English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Preliminary study of sediment ages and accumulation rates has been carried out in Jakarta Bay using unsupported 210 Pb. 210 Pb occurs naturally in sediments as one of the radioisotopes in the 238 U decay series. The total 210 Pb activity in sediments has two components, namely; supported and unsupported. The latter derives from dissociation of 210 Pb from 226 Ra through diffusion of the intermediate gaseous isotope 222 Rn which diffuse into the atmosphere and decay to 210 Pb. 210 Pb falling directly into seawater and deposit on the bed of the marine with sediments. 210 Pb has half-life of 22.26 years makes it well suited to dating and determining the accumulation rate of sediments laid down over the past 100 – 150 years. Two cores samples with diameter 7.5 cm were taken by scuba divers from Jakarta Bay and were analyzed of 210 Pb using -spectrometer equipped with PIPS detector. The sediment ages and range of sediment accumulation rates of core I and II are up to 169 years and (0.25 – 1.93) kg/m 2 y and up to 157 years and (0.15 – 2.68) kg/m 2 y, respectively.

PRELIMINARY STUDY OF SEDIMENT AGES AND ACCUMULATION RATES IN JAKARTA BAY DERIVED FROM DEPTH PROFILES OF UNSUPPORTED <sup>210</sup>Pb