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人工新湖的化学制约因素。

Chemical constraints on new man-made lakes.

机构信息

Programa de Pós-Graduação em Ecologia e Recursos Naturais, Departamento de Hidrobiologia, Universidade Federal de São Carlos, Rodovia Washington Luiz, km 235, Cx. Postal 676, 13565-905, São Carlos, São Paulo, Brazil,

出版信息

Environ Monit Assess. 2013 Dec;185(12):10177-90. doi: 10.1007/s10661-013-3322-0. Epub 2013 Jul 23.

Abstract

The formation of reservoirs often affects water quality strongly, with the changes in the physicochemical properties being ascribed to decomposition of remaining organic matter arising from leaching and (biological and chemical) breakdown processes. In this study, experiments under laboratory conditions were performed to show that the nature of the course particulate organic matter (CPOM; i.e., leaves, branches, barks, and litter) determines the decomposition kinetics in new reservoirs. Effects on the water quality can be of short-, mid-, and long-term duration for all types of CPOM, as indicated in the mathematical modeling of the decomposition kinetics. Leaves and litter displayed the shortest half-life times (51 and 40 days, respectively) and the highest potential of leaching/oxidation of labile compounds (19 and 21%, respectively). On the other hand, decomposition of branches and barks generated the lowest oxygen consumption (74 and 44 mg oxygen/g dry mass (DM), respectively). During formation of the reservoir, the incorporation and decomposition of organic matter prevailed over material exportation. Therefore, in addition to a decrease in oxygen availability the concentration of biochemical oxygen demand (BOD) and nutrients increased. After the filling stage, there was significant loss of organic matter via oxidation, sedimentation, biological assimilation, and export, thus causing the BOD concentration and the fertility of the water to decrease.

摘要

水库的形成通常会强烈影响水质,其理化性质的变化归因于剩余有机物的分解,这些有机物来自浸出和(生物和化学)分解过程。本研究通过实验室条件下的实验表明,新水库中颗粒有机物质(CPOM;即叶片、树枝、树皮和凋落物)的性质决定了其分解动力学。所有类型的 CPOM 对水质的影响都具有短期、中期和长期的持续时间,这在分解动力学的数学建模中有所体现。叶片和凋落物的半衰期最短(分别为 51 天和 40 天),易降解化合物的浸出/氧化潜力最高(分别为 19%和 21%)。另一方面,树枝和树皮的分解产生的耗氧量最低(分别为 74 和 44 毫克氧/克干物质(DM))。在水库形成过程中,有机物的掺入和分解占主导地位,超过了物质的输出。因此,除了氧气供应减少外,生化需氧量(BOD)和养分的浓度也会增加。在蓄水阶段之后,大量的有机物通过氧化、沉淀、生物同化和输出而损失,从而导致 BOD 浓度和水的肥力下降。

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