Rampoldi E Ariel, Hang Susana, Barriuso Enrique
J Environ Qual. 2014 Mar;43(2):558-67. doi: 10.2134/jeq2013.09.0362.
The recognition of glyphosate [(-phosphonomethyl) glycine] behavioral patterns can be readily examined using a pedoclimatic gradient. In the present study, glyphosate adsorption-desorption and degradation were examined under different scenarios in relationship to soil properties and soil use applications. Three sites with varied pedoclimatic conditions and two crop sequences were selected. Adsorption-desorption and glyphosate distribution in mineralized, extractable, and nonextractable fractions were assessed under laboratory conditions. Glyphosate sorption was characterized by isotherms and glyphosate degradation using the distribution of C-glyphosate radioactivity among mineralized fractions, two extractable fractions (in water, ER1; in NHOH, ER2), and nonextractable fractions. Results showed sorption indices (distribution coefficient and Freundlich sorption coefficient : 13.4 ± 0.3-64.1 ± 0.9 L kg and 16.2-60.6, respectively), and hysteresis increased among soil sites associated with decreasing soil particle size <2 μm, soil organic matter, and other soil properties associated with soil granulometry. A multiple stepwise regression analysis was applied to estimate the relationship between values and soil properties. Cation exchange capacity, water field capacity, and Bray-1 P were the soil properties retained in the equation. Soils under continuous soybean [ (L.) Merr.] (monoculture) treatment exhibited reduced glyphosate adsorption and decreased hysteresis desorption relative to soils under rotation. To our knowledge, these results are the first to demonstrate that soils with identical properties exhibited different glyphosate retention capacities based on crop sequence. We propose possible explanations for this observation. Our results suggested that characterization of the variability in soil property gradients can serve to determine glyphosate behavioral patterns, which can establish a criterion for use in reducing potential environmental risks.
利用土壤气候梯度可以很容易地研究草甘膦[(膦酰基甲基)甘氨酸]的行为模式。在本研究中,研究了草甘膦在不同情景下与土壤性质及土壤利用应用相关的吸附-解吸和降解情况。选择了三个具有不同土壤气候条件的地点和两种作物轮作序列。在实验室条件下评估了矿化、可提取和不可提取部分中的草甘膦吸附-解吸及分布情况。草甘膦吸附通过等温线进行表征,草甘膦降解则利用C-草甘膦放射性在矿化部分、两个可提取部分(水中,ER1;在NH₄OH中,ER2)和不可提取部分中的分布来进行。结果显示吸附指数(分配系数和弗伦德利希吸附系数分别为:13.4±0.3 - 64.1±0.9 L/kg和16.2 - 60.6),并且与土壤颗粒尺寸<2μm减小、土壤有机质以及与土壤粒度相关的其他土壤性质相关的土壤地点之间的滞后现象增加。应用多元逐步回归分析来估计这些值与土壤性质之间的关系。阳离子交换容量、田间持水量和Bray-1 P是方程中保留的土壤性质。与轮作土壤相比,连续种植大豆[(L.)Merr.](单一栽培)处理下的土壤表现出草甘膦吸附减少和滞后解吸降低。据我们所知,这些结果首次证明具有相同性质的土壤基于作物轮作序列表现出不同的草甘膦保留能力。我们对这一观察结果提出了可能的解释。我们的结果表明,表征土壤性质梯度的变异性有助于确定草甘膦行为模式,这可以建立一个用于降低潜在环境风险的标准。