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Relationship of the Characteristics of Sediments and Organic Materials Sediment with the Abundance of Kerang Darah (Anadara granosa) in Tanjung Balai Asahan Waters, North Sumatra Province Naomi Simanjuntak; Rifardi Rifardi; Afrizal Tanjung
Jurnal Perikanan dan Kelautan Vol. 25 No. 1 (2020): Februari
Publisher : Faculty of Fisheries and Marine, Universitas Riau

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31258/jpk.25.1.6-17

Abstract

This research was conducted in March-April 2019 in the waters of Tanjung Balai Asahan, North Sumatra Province. Aim to determine the particle size of sediments, determine the abundance and distribution patterns of kerang darah (A. granosa), and analyze the effect of particle size of sediments and organic matter on the abundance of kerang darah (A. granosa). Sediment and kerang darah (A. granosa) samples were taken using a grab sampler from 4 stations, each station consists of 5 sampling points. The results showed that the environmental conditions of Tanjung Balai Asahan waters were still able to support the life of kerang darah (A. granosa). The type of sediment in these waters is dominated by sandy mud. The average diameter of sediments (Mz) 3-7.7 Ø with classification as very fine sand-very fine silt. The highest average content of organic sediment is found at station 2 (13.70%) which is located around the mangrove forest which is included in the classification of medium organic matter. The highest average value of kerang darah (A. granosa) abundance is at station 4 (54 ind/m2), with a clustered distribution pattern at all stations. The relationship between sediment characteristics and abundance of kerang darah (A. granosa) in Tanjung Balai Asahan waters is classified as a strong relationship with a determination coefficient (R2) of 0.529, this means that the size of sediment particles 52.9% affects the abundance of kerang darah (A. granosa) throughout the station while the remaining 41.7% are influenced by other factors not examined. The relationship of the content of organic matter with the abundance of kerang darah (A. granosa) is classified as a weak relationship, with a coefficient of determination (R2) of 0.004, meaning that the content of 0.4% sediment affects the abundance of kerang darah (A. granosa) throughout the temporary station 99.6% is influenced by other factors not examine.
The Effect of Changes in The Shoreline of The Sea Law Implementation in West Rangsang Subdistrict, Kepulauan Meranti District Hendra Yosep Siburian; Rifardi; Afrizal Tanjung
Jurnal Perikanan dan Kelautan Vol. 25 No. 1 (2020): Februari
Publisher : Faculty of Fisheries and Marine, Universitas Riau

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31258/jpk.25.1.53-63

Abstract

This research was conducted in October 2018 at the West Rangsang Beach Waters, Meranti Islands Regency, Riau Province. This study aims to determine changes in shoreline that occurred in West Rangsang Sub-District in the last 10 years and the implementation of marine law regarding the regulation of shoreline change problems. Results of processing Landsat 5 and Landsat 8 images with large Changes in the coastline in the Melai Village were 55.56 m (accretion), in the Village of Kedabu Rapat as much as 50.94 m (abrasion) and in the village Bungur at 42.10 m (abrasion). The implementation of the law of the sea according to article 15 of UNCLOS 1982 in the determination of territorial sea areas adjacent to other countries decided the law No. 2 of 1971 concerning the determination of the borders of the two countries in the Malacca Strait. Determination of these coordinates are based on the baseline of each country. With the enactment of the 1982 International Law on the Law of the Sea, the Republic of Indonesia Government Regulation No. 38 of 2002 stipulated a list of geographical coordinates of the baseline points of the Indonesian archipelago. With the determination of geographical coordinates the problems in the changes in the coastline of the countries of Indonesia and Malaysia as a result of abrasion and accretion can be solved by observing the geographical coordinate points on the island of Rangsang