Hydrodynamic Modeling and Simulation of Water Residence Time in the Estuary of the Lower Amazon River

被引:18
|
作者
de Abreu, Carlos Henrique M. [1 ,2 ]
Cavalcanti Barros, Maria de Lourdes [3 ,4 ]
Brito, Daimio Chaves [5 ]
Teixeira, Marcelo Rassy [6 ]
da Cunha, Alan Cavalcanti [7 ]
机构
[1] Fed Univ Amapa UNIFAP, Postgrad Program Bionorte, Macapa 68903419, Brazil
[2] Amapa State Univ UEAP, Environm Engn Sch CEAM, Macapa 68900070, Brazil
[3] Fed Univ Amapa UNIFAP, Postgrad Course Environm Sci CPGCA TEDPLAN Projec, Macapa 68903419, Brazil
[4] Fed Univ Para UFPA, PRODERNA ITEC, Postgrad Program Nat Resources Engn Amazon, Belem 66075110, Para, Brazil
[5] Fed Univ Amapa UNIFAP, Dept Environm & Dev, Macapa 68903419, Brazil
[6] Fed Univ Para UFPA, Fac Civil & Environm Engn, BR-68464000 Tucurui, Brazil
[7] Univ Amapa UNIFAP, Dept Civil Engn, Macapa 68903419, Brazil
关键词
hydrodynamics; fluvial geomorphology; Amazonian estuary; dilution capacity; renovation rate; self-depuration; North Channel; Santana Channel; Amapa; TIDAL ASYMMETRY; FLOW; QUALITY; SHALLOW; TRANSFORMATION; DYNAMICS; NITROGEN; SYSTEM; LAKE; BAY;
D O I
10.3390/w12030660
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Studies about the hydrodynamic behavior in the lower Amazon River remain scarce, despite their relevance and complexity, and the Water Residence Time (Rt) of this Amazonian estuary remains poorly unknown. Therefore, the present study aims to numerically simulate three seasonal Rt scenarios based on a calibrated hydrodynamic numerical model (SisbaHiA) applied to a representative stretch of the lower Amazon River. The following methodological steps were performed: (a) establishing experimental water flow in natural channels; (b) statistically test numerical predictions (tidal range cycles for different hydrologic periods); and (c) simulating velocity fields and water discharge associated with Rt numerical outputs of the hydrodynamic model varied from 14 <= Rt <= 22 days among different seasonal periods. This change has shown the significant influence of hydrologic period and geomorphological features on Rt. Rt, in its turn, has shown significant spatial heterogeneity, depending on location and stretch of the channels. Comparative analyses between simulated and experimental parameters evidenced statistical correlations higher than 0.9. We conclude that the generated Rt scenarios were consistent with other similar studies in the literature. Therefore, they depicted the applicability of the hydrodynamics to the conservation of the Amazonian aquatic ecosystem, as well as its relevance for biochemical and pollutant dispersion studies, which still remain scarce in the literature.
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页数:29
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