慈乌兰河口潮汐造成的陆地形成动力学

A. Fauzi, I. Lestari, N. Hakiki, Tri Sutrisno, Ardli Swardana
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引用次数: 0

摘要

- 沿海地区是陆地和海洋之间的边界地区。沿海地区出现的现象之一是磨损和沉积。沉积作用导致河口附近地区形成隆起的土壤。本研究旨在通过对谷歌地球卫星图像的连续观测,确定隆起土壤的形成。研究在西爪哇 Tasikmalaya 县 Karangnunggal 区 Ciwulan 河口进行。研究于 2023 年 4 月至 6 月进行。这项研究采用的方法是每年对每颗卫星进行比较。根据逐年的卫星图像观察,可以发现慈乌兰河的水量增加,导致新出现的土地面积在 2019 年、2020 年和 2021 年开始逐年减少。新出现的陆地面积减少的原因是河口的磨损,因此新出现的陆地因被大量河水淹没而消失。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
DINAMIKA TERBENTUKNYA TANAH TIMBUL AKIBAT PASANG SURUT DI MUARA SUNGAI CIWULAN
- Coastal areas are border areas between land and sea areas. One of the phenomena that occurs in coastal areas is abrasion and sedimentation. Sedimentation results in the formation of raised soil in areas near the estuary. This research aims to identify the formation of emergent soil through continuous observation of Google Earth satellite images. The research was conducted at the mouth of the Ciwulan River, Karangnunggal District, Tasikmalaya Regency, West Java. The research was carried out in April – June 2023. The method used in this research was a comparison of each satellite each year. Based on observations of satellite imagery from year to year, it is observed that the volume of water in the Ciwulan River has increased, causing the area of emerging land to start to decrease from year to year in 2019, 2020, and 2021. The decrease in emerging land is due to abrasion at the mouth of the river, so the emerging land has disappeared because it was submerged by the high volume of river water.
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