Effects of soil bulk density and corresponding soil infiltration rate on the migration and transformation of gibberellic acid.

IF 3.5 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Journal of contaminant hydrology Pub Date : 2024-12-08 DOI:10.1016/j.jconhyd.2024.104488
Xiaolei Hu, Linxian Huang, Huihua Chen, Liang Chen, Paul H Fallgren
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Abstract

High intensity agricultural activities can lead to a decrease in soil fertility and an increase in soil bulk density, which may significantly impact the migration and transformation of pesticides in soil. As a new widely-used micro-toxic pesticide, gibberellic acid (GA3) is more soluble and hydrophilic than most pesticides, which could readily migrate throughout the soil during water infiltration and impact groundwater quality. In this study, the leaching of GA3 in saturated soils with different bulk densities (1.15-1.75 g/cm3) and infiltration rates (0.2215-0.0017 mm/s) were analyzed using column experiments. The migration and distribution of GA3 in the soil with a depth of 50 cm were also investigated. The results indicated that GA3 could completely penetrate the soil with bulk densities less than 1.45 g/cm3, and GA3 mass variation in the effluent was normally distributed. The maximum mass of GA3 in the effluent was calculated using the equation Moutlet(max) = 79.01 t-0.97 (R2 = 0.9811), and 83.69-93.16 % mass of the added GA3 migrated downward in the soil. The analysis of the distribution of GA3 in the soil showed that GA3 accumulated in the upper soil layers with depths of 0-25 cm (the total depth of soil was 50 cm). In addition, the residual and hydrolyzed GA3 amounts in the soil were 75.07-96.47 % and 5-30 % of the added GA3, respectively. Overall, the soil bulk density and irrigation volume determine what type of impact that GA3 may potentially have on the environment.

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高强度的农业活动会导致土壤肥力下降,土壤容重增加,这可能会严重影响农药在土壤中的迁移和转化。赤霉素(GA3)是一种广泛使用的新型微毒农药,与大多数农药相比,它的溶解性和亲水性更强,在水的渗透过程中很容易迁移到整个土壤中,影响地下水水质。本研究利用柱状实验分析了 GA3 在不同容重(1.15-1.75 g/cm3)和不同渗透速率(0.2215-0.0017 mm/s)的饱和土壤中的浸出情况。此外,还研究了 GA3 在 50 厘米深的土壤中的迁移和分布情况。结果表明,GA3 可以完全渗透到体积密度小于 1.45 g/cm3 的土壤中,且 GA3 在污水中的质量变化呈正态分布。根据公式 Moutlet(max) = 79.01 t-0.97 (R2 = 0.9811)计算出出水中 GA3 的最大质量,添加的 GA3 有 83.69-93.16% 的质量在土壤中向下迁移。GA3 在土壤中的分布分析表明,GA3 在 0-25 厘米深的上层土壤中积累(土壤总深度为 50 厘米)。此外,土壤中 GA3 的残留量和水解量分别为添加量的 75.07%-96.47% 和 5%-30%。总之,土壤容重和灌溉量决定了 GA3 可能对环境产生的潜在影响类型。
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来源期刊
Journal of contaminant hydrology
Journal of contaminant hydrology 环境科学-地球科学综合
CiteScore
6.80
自引率
2.80%
发文量
129
审稿时长
68 days
期刊介绍: The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide). The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.
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