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Modeling nutrients, oxygen and critical phosphorus loading in a shallow reservoir in China with a coupled water quality - Macrophytes model

机译:水质耦合模拟中国浅层水库中的养分,氧气和临界磷负荷-Macrophytes模型

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Many macrophyte-dominated clear lakes switch to a phytoplankton-dominated turbid state when the lake becomes eutrophic. An existing Yugiao Reservoir Water Quality Model (YRWQM) and the macrophyte submodel were coupled to simulate the effect of submerged macrophytes on nutrients and dissolve oxygen cycles in a shallow reservoir in China. The level of phosphorus loading in a transition from a clear to turbid state was addressed using the integrated model. The model runs from seedling establishment until dying out, from March 1 to July 18 in 2009. The simulations were performed for a contingent range of P loadings, starting from three different initial conditions. The results indicated that the integrated model improves accuracy of predictions compared to YRWQM. The concentrations of nutrients declined slightly during the macrophyte growth period in the reservoir and dissolved oxygen increased slightly. Although nutrient concentrations increased by submerged macrophyte release during the extinction period, the effect on the nutrients was less than that of transfer with nutrient-rich water. More released nutrients may enhance increases in substantial abundance. The critical phosphorus loading level during a switch from the clear to turbid state was estimated by these scenarios. The threshold for the switch is similar to 6.1 mgP m(-2) d(-1) with an initial total phosphorus concentration of 160 mu g l(-1). Moreover, the results demonstrated that the switch was also dependent on the initial total phosphorus concentration. These results suggest that the reservoir in a clear water state is at risk of a switch as nutrient levels are close to the critical levels. (C) 2016 Elsevier Ltd. All rights reserved.
机译:当湖泊变得富营养化时,许多以大型植物为主的清澈湖泊会转变为以浮游植物为主的混浊状态。结合现有的鱼g水库水质模型(YRWQM)和大型植物亚模型,模拟了中国浅水库中大型植物的淹没对养分的影响并溶解了氧气。使用集成模型解决了从透明状态到浑浊状态过渡过程中磷的负载水平。该模型从2009年3月1日至7月18日从苗木建立到死亡,一直运行。从三个不同的初始条件开始,针对一定范围的P负荷进行了模拟。结果表明,与YRWQM相比,集成模型提高了预测的准确性。在水生植物的生长期间,养分的浓度略有下降,溶解氧略有增加。尽管在灭绝时期淹没的大型植物释放出养分,从而增加了养分的浓度,但对养分的影响却小于用富养分的水转移的养分。释放出更多的养分可能会增加实质性丰度的增加。通过这些场景,可以估算出从透明状态转变为浑浊状态期间的临界磷负荷水平。切换的阈值类似于6.1 mgP m(-2)d(-1),初始总磷浓度为160μgl(-1)。此外,结果表明,转换也取决于初始总磷浓度。这些结果表明,当营养水平接近临界水平时,处于清水状态的水库有转换风险。 (C)2016 Elsevier Ltd.保留所有权利。

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