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饮用水库中二氧化碳排放与富营养化的相互作用:一种三维生态建模方法。

Interaction between carbon dioxide emissions and eutrophication in a drinking water reservoir: A three-dimensional ecological modeling approach.

机构信息

Department of Environmental Science, School of Environmental Science and Engineering, Sun Yat-sen University, Guangzhou 510275, China.

出版信息

Sci Total Environ. 2019 May 1;663:369-379. doi: 10.1016/j.scitotenv.2019.01.336. Epub 2019 Jan 29.

Abstract

We developed a three-dimensional model to study the dynamics of carbon dioxide (CO) emission from a subtropical drinking water reservoir. The quantitative effects of dissolved CO concentration on phytoplankton growth were coupled in an inorganic carbon module. Water quality monitoring was carried out to calibrate and validate the model. The simulated surface CO concentrations showed no significant difference between seasons (p>0.05). Regarding the spatial distribution, high CO concentrations were observed in the inflow and dam regions (p<0.05). Four scenarios of different atmospheric CO pressures and eutrophic levels were simulated to test the following hypotheses: (1) eutrophication will reverse the carbon budgets in reservoir systems and (2) rising CO levels will increase phytoplankton biomass. The results showed that water quality improvements will promote the emission of CO into the atmosphere. Simultaneously, the elevated CO in the air will stimulate algal biomass, especially in nutrient-rich systems. The systematic analysis of carbon cycling revealed the different internal transformation rates under different scenarios and showed that 32% of carbon was removed via CO emission and carbon burial. The interaction provides a novel direction to understand the feedback loops between aquatic ecosystems and increasing CO pressure in the future.

摘要

我们开发了一个三维模型来研究亚热带饮用水库中二氧化碳(CO)排放的动力学。溶解 CO 浓度对浮游植物生长的定量影响通过无机碳模块耦合在一起。进行了水质监测以校准和验证模型。模拟的表层 CO 浓度在季节之间没有显著差异(p>0.05)。关于空间分布,在入流区和大坝区观察到高 CO 浓度(p<0.05)。模拟了四种不同大气 CO 压力和富营养化水平的情景,以检验以下假设:(1)富营养化将逆转水库系统中的碳预算;(2)CO 水平升高将增加浮游植物生物量。结果表明,水质改善将促进 CO 排放到大气中。同时,空气中的 CO 会刺激藻类生物量增加,尤其是在营养丰富的系统中。对碳循环的系统分析揭示了不同情景下的不同内部转化速率,并表明 32%的碳通过 CO 排放和碳埋藏去除。这种相互作用为理解未来水生生态系统与 CO 压力增加之间的反馈循环提供了一个新的方向。

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