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首页> 外文期刊>Environmental Monitoring and Assessment >Rapid photodegradation of terrestrial soil dissolved organic matter (DOM) with abundant humic-like substances under simulated ultraviolet radiation
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Rapid photodegradation of terrestrial soil dissolved organic matter (DOM) with abundant humic-like substances under simulated ultraviolet radiation

机译:模拟紫外线辐射下富含腐殖质类物质对土壤可溶性有机物(DOM)的快速光降解

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Solar ultraviolet (UV) radiation exhibits a significant degradation for dissolved organic matter (DOM) in natural water ecosystems. However, research on photodegradation process of terrestrial components (e.g., humic-like substances) of DOM are limited due to drastic water dilution and rapid degradation. Here, photochemical degradation of terrestrial soil DOM with abundant humic-like substances from different land use were investigated by utilizing spectral technologies. Simulated UV radiation caused obvious losses on concentration, component structures, and fluorescence characteristic of soil DOM samples. The correlations between absorption specific parameters (a(280), SUVA(254), and S-R) and dissolved organic carbon (DOC) were especially pronounced (p < 0.05), which could be used as valid indicators to determine changes in DOM composition and molecular size during photobleaching process. The decreases of DOM fluorescence intensity were corresponded to first-order kinetic and half-life reactions. The greatest reduction on fluorescence intensity (31.56-81.97%) belonged to peak C (i.e., humic-like substances). Overall, DOM from forest and grass soil ecosystems was more easily photochemical degraded than anthropogenic soil DOM. Enhancive contribution of fresh DOM formed by photodegradation increased autochthonous characteristic and bioavailable nutrition by increasing biological index (BIX) values and ammonia nitrogen (NH4+-N) concentration. The slight microbial decomposition effects on DOM happened in unsterilized dark condition. Our findings provided insights for understanding the rapid photodegradation processes of composition and structure of terrestrial DOM.
机译:太阳紫外线(UV)辐射对天然水生态系统中的可溶性有机物(DOM)表现出显着的降解作用。然而,由于水的急剧稀释和快速降解,对DOM的陆地组分(例如腐殖质样物质)的光降解过程的研究受到限制。在这里,利用光谱技术研究了来自不同土地利用的大量腐殖质样物质对陆地土壤DOM的光化学降解。模拟的紫外线辐射对土壤DOM样品的浓度,组分结构和荧光特性造成明显损失。吸收特定参数(a(280),SUVA(254)和SR)与溶解有机碳(DOC)之间的相关性特别明显(p <0.05),可以用作确定DOM组成和变化的有效指标。光漂白过程中的分子大小。 DOM荧光强度的降低对应于一级动力学和半衰期反应。荧光强度的最大降低(31.56-81.97%)属于峰C(即腐殖质样物质)。总体而言,来自森林和草地土壤生态系统的DOM比人为土壤DOM更容易光化学降解。通过增加生物指标(BIX)值和氨氮(NH4 + -N)的浓度,光降解形成的新鲜DOM的增强作用增加了自发特性和生物利用营养。微生物对DOM的轻微分解作用发生在未灭菌的黑暗条件下。我们的发现为理解地面DOM的快速光降解过程提供了见识。

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