Global Centre for Environmental Remediation (GCER), Advanced Technology Centre, College of Engineering, Science and Environment, The University of Newcastle, Callaghan, NSW, 2308, Australia; Department of Natural Resources, Faculty of Applied Sciences, Sabaragamuwa University, Belihuloya, 70140, Sri Lanka.
School of Mathematical and Physical Sciences, Faculty of Science, The University of Newcastle, Callaghan, NSW, 2308, Australia.
J Environ Manage. 2021 Apr 15;284:112008. doi: 10.1016/j.jenvman.2021.112008. Epub 2021 Jan 30.
Biosolids produced at wastewater treatment facilities are extensively used in agricultural land and degraded mine sites to improve soil health and soil organic carbon (SOC) stocks. Many studies have reported increases in SOC due to application of biosolids to such sites. However, lack of a comprehensive quantification on overall trends and changes of magnitude in SOC remains. Here, we performed a meta-analysis to identify drivers with a relationship with SOC stocks. A meta-regression of 297 treatments found four variables with a relationship with SOC stocks: cumulative biosolids carbon (C) input rate, time after application, soil depth and type of biosolids. The cumulative biosolids C input rate was the most influencing driver. The highest mean difference for SOC% of 3.3 was observed at 0-15 cm soil depth for a cumulative C input of 100 Mg ha at one year after biosolids application. Although years after biosolids application demonstrated a negative relationship with SOC stocks, mineralization of C in biosolids-applied soils is slow, as indicated with the SOC% decrease from 4.6 to 2.8 at 0-15 cm soil depth over five years of 100 Mg ha biosolids C input. Soil depth illustrated a strong negative effect with SOC stocks decreasing by 2.7% at 0-15 cm soil depth at a cumulative biosolids C input of 100 Mg ha over a year. Overall, our model estimated an effect of 2.8 SOC% change, indicating the application of biosolids as a viable strategy for soil C sequestration on a global scale.
污水处理厂产生的生物固体被广泛应用于农业土地和退化矿山,以改善土壤健康和土壤有机碳(SOC)储量。许多研究报告称,由于将生物固体应用于这些地点,SOC 有所增加。然而,SOC 总体趋势和变化幅度的综合量化仍然缺乏。在这里,我们进行了荟萃分析,以确定与 SOC 储量相关的驱动因素。对 297 种处理方法的元回归发现,有四个变量与 SOC 储量有关:生物固体碳(C)累积输入率、应用后时间、土壤深度和生物固体类型。生物固体 C 累积输入率是最具影响力的驱动因素。在生物固体应用一年后,累积 C 输入为 100 Mg ha,0-15 cm 土壤深度的 SOC%最高差异为 3.3。尽管生物固体应用后的年份与 SOC 储量呈负相关,但生物固体应用土壤中 C 的矿化速度较慢,这表明在 100 Mg ha 生物固体 C 输入的五年内,0-15 cm 土壤深度的 SOC%从 4.6 下降到 2.8。土壤深度对 SOC 储量具有强烈的负效应,在一年中,累积生物固体 C 输入为 100 Mg ha 时,0-15 cm 土壤深度的 SOC 储量下降了 2.7%。总的来说,我们的模型估计 SOC 变化率为 2.8%,表明在全球范围内,应用生物固体是一种可行的土壤 C 固存策略。