Investigation of physical properties and suspended particulate matter discharge in a macrotidal estuary at the Amazon-semiarid transition zone

被引:0
作者
dos Santos, Vinicius Henrique Maciel [1 ]
Dias, Francisco Jose da Silva [1 ]
Dottori, Marcelo [2 ]
Torres Junior, Audalio Rebelo [1 ]
Santos, Ricardo Luvizotto [3 ]
Soares, Romulo de Araujo [1 ]
Ribeiro Junior, Julio Cesar Martins [1 ]
Serejo, Jefferson Horley Feitosa [1 ]
Lima, Hugo Pereira [1 ]
Azevedo, Igor Hamid Ribeiro [1 ]
机构
[1] Univ Fed Maranhao UFMA, Lab Hidrodinam Costeira Estuarina & Aguas Interior, Programa Posgrad Oceanog PPGOceano, Cidade Univ Dom Delgado, BR-65080805 Sao Luis, MA, Brazil
[2] Univ Sao Paulo, Lab Hidrodinam Costeira LHiCO, Inst Oceanog IO, Praca Oceanog 191,Cidade Univ, BR-05508120 Sao Paulo, SP, Brazil
[3] Univ Fed Maranhao UFMA, Lab Ecotoxicol LabEcotox, Programa Posgrad Oceanog PPGOceano, Cidade Univ Dom Delgado, BR-65080805 Sao Luis, MA, Brazil
关键词
Estuarine complex; Hydrodynamics; Current field; Macrotidal estuary; Hydraulic barrier; PEARL RIVER DELTA; TURBIDITY MAXIMUM; SALT INTRUSION; SEDIMENT TRANSPORT; DRY SEASON; SALINITY; CIRCULATION; DISPERSION; INTERFACE; DYNAMICS;
D O I
10.1016/j.rsma.2023.103194
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
This study evaluated the hydrodynamic circulation and discharge of Suspended Particulate Matter (SPM) in the Arraial-Sao Jose Estuarine Complex (ASJEC) located at the Amazon-semiarid interface, northeastern Brazil. Quasi-synoptic data were collected in the rainy and dry seasons of 2017 under spring tide conditions. For each sampling event, two mooring stations (one downstream [S-A] and one upstream [S-B]) were deployed during a complete tidal cycle. The physical characteristics in the rainy and dry seasons enabled dividing the estuarine complex into zones, with a mixing zone/coastal zone interface and a tidal river zone/mixing zone interface. The estuary is vertically quasi-homogeneous, indicating conditions of high vertical instability. The currents at the stations were more intense during the flood tide, demonstrating the importance of the marine component in the region. The estuarine system ranged from partially mixed to well mixed at both stations in the rainy season and was well mixed at both stations in the dry season. Total salt transport was towards the upstream portion of the estuary, suggesting the accumulation of matter in the ASJEC, most likely associated with the entrance of marine waters. The input of coastal water in the ASJEC intensifies the baroclinic pressure gradient, which creates a hydraulic barrier, indicating that SPM discharges from the continental drainage to the estuary and is interrupted from the estuary to the adjacent continental shelf. (c) 2023 Elsevier B.V. All rights reserved.
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页数:16
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