water Article Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin Rogério Ribeiro Marinho 1,2,* , Naziano Pantoja Filizola Junior 1,3 and Édipo Henrique Cremon 4 1 Postgraduation Program CLIAMB, Instituto Nacional de Pesquisas da Amazônia (INPA)—Universidade do Estado do Amazonas (UEA), Ave. André Araújo, 2936, Manaus CEP 69060-001, Brazil; nazianofi
[email protected] 2 Departamento de Geografia, Universidade Federal do Amazonas (UFAM), Ave. General Rodrigo Otávio, Jordão Ramos 6200, Campus Universitário, Coroado I, Manaus CEP 69077-000, Brazil 3 Departamento de Geociências, Universidade Federal do Amazonas (UFAM), Ave. General Rodrigo Otávio, Jordão Ramos 6200, Campus Universitário, Coroado I, Manaus CEP 69077-000, Brazil 4 Grupo de Estudos em Geomática (GEO), Instituto Federal de Goiás (IFG), Rua 75, 46, Setor Central, Goiânia CEP 74055-110, Brazil;
[email protected] * Correspondence:
[email protected] Received: 5 March 2020; Accepted: 7 April 2020; Published: 9 April 2020 Abstract: This article analyzes the flows of water and total suspended sediment in different reaches in the lower course of the Negro River, the largest fluvial blackwater system in the world. The area under study is the Anavilhanas Archipelago, which is a complex multichannel reach on the Negro River. Between the years 2016 and 2019, data about water discharge, velocity, and concentration of total suspended solids (TSS) were acquired in sample sections of the Negro River channels located upstream, inside, and downstream of the Anavilhanas Archipelago. In the study area, the Negro River drains an area greater than 700,000 km2, and the mean water discharge observed before the Anavilhanas was about 28.655 m3 s 1, of which 97% flows through two channels of the Archipelago close to the · − right and left banks.