成和碳汇能力的具体影响可能很复杂。我们的研究通过在人工林土壤中加入不同量的生物炭,且不进行任何额外的种植或施肥,进行了一项为期两年的详细田间试验,从而规避了这些变量。研究结果表明,生物炭显著增加了未开垦的林下铁铝土中的有机碳含量和密度,从而增强了其碳汇功能。有趣的是,虽然生物炭提高了小土壤团聚体(<0.25毫米)的比例及其有机碳含量,但它降低了较大团聚体(>0.25毫米)的比例,对土壤团聚体稳定性产生了不利影响。这些结果表明,在没有植物生长的情况下,生物炭可能会损害土壤团聚体结构和稳定性。发现生物炭对土壤碳储存的积极影响更多地取决于其固有的惰性碳含量,而不是土壤类型。此外,没有植物根系分泌物的结合作用,仅生物炭不足以增加土壤大团聚体的数量。生物炭的关键作用似乎在于增强由植物根系和微生物促进的土壤团聚体形成过程。因此,为了在森林土壤中实现最佳的碳固存,建议将生物炭的施用与适当的农业实践相结合。