Abstract
Bamen Bay is located at the intersection of the Wenjiao River and Wenchang River in Hainan Province (China), where mangroves have been facing a threat of water quality deterioration. Therefore, it is imperative to study the characteristics of the surface water quality on a watershed scale. Water samples were collected three times from 36 monitoring sites from 2015 to 2016. It was found that nitrate was the main inorganic nitrogen form and all the surface water types were alkaline. Meanwhile, aquaculture water had high content of nitrogen, total phosphorus, chlorophyll a (Chl.a), total organic carbon (TOC), and chemical oxygen demand (COD). Significant spatial and temporal variations were found for most parameters. However, stable isotopes of δD and δ18O indicated that river water mainly originated from atmospheric precipitation and experienced strong evaporation. The water chemistry and isotopes of the Bamen Bay, mangroves, and aquaculture water were initially affected by the mixing of fresh water and seawater, followed by evaporation. The river and reservoir water chemistry were mainly controlled by water–rock interactions and cation exchange as deduced from the ionic relationships and Gibbs plots. These interactions involved the dissolution of calcite-, bicarbonate-, carbonate-, and calcium-containing minerals. Oxidized environments (river, reservoir, and Bamen Bay) were conducive for nitrification, while anaerobic conditions (mangrove and aquaculture water) were beneficial to the reduced nitrogen forms.
Highlights
Rivers carry dissolved elements and suspended solids from various sources and/or tributaries, and deposit them in different locations or transfer them to lakes or oceans [1,2,3]
General water chemistry and stable isotopes of the surface water are reported in S1 Table. pH ranged from 7.94 to 9.43, showing that the all the water systems were alkaline, with the order of pH as: reservoir > aquaculture > mangrove > Bamen Bay > river
Our research focused on the water chemistry composition and stable isotopes, and determining the surface water controlling factors in the Bamen Bay watershed, where a natural reservation of mangroves is located
Summary
Rivers carry dissolved elements and suspended solids from various sources and/or tributaries, and deposit them in different locations or transfer them to lakes or oceans [1,2,3]. Rivers play a major role in the global water cycle. River water chemistry or quality provides information on chemical weathering processes on a basin scale, and reveals the dissolved elements cycle in the continent-river-ocean system [4,5,6,7]. Given the complexity of river systems, the geochemical processes are controlled by many factors. Surface water chemistry in river basins is usually impacted by natural factors and anthropogenic activities.
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