Department of the Sciences of Agriculture, Food and Environment, University of Foggia, via Napoli 25, 71122 Foggia, Italy.
Department of Soil, Plant and Food Sciences, University of Bari "Aldo Moro", via Amendola 165/A, 70126 Bari, Italy.
Sci Total Environ. 2018 Apr 15;621:67-74. doi: 10.1016/j.scitotenv.2017.11.152. Epub 2017 Nov 22.
Arsenic (As) occurs in soils mostly in inorganic forms, whereas the organic forms usually occur only in trace amounts. Peatlands are waterlogged, generally anoxic, organic soils representing the first step in coal formation; the contribution of organic vs. inorganic As species in this environment has received little research attention. Here, 57 peat samples collected throughout a 4-m deep, free-floating mire were analysed for total As and for its organic species, including dimethylarsinic acid (DMA), methylarsonic acid (MA), trimethylarsine oxide (TMAO) and arsenobetaine (AB), by HPLC-ICPMS. Aqueous trifluoroacetic acid was used as extractant, resulting in an average extraction efficiency of almost 80%. Total As concentration throughout the profile ranged between 0.2 and 9.8mg/kg (mean: 1.4±1.2mg/kg). Organic As species (DMA+MA+TMAO+AB) accounted, on average, for 28±10% of total As (range: 6-51%), and for 37±13% of the extracted As (range: 7-64%). The relative abundance of organoarsenicals generally followed the order DMA>TMAO~MA≫AB. A positive correlation (p<0.001) was found among all organic As compounds, whereas their concentrations were negatively correlated with total sulfur content. The submerged zone (bottom 300cm) showed average and maximum concentrations of organoarsenic compounds that were almost twice those found in the top 100cm. This study shows that significant proportions of methylated As species occur even in peat samples characterized by low total As concentration (mostly <2mg/kg). Finally, this work provides the first evidence of organoarsenic species in free-floating mires, i.e., a globally distributed but scarcely investigated ecosystem.
砷(As)在土壤中主要以无机形式存在,而有机形式通常只以痕量存在。泥炭地是水饱和的,通常是缺氧的,有机土壤代表了煤炭形成的第一步;在这种环境中,有机砷和无机砷的贡献受到的关注很少。在这里,通过高效液相色谱-电感耦合等离子体质谱法(HPLC-ICPMS)分析了 57 个从 4 米深的自由漂浮沼泽中采集的泥炭样本中的总砷及其有机形态,包括二甲基砷酸(DMA)、砷酸(MA)、三甲砷氧化物(TMAO)和砷甜菜碱(AB)。采用三氟乙酸水溶液作为提取剂,平均提取效率接近 80%。整个剖面的总砷浓度范围为 0.2 至 9.8mg/kg(平均值:1.4±1.2mg/kg)。有机砷形态(DMA+MA+TMAO+AB)平均占总砷的 28±10%(范围:6-51%),占提取砷的 37±13%(范围:7-64%)。有机砷的相对丰度通常遵循 DMA>TMAO~MA≫AB 的顺序。所有有机砷化合物之间均存在正相关(p<0.001),而其浓度与总硫含量呈负相关。水下区(底部 300cm)的有机砷化合物的平均和最高浓度几乎是上覆层(100cm 以内)的两倍。本研究表明,即使在总砷浓度较低(主要<2mg/kg)的泥炭样本中,甲基化砷的比例也相当大。最后,这项工作首次提供了自由漂浮沼泽中有机砷形态的证据,即全球分布但研究甚少的生态系统。