(Table 2) pH and concentrations of dissolved and particulate chemical elements in the mixing zone of the Yur'eva River water and the Okhotsk Sea water

• Main Authors: Fazlullin, Sergey M, Savenko, Vitaly S
• Format: Dataset
• Language: English
• Published: PANGAEA 1992
• Subjects: Archive of Ocean Data; ARCOD; Atomic absorption spectrometry (AAS); Calculated; Chlorine; Copper; particulate; Depth; bottom/max; sediment/rock; top/min; Event label; Filtration; Iron; Latitude of event; Longitude of event; Manganese; Manganese 2+; Nickel; pH; pH meter; Titration; Total particulate matter; Water sample; WS; Yur-8-9/87-1; Yur-8-9/87-10; Yur-8-9/87-11; Yur-8-9/87-12; Yur-8-9/87-13; Yur-8-9/87-14; Yur-8-9/87-15; Yur-8-9/87-16; Yur-8-9/87-17; Yur-8-9/87-18; Yur-8-9/87-19; Yur-8-9/87-2; Yur-8-9/87-20; Yur-8-9/87-3; Yur-8-9/87-4; Yur-8-9/87-5; Okhotsk; Yur; okhotsk sea
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.759113; https://doi.org/10.1594/PANGAEA.759113

Data on behavior of iron, manganese, nickel, copper, and zinc in the zone where acidic volcanic waters of the Yur'eva River (Paramushir Island, Kuril Islands) mix with sea water are presented. Distributions of dissolved and particulate forms of these elements indicate that the mixing zone acts as a pH-based geochemical barrier, at which almost all dissolved iron and smaller amounts of other metals are precipitated. When chemogenic particulate matter formed in the mixing zone enters the open ocean, it can sorb trace elements from sea water.