洪泛平原土壤雨水径流中溶解有机质和颗粒有机质的淋滤动力学

IF 4.4 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Hui Xia , Zhiquan Yan , Kui Huang , Bangchi Wang , Tonghuan Li , Qunfeng Chen
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引用次数: 0

摘要

洪泛平原土壤有机质在雨水径流过程中经历了复杂的淋滤过程,直接影响流域水环境质量。通过模拟降雨试验,研究了黄河上游河漫滩土壤中溶解有机质(DOM)和颗粒有机质(POM)的淋滤行为。结果表明,DOM和POM在降雨初期(0 ~ 20 min)大量释放,随后浸出速率逐渐下降并趋于稳定。色氨酸样物质在DOM中占主导地位,占总DOM释放量的45% - 55%,而腐殖质物质则表现出延迟释放的模式。POM的释放受粒径的显著影响,早期径流中以小颗粒为主,25 min后大颗粒更加突出。POM的二维相关光谱(2D-COS)显示功能基团的顺序变化,依次为:醇类;脂肪族化合物;羧酸>;酯/酮比;芳香族化合物。发现多糖和脂肪族化合物在径流中优先浸出。此外,还观察到DOM和POM之间的转化,较大的POM颗粒逐渐转化为DOM,从而影响径流的物理化学特征。该研究强调了降雨期间DOM和POM淋滤行为的明显差异,蛋白质类化合物和脂肪族化合物的释放速度更快,较小的颗粒更容易被调动到径流中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Leaching dynamics of dissolved organic matter and particulate organic matter in stormwater runoff from floodplain soils

Leaching dynamics of dissolved organic matter and particulate organic matter in stormwater runoff from floodplain soils
Organic matter in floodplain soils undergoes complex leaching dynamics during stormwater runoff, directly impacting the water environmental quality of river basin. This study explored the leaching behavior of dissolved organic matter (DOM) and particulate organic matter (POM) in soils from the upper Yellow River floodplain through simulated rainfall experiments. The results showed that DOM and POM were extensively released into the initial rainfall phase (0–20 min), followed by a gradual decline and stabilization in leaching rates. Tryptophan-like substances dominate in the DOM, contributing 45 %–55 % of the total DOM released, while humic substances exhibited a delayed release pattern. POM release was significantly affected by particle size, with smaller particles predominant in the early runoff and larger particles becoming more prominent after 25 min. Two-dimensional correlation spectroscopy (2D-COS) of POM revealed a sequential shift in functional groups, following the order: alcohols > aliphatic compounds > carboxylic acids > esters/ketones > aromatic compounds. Polysaccharides and aliphatic compounds were found to leach preferentially during runoff. Additionally, a transformation between DOM and POM was observed, with larger POM particles gradually converting into DOM, thereby influencing the physicochemical characteristics of the runoff. This study highlights distinct differences in the leaching behavior of DOM and POM during rainfall events, with protein-like and aliphatic compounds showing faster release rates, and smaller particles being more readily mobilized into runoff.
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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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