EMBRAPA Soils, Rua Jardim Botânico, 1024, 22460-000, Rio de Janeiro, RJ, Brazil.
EMBRAPA Soils, Rua Jardim Botânico, 1024, 22460-000, Rio de Janeiro, RJ, Brazil; Program of Territorial Development and Public Policy, Federal Rural University of Rio de Janeiro, Seropedica 23890-000, Brazil.
Environ Pollut. 2020 Nov;266(Pt 1):115298. doi: 10.1016/j.envpol.2020.115298. Epub 2020 Aug 7.
The global increase of food production has been achieved mainly through the intensive use of inputs such as pesticides. Once released to the soil, sorption (which could be represented by Freundlich solid-water distribution coefficients - K) and degradation are two governing processes that determine the distribution and persistence of pesticides in the environment. In spite of the huge dataset, the only apparent generalisation is the high correlation between K and soil organic matter (SOM) content. However, in this work no correlation was observed between K and organic C content (OC) and so the obtained K (K normalised by OC) spread out in a wide range: 1100 to 11,400 mL g for abamectin; and 30-150 mL g for atrazine, both ranges corroborate with data from literature. These high variabilities indicate that other soil components or SOM quality strongly interfere in the pesticide sorption in addition to SOM content. Seeking to estimate the influence of SOM quality in the abamectin and atrazine K values, the humic acids, a fraction of the SOM, was analysed by C nuclear magnetic resonance spectroscopy (C NMR) and Principal Component (PC) Regression. The first PC of C NMR spectra presented negative loadings for aliphatic compounds and positive loadings for aryl C, typical of partially oxidised pyrogenic C. Their scores showed strong correlation with the abamectin K values (R = 0.91, p < 5 10) and weaker with atrazine K (R = 0.63, p < 0.0001), in addition to a smaller standardised slope: 1.01 for abamectin and 0.76 for atrazine. These results could be explained by the higher hydrophobicity of abamectin, being thus more prone to interact with the polycondensed aryl groups from the pyrogenic C. It is also important to highlight that humic acids are useful proxies for understanding the paramount interaction of SOM with pesticides.
全球粮食产量的增加主要是通过大量使用农药等投入品来实现的。一旦释放到土壤中,吸附(可以用弗伦德利希固-水分配系数 K 来表示)和降解是决定农药在环境中分布和持久性的两个主要过程。尽管有大量的数据,但唯一明显的概括是 K 与土壤有机质(SOM)含量之间存在高度相关性。然而,在这项工作中,没有观察到 K 与有机碳(OC)含量之间的相关性,因此得到的 K(用 OC 归一化的 K)分布在很宽的范围内:阿维菌素为 1100 至 11400 mL/g;莠去津为 30-150 mL/g;这两个范围都与文献中的数据相符。这些高度的变异性表明,除了 SOM 含量外,其他土壤成分或 SOM 质量强烈干扰了农药的吸附。为了估计 SOM 质量对阿维菌素和莠去津 K 值的影响,对土壤有机质的一个组成部分腐殖酸进行了 13 C 核磁共振波谱(C NMR)和主成分(PC)回归分析。C NMR 光谱的第一主成分呈现出脂肪族化合物的负载荷和芳族 C 的正载荷,这是部分氧化的热解 C 的典型特征。它们的得分与阿维菌素 K 值呈强烈相关(R=0.91,p<0.0001),与莠去津 K 值的相关性较弱(R=0.63,p<0.0001),并且标准化斜率较小:阿维菌素为 1.01,莠去津为 0.76。这些结果可以用阿维菌素的较高疏水性来解释,因为它更容易与热解 C 的多缩芳族基团相互作用。还需要强调的是,腐殖酸是理解 SOM 与农药之间相互作用的有用指标。