Environmental Science Department, University of Arizona, United States of America.
Pima County Regional Wastewater Reclamation Department, United States of America.
Sci Total Environ. 2021 Nov 1;793:148449. doi: 10.1016/j.scitotenv.2021.148449. Epub 2021 Jun 18.
This field study investigated the impact of long-term land application of biosolids on PFAS presence in soils that received annual repetitive land application of Class B biosolids from 1984 to 2019. Soil samples were collected from three depths of 30.5, 91 and 183 cm below land surface. Biosolid and groundwater samples used for irrigation were also collected. Concentrations measured for 18 PFAS compounds were evaluated to assess incidence rates and potential impact on groundwater. No PFAS analytes were detected at the three sampling depths for soil samples collected from undisturbed sites with no history of agriculture, irrigation, or biosolids application (background control sites). Relatively low mean concentrations of PFAS ranging from non-detect to 1.9 μg/kg were measured in soil samples collected from sites that were used for agriculture and that received irrigation with groundwater, but never received biosolids. PFAS concentrations in soils amended with biosolids were similarly low, ranging from non-detect to a mean concentration of 4.1 μg/kg. PFOS was observed at the highest concentrations, followed by PFOA for all locations. PFAS detected in the irrigation water were also present in the soil. These results indicate that biosolids and irrigation water are both important sources of PFAS present in the soils for all of the study sites. Not all PFAS detected in the biosolids were detected in the soil. Very long chain PFAS present in the biosolids were not detected or were detected at very low levels for soil, suggesting potential preferential retention within the biosolids. The precursor NMeFOSAA was present at the second highest concentrations in the biosolids but not detected in soil, indicating possible occurrence of transformation reactions. The total PFAS soil concentrations exhibited significant attenuation with depth, with a mean attenuation of 73% at the 183 cm depth. Monotonically decreasing concentrations with depth were observed for the longer-chain PFAS.
本田间研究调查了长期土地应用生物固体对土壤中全氟辛烷磺酸 (PFAS) 存在的影响,这些土壤在 1984 年至 2019 年期间每年重复接受 B 级生物固体的土地应用。从地表以下 30.5、91 和 183 厘米三个深度采集土壤样本。还采集了用于灌溉的生物固体和地下水样本。评估了测量的 18 种 PFAS 化合物的浓度,以评估其发生率和对地下水的潜在影响。在未受干扰且没有农业、灌溉或生物固体应用史(背景对照点)的地点采集的土壤样本的三个采样深度均未检测到任何 PFAS 分析物。在从未接收过生物固体的农业和地下水灌溉用地采集的土壤样本中,测量到相对较低浓度的 PFAS,范围从未检出到 1.9μg/kg。用生物固体改良的土壤中 PFAS 浓度也较低,范围从未检出到平均浓度 4.1μg/kg。所有地点的 PFOS 浓度最高,其次是 PFOA。灌溉水中检测到的 PFAS 也存在于土壤中。这些结果表明,生物固体和灌溉水是所有研究地点土壤中存在的 PFAS 的重要来源。并非所有在生物固体中检测到的 PFAS 都在土壤中检测到。生物固体中存在的非常长链 PFAS 未检出或检出水平非常低,表明其在生物固体中可能存在优先保留。生物固体中存在的前体 NMeFOSAA 浓度位居第二,但在土壤中未检出,表明可能发生了转化反应。土壤中总 PFAS 浓度随深度呈显著衰减,在 183 厘米深度处平均衰减 73%。较长链 PFAS 表现出随深度单调递减的浓度。