Department of Engineering, Dalhousie University Faculty of Agriculture, PO Box 550, Truro, NS, B2N 5E3, Canada.
Department of Engineering, Dalhousie University Faculty of Agriculture, PO Box 550, Truro, NS, B2N 5E3, Canada.
J Environ Manage. 2024 Jun;361:121249. doi: 10.1016/j.jenvman.2024.121249. Epub 2024 May 30.
This study investigated the influence of biosolid applications on soil carbon storage and evaluated nutrient management strategies affecting soil carbon dynamics. The research assessed alterations in soil pH, soil carbon stock, and soil nitrogen content within short-term and long-term biosolids-amended soils in Bible Hill, Nova Scotia, Canada, extending to a depth of 0-60 cm. The findings indicated an increase in soil pH with alkaline treatment biosolids (ATB) applications across both study sites, with a legacy effect on soil pH noted in the long-term biosolids-amended soil following a single ATB application over 13 years. Both sites demonstrated significant increases in soil total carbon (STC) and soil organic carbon (SOC) within the 0-30 cm soil depth after biosolid application, and soil inorganic carbon (SIC) accounted for approximately 5-10% of STC, specifically in the surface soil layer (0-15 cm). In the long-term study site, annual 14, 28 and 42 Mg ATB ha treatments resulted in a substantial rise in soil carbon stock (59.5, 60.1 and 68.0 Mg C ha), marking a 25% increase compared to control soil. The SOC content in biosolids-amended soil showed a declining trend with increasing soil depth at both study sites. Notably, the carbon stock in the short-term site was observed in composted biosolids (COMP) > ATB > liquid mesophilic anaerobically digested biosolids (LMAD) from the 0-60 cm soil depth. Approximately 79-80% of the variation in SOC response at both sites was concentrated within the top 30 cm soil. Soil total nitrogen (STN) showed no significant differences at the short-term site, and STN in biosolids-amended soil decreased with increasing soil depth at the long-term site. Biosolids-induced C retention coefficients (BCR) for ATB remained consistent at both sites, ranging from -13% to 31.4% with a mean of 11.12%. BCR values for COMP ranged from 1.9% to 34.4% with a mean of 18.73%, while those for LMAD exhibited variability, spanning from -6.2% to 106.3% with a mean of 53.9%.
本研究探讨了生物固体应用对土壤碳储存的影响,并评估了影响土壤碳动态的养分管理策略。该研究评估了在加拿大新斯科舍省比奇山的短期和长期生物固体处理土壤中,土壤 pH 值、土壤碳储量和土壤氮含量的变化,深度达 0-60cm。研究结果表明,碱性处理生物固体(ATB)的应用会导致土壤 pH 值升高,而且在经过 13 年的单次 ATB 应用后,长期生物固体处理土壤中仍存在土壤 pH 值的遗留效应。两个地点在生物固体处理后,0-30cm 土壤深度内的土壤总碳(STC)和土壤有机碳(SOC)均显著增加,土壤无机碳(SIC)占 STC 的 5-10%,特别是在表层土壤(0-15cm)。在长期研究地点,每年 14、28 和 42 Mg ATB ha 的处理导致土壤碳储量(59.5、60.1 和 68.0 Mg C ha)大幅增加,比对照土壤增加了 25%。生物固体处理土壤中的 SOC 含量随着两个研究地点土壤深度的增加呈下降趋势。值得注意的是,短期研究地点的碳储量在 composted biosolids (COMP) > ATB > liquid mesophilic anaerobically digested biosolids (LMAD) 中从 0-60cm 土壤深度。两个地点的 SOC 响应的约 79-80%的变化集中在 30cm 土壤表层内。短期研究地点的土壤总氮(STN)没有显著差异,而长期研究地点的生物固体处理土壤中 STN 随土壤深度的增加而减少。ATB 的生物固体诱导碳保留系数(BCR)在两个地点保持一致,范围为-13%至 31.4%,平均值为 11.12%。COMP 的 BCR 值范围为 1.9%至 34.4%,平均值为 18.73%,而 LMAD 的 BCR 值则变化较大,范围为-6.2%至 106.3%,平均值为 53.9%。