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PEMANFAATAN HUTAN BAKAU MENJADI DESTINASI EKOWISATA MANGROVE DI KAMPUNG TUA BAKAU SERIP KELURAHAN SAMBAU, KECAMATAN NONGSA, KOTA BATAM Gatot Morwanto; Depri; Yuanita FD Sidabutar; Ismael P Sinaga
Jurnal Potensi Vol. 3 No. 2 (2023): SEPTEMBER
Publisher : Universitas Batam

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37776/jpot.v3i2.1215

Abstract

The potential of the Mangrove Forest ecosystem to become an ecotourism attraction for the community's awareness and love for Mangrove Forests is also small. Mangrove ecotourism is located in the Old Mangrove Village of Serip, Nongsa District, Sambau Village. This coastal area has great tourism potential, especially ecotourism potential in the form of beaches or mangrove ecosystems. The use of mangrove forests to become ecotourism is in line with the shift in tourist interest from old tourism to new tourism. Determining the development strategy for Mangrove Forest ecotourism. The type of research used is Data Analysis research, namely SWOT analysis. Strengths are the strength factors possessed by an organization which include skills, products, and so on to achieve organizational goals. Weaknesses that exist within an organization such as limitations in terms of resources, skills, and abilities are serious obstacles to the appearance of satisfactory organizational performance. Opportunities are some favorable environmental situations for a company. Meanwhile, threats are unfavorable environmental factors. Internal and external factors greatly influence the development of mangrove forest sustainability and the development of mangrove ecotourism. Based on the analysis that has been carried out to identify strengths, weaknesses, opportunities, and threats, it can be seen that there are more strengths and opportunities. The development of mangrove forest ecotourism has the opportunity to take advantage of the power to develop ecotourism in the Kampung Tua Bakau Serip area, namely to be able to create new jobs, especially in the field of tourism, especially for local communities. other tourism communities that take advantage of the available potential. Utilizing available attractions and adding supporting attractions, empowering local communities, and utilizing locations to become tourism businesses.
Analysis of Subsidence Hazards in Pandan Cave Area, Giri Mulyo Village, Marga Sekampung District, East Lampung using Analytical Hierarchy Process Bilal Al Farishi; Natalia, Happy Christin; Naufal, Rifqi Andi; Aganda, Riyanto Dedinta; Octafiani, Aulia; Hita Kirana; Depri; Pakpahan, Andreas Maruli; Sari, Hissy Ijitiha; Santoso, Nono Agus; Antosia, Risky Martin; Putri, Intan Andriani
Journal of Geoscience, Engineering, Environment, and Technology Vol. 9 No. 2 (2024): JGEET Vol 09 No 02 : June (2024)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2024.9.2.16848

Abstract

Pandan Cave is a basalt lava cave which is a unique geological tourism area located in Giri Mulyo Village, Marga Sekampung District, East Lampung Regency, Lampung Province. This cave was formed when the lava flow cooled at the top because it was in contact with the cold atmosphere, while at the bottom it was still flowing. This uniqueness caused Pandan Cave to become one of the tourist attractions that was once crowded with tourists. However, the condition of this cave is still very natural which can lead to the risk of geological disasters such as subsidence which can endanger tourists, so it is necessary to research to minimize the occurrence of geological disasters in the area. This research was conducted by observing aerial photographs, collecting data directly in the field, and then processing it with the Analytical Hierarchy Process (AHP). Parameters used in this AHP method include lithology, vegetation, weathering, rock mass class, and cave roof thickness. The existence of subsidence in the study area is influenced by weathering (34%), vegetation (31%), thickness of the cave roof layer (16%), lithology (10%), and rock mass class (9%). Based on the overlay results for each parameter that has been weighted, the Pandan Cave tourism area is divided into three subsidence hazard zone classifications, that is low hazard zone with value of 0.28-0.44, medium hazard zone with range of 0.44-0.60, and high hazard zone with range of 0.60-0.75. Through the Analytical Hierarchy Process (AHP) method and overlay of each parameter used, the distribution of subsidence hazard zones in the study area was obtained.  The low threat zone of 27.57 ha is about 57.07% of the total research area, the medium threat zone is 15.86 ha or about 32.83% of the total research area, and the high threat zone is 4.88 ha or about 10. 10% of the total research area.
Groundwater Quality Analysis Based on Physical Properties of The Gunungtiga and Surrounding Areas Hilman, Zaki; Widiatama, Angga Jati; Awfa, Dion; Alfarishi, Bilal; Prayogo, Wisnu; Depri
International Journal of Natural Science and Engineering Vol. 7 No. 2 (2023): Juli
Publisher : Lembaga Penelitian dan Pengabdian kepada Masyarakat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23887/ijnse.v7i2.67866

Abstract

Gunungtiga area has never been studied for the quality of groundwater, and residents have also complained about the quality of groundwater, these became the basis for selecting the research location. This study aims to analyze groundwater quality in the Gunungtiga Region, Lampung Province. Quantitative approached was used for this research, it was carried out by mapping the groundwater level to estimate the recharge area and collecting data on parameters of the physical properties of groundwater, including color, taste, odor, temperature, pH, TDS, and EC.  The physical properties approach was selected because it is relatively cheap and easy to observe, the data collection can also be done in situ. The physical property parameter data is then checked based on the Republic of Indonesia Minister of Health Regulation No. 492 of 2010. The observations at 14 points showed that the groundwater level in the research area is relatively shallow towards the west or in the direction with higher topography, so it can be interpreted as a recharge area, and it flowed towards the east area which has lower topography. The physical properties of the groundwater had no taste, odor, or color. The EC value ranges from 188.07 to 1066.82 µs/cm, including fresh water, the pH ranges from 5.41 to 7.5, the temperature ranges from 27.2 to 29.7 0C, and the TDS value ranges from 94. 04-542.91 mg/l. Of the 14 observation points, only 1 location met the quality standards, namely 22/DP/02. Treatment is required before groundwater can be used, such as filtering.