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Image of Analysis Of Sedimentation Rate On The Coast Of Selat Baru Bengkalis Regency, Riau
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Analysis Of Sedimentation Rate On The Coast Of Selat Baru Bengkalis Regency, Riau

Patricia Tania / 1904110590 - Nama Orang;

Analysis of sedimentation rate on the coast of Selat Baru, Bengkalis Regency, Riau. This research was conducted in March 2023 at the Mouth of Jangkang River, Tourist Beach, and the Mouth of Liong River, Bengkalis Regency, Riau. The method used in this research is a survey method, involving observation and sample collection conducted at the research location. Based on the results of field sample collection and analysis conducted on the samples in the Marine Chemistry Laboratory. According to the Sheppard triangle, it is identified that at stations 1 and 3, the substrate type is muddy sand, while at station 2, the substrate type is sand. This is due to the weak currents in the research area, causing suspended sediments to settle easily.The sedimentation rate at station 1 is 97.42 cm/year, at station 2 is 80.86 cm/year, while at station 3 is 103.2 cm/year. It can be observed that station 3 has a higher sedimentation rate compared to the others due to the frequent ferry activities at the International port and local fishing vessel activities, making it a significant source of high sediment input.

Keywords : Sedimentation rate, Substrate, Sediment fraction, Bengkalis regency


Ketersediaan
#
Perpustakaan Universitas Riau 1904110590
1904110590
Tersedia
Informasi Detail
Judul Seri
-
No. Panggil
1904110590
Penerbit
Pekanbaru : Universitas Riau - FAPERIKA – Ilmu Kelautan., 2024
Deskripsi Fisik
-
Bahasa
Indonesia
ISBN/ISSN
-
Klasifikasi
1904110590
Tipe Isi
-
Tipe Media
-
Tipe Pembawa
-
Edisi
-
Subjek
ILMU KELAUTAN
Info Detail Spesifik
-
Pernyataan Tanggungjawab
Jaka
Versi lain/terkait

Tidak tersedia versi lain

Lampiran Berkas
  • COVER
  • DAFTAR ISI
  • ABSTRAK
  • BAB I PENDAHULUAN
  • BAB III METODE PENELITIAN
  • BAB III HASIL DAN PEMBAHASAN
  • BAB IV KESIMPULAN DAN SARAN
  • DAFTAR PUSTAKA
  • LAMPIRAN
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