Suspended matter on the meridional section in the Laptev Sea in August-September 1991

• Main Authors: Kuptsov, Vladimir M, Lisitzin, Alexander P, Shevchenko, Vladimir P, Burenkov, Vladimir I
• Format: Dataset
• Language: English
• Published: PANGAEA 1999
• Subjects: Archive of Ocean Data; ARCOD; Laptev Sea; SPASIBA-91; SPASIBA-91_susp1; SPASIBA-91_susp10; SPASIBA-91_susp2; SPASIBA-91_susp23; SPASIBA-91_susp25; SPASIBA-91_susp27; SPASIBA-91_susp29; SPASIBA-91_susp3; SPASIBA-91_susp31; SPASIBA-91_susp33; SPASIBA-91_susp4; SPASIBA-91_susp5; SPASIBA-91_susp6; SPASIBA-91_susp7; SPASIBA-91_susp8; SPASIBA-91_susp9; Water sample; WS; Yakov Smirnitskiy; laptev; lena river
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.760871; https://doi.org/10.1594/PANGAEA.760871

Suspended matter concentration along a meridian section from the Lena River delta to 78°N (~500 km) at ten stations from the surface to the bottom was studied with weight and optical (light attenuation index) techniques. At seven stations average residence time of suspended matter in surface waters was determined by the disequilibrium 234Th method. Average residence time of suspended matter in other depth intervals was calculated by regression dependence between the 234Th/238U ratio and suspended matter concentration. Differential and integral fluxes of suspended matter in the water column were also calculated. Nepheloid matter dominates in suspended matter composition in surface waters. Calculations indicate that, before being buried on the bottom, solid river run-off is resuspended 2.3 times (aver.). Redistribution of nepheloid suspended matter in the near-bottom layer results in formation of a strongly pronounced depocentre - an area of maximal discharge of solid river run-off within the Laptev Sea.