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EVALUATION OF LOCAL RECLAMATION DATA FOR SUSTAINIBILITY INFRASTUCTURE FACILITIES (CASE STUDY OF KLAWAS ZONE AND SUBAN ZONE IN POST COAL MINING AIR LAYU TANJUNG ENIM) Gumanti, Johnnedy; Sutriyono, Edy; Salni, Salni; Harnani, Harnani
BIOVALENTIA: Biological Research Journal Vol. 4 No. 1 (2018)
Publisher : Biology Department, Faculty of Mathematics and Natural Sciences, Sriwijaya University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (764.813 KB) | DOI: 10.24233/BIOV.4.1.2018.109

Abstract

This study identifies and analyzes the biophysical and environmental aspects of the environment, potentials and constraints, and then evaluates the post-mining reclamation land use that will be used for Other Use Areas (APL), the Residential Infrastructure Facility. Based on the Mining Closure Plan (RPT) on the utilization of former coal mine land at Air Laya Tanjung Enim, Klawas reclamation land use plan for Resettlement Facility and Zoning Infrastructures (Zone 2) while Suban reclamation land use plan for Productive Research area. Analysis in this research are scoring, SWOT and map overlay such as area function analysis and land suitability analysis based on physical condition of existing land. The result of this research is land suitability level for Residential Infrastructure Facility in Klawas, suitable land equal to 12% or 38 ha while 98% unfit or 258,7 ha from total area of 277,8 ha. Terms of land suitability in Klawas research area including Marginal (S3) with total scores of 80. where climate condition support with average temperature 24oC and rainfall 23,93 - 27,87 mm / day, slope of flat slope approaching water level river 0 - 3%, complex geological structure there are anticline in the form of fault and fracture, soil type Alluvial and Latosol, there are many aquifer with shallow depth to medium, there is vulnerability of geological disaster in the form of mass movement of soil / rock, flood, erosion and radiation exposure TENORM of moderate intensity. The results of land use evaluation for the Klawas reclamation area are more suitable for Freshwater Fishery Cultivation area than for Residential Infrastructure Facility area. Land tenure rate for Residential Infrastructure Facility in Suban, suitable land equal to 76 % or 237 ha while unsuitable 24% or 105 ha of total area of 342 ha. Conditions of land suitability in Suban's research area include Match (S2) with a total scores of 130. Climatic conditions support the average air temperature of 24°C and rainfall of 23.93 - 27.87 mm / day, the slope of flat slope is 3 - 8% there is no anticline structure in the form of fault, Andosol and Podsolic soil types, there is a shallow shallow depth of aquifer, no geological disaster vulnerability and low intensity TENORM radiation exposure. The results of the land-use evaluation for the Suban reclamation area are more suitable for the Residential Infrastructure area rather than for Productive Research area.
Kajian Tingkat Pencemaran Minyak Bumi Akibat Pengeboran Ilegal Berdasarkan Pemetaan Sungai Sumur Dan Fisika-Kimia Air Studi Kasus : Kecamatan Keluang Kabupaten Musi Banyuasin Sumatera Selatan Harnani Harnani
PROMINE Vol 6 No 2 (2018): PROMINE
Publisher : Jurusan Teknik Pertambangan, Fakultas Teknik, Universitas Bangka Belitung

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (508.158 KB) | DOI: 10.33019/promine.v6i2.779

Abstract

Water pollution is a thing that can affect the environment, especially on health and hygiene environment around. Sub Keluang Regency Musi Betung South Sumatra known to have oil drilling wells of the Earth where illegal do not fit a common standardization is done, so worried about polluted areas the surroundings. This research aims to study and know the impact of environmental pollution due to the illegal drilling by local people, as well as provide information research results to the Government and the police to cooperate in enforcing laws that have set. To find out which level contamination using a research method that is mapping rivers and wells include deskipsi the physical characteristics, such as water color, flavor, odor, retrieval example of a sample for the analysis of physical-chemical content of the water, and the projection of the level of public health. The result of the physical identification of the water as much as 8 samples were declared contaminated. Sampling see the provisions on physical changes on either the river or the well, the results of the analysis of physical-chemical water, found many chemical compounds which exceed standard pH obtained ranged from 6.25- 8.16 and types of groundwater salt (31-464 mg/L TDS), increase the value of pH and TDS is assumed to be due to saltwater waste results from drilling for petroleum is illegal, and the presence of chemical compounds, either the main or excessive accessories in water then it can affect health, which that is evidenced by the results of the projection of the level of public health from the years 2016 to now that continues to decline. referring to the decision of the Minister of State for the environment number: 115 the year 2003 on guidelines for the determination of the Status of Water quality by the State Minister for the environment using STORET method with a score of 16 (polluted medium).
ANALISIS KESTABILAN LERENG DENGAN METODE BISHOP DAN KUAT GESER BATUAN PADA DAERAH PULAU PINANG, KABUPATEN LAHAT SUMATERA SELATAN Ferdian Syahputra; Harnani Harnani; Budhi Setiawan
Jurnal Sumberdaya Bumi Berkelanjutan (SEMITAN) Vol 1, No 1 (2022)
Publisher : Institut Teknologi Adhi Tama Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.semitan.2022.3223

Abstract

Pada lokasi penelitian secara geografis terletak pada daerah Pulau Pinang dan sekitarnya Kabupaten Lahat, Sumatera Selatan. Tujuan dilakukannya penelitian ini yaitu untuk mengetahui daerah yang termasuk kedalam daerah yang rawan longsor dan melakukan upaya mitigasinya. Metode yang digunakan berupa metode kuat geser tanah dengan melakukan pengujian kuat geser langsung (Direct Shear Test) dan pengujian berat jenis tanah (Unit Weight). Kemudian dilanjutkan dengan metode Bishop untuk mencari nilai Faktor Keamanan (FK). Parameter yang digunakan didalam mencari nilai Faktor Keamanan (FK) yaitu kohesi (C), sudut geser dalam (ϕ), dan berat jenis tanah (Υ). Hasil penelitian didapatkan nilai faktor keamanan lokasi pengamatan pada lokasi penelitian 1 dan 2 termasuk (Kelas Labil) dikarenakan nilai faktor keamanannya 0,846 dan 0,586 , lokasi penelitan 3 termasuk (Kelas Stabil) dikarenakan nilai faktor keamanannya 2,543, lokasi penelitan 4 dan 5 termasuk (Kelas Kritis) dikarenakan nilai faktor keamanannya 1,119 dan 1,156. Upaya mitigasi yang dapat dilakukan yaitu prinsip soil nailing dengan cara memberi tanah paku – paku dengan panjang tertentu dengan jaraknya rapat.
Identifikasi Peningkatan Strength Factor Dengan Metode Q-System Pada Terowongan Tambang Bawah Tanah Daerah Perambahan, Kota Sawahlunto, Sumatera Barat Pebby Putra Juenda; Harnani Harnani; Budhi Setiawan
MINERAL Vol 7 No 2 (2022): MINERAL
Publisher : Jurusan Teknik Pertambangan Universitas Bangka Belitung

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33019/mineral.v7i2.3418

Abstract

Underground mining activities (Undergound Mining) at PT Allied Indo Coal Jaya Encroachment area, Sawahlunto City has the risk of subsidence due to reduced soil carrying capacity due to excavation of underground mine openings. The excavation of underground mine openings will result in disruption of the stability of the area such as roof collapse, rib spalling, and floor heave. This research was conducted in 2 research locations, namely Tunnel 6 Seam B and Tunnel 3 Seam C which aims to determine the recommendation of a buffer system in underground mine openings (Tunnel) by analyzing the geomechanical value of rocks using the Rock Tunnelling Quality Index (Q-System) method. ) so that the Strength Factor value increases. Data collection methods were carried out by field observation and laboratory testing, while data processing used Phase 8.0 software with Mohr-Coulomb failure criteria. The results of calculations and data processing showed that the Strength Factor value in Tunnel 6 Seam B was 1,04 (relatively stable) and Tunnel 3 Seam C was 0,84 (unstable). These results indicate that Tunnel 6 Seam B and Tunnel 3 Seam C must be supported by a buffer system. After the buffering system was carried out the Strength Factor value of Tunnel 6 Seam B increased to 1,59 (stable) and Tunnel 3 Seam C increased to 1,63 (stable).
Characteristic and Provenance of Talang Akar Formation Sandstone, Sukamoro Area, South Sumatera Yogie Zulkurnia Rochmana; Idarwati Idarwati; Harnani Harnani; Elisabet Dwi Mayasari
Jurnal IPTEK Vol 27, No 1 (2023)
Publisher : LPPM Institut Teknologi Adhi Tama Surabaya (ITATS)

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.iptek.2023.v27i1.4434

Abstract

Sukamoro area, Banyuasin Regency, South Sumatera, was the research location. This investigation focuses on the origin of sandstones from the Talang Akar Formation. In the area of investigation, sandstones are widely dispersed and exhibit a variety of properties. Due to the abundance of sandstones found and their high resistance and physical compactness, an analysis of the original rock can be carried out. Generally, the material that makes up sandstone comes from the previous rock. This investigation was undertaken using a descriptive-analytical methodology to determine the origin of the rock. The collected surface data is subsequently petrographically examined. After determining the composition of the constituent minerals, a provenance analysis was conducted to determine that the Talang Akar Formation's sandstones originated from the Magmatic Arc. Furthermore, the Talang Akar sandstone reveals the origin of the Recycle Orogen. Thus, it is considered that the sandstones of the Talang Akar Formation have seen many uplift episodes as a result of tectonic activity, almost to the point where they have experienced an increase in the maturity or stability of their continental block provenances
Zonasi Area Potensi Banjir Berdasarkan Analisa Topographic Wetness Index Hafizh Fikra Ramadhan; Harnani Harnani; Budhi Setiawan
Journal of Geology Sriwijaya Vol 1 No 2 (2022): The Journal of Geology Sriwijaya
Publisher : Teknik Geologi, Fakultas Teknik, Universitas Sriwijaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.62932/jgs.v1i2.1136

Abstract

Banjir merupakan bencana alam yang terjadi akibat aliran air yang terakumulasi pada suatu daerah atau cekungan, daerah aliran sungai umumnya memiliki banyak terdapat daerah yang berpotensi banjir, hal ini didasari oleh bentuk sungai, kerapatan sungai aspek hidrolika dan morfologi pada daerah tersebut. Di Indonesia provinsi Jawa Barat dan Jawa Tengah menduduki peringkat pertama dan kedua daerah dengan kejadian banjir tersbesar. Metode yang digunakan untuk mendeteksi daerah rawan banjir yang dapat dilakukan adala Topographic Wetness Index (TWI). Metode ini dapat menentukan nilai index kebasahan pada suatu daerah dan berfokus pada nilai kuantitatif terhadap topografi terhadap limpasan air hujan serta kondisi elevasi dan morfologi pada daerah tersebut, TWI melihat akumulasi air yang dapat terbentuk akibat kondisi topografi dan kemiringan lereng ataupun cekungan pada suatu daerah. Data yang digunakan pada analisa TWI adalah Digital Elevation Model (DEM), dari analisa tersbut akan didapatkan Indeks nilai TWI dan nilai Kerapatan sungai . Nilai TWI akan berasosiasi dengan tingkat kerapatan sungai dan dengan tingginya nilai kerawanan banjir. Berdasarkan hasil perhitungan dan analisa yang dilakukan nilai index TWI adalah -9.747 adalah yang terendah dan 12.5633 dengan nilai TWI tertinggi sedangkan pada nilai kerapatan sungai pada daerah penelitian masuk kedalam kelas sedang dan daerah yang terdampak banjir adalah kecamatan Karangnunggal, Bojongasih dan Bantarkalong.
Identifikasi Morfologi Berdasarkan Lineament dan Analisis Struktur Geologi Daerah Tanjung Beringin dan Sekitarnya Kabupaten Lahat, Provinsi Sumatera Selatan Dimas Indra Arifianto; Budhi Setiawan; Harnani Harnani
Journal of Geology Sriwijaya Vol 1 No 2 (2022): The Journal of Geology Sriwijaya
Publisher : Teknik Geologi, Fakultas Teknik, Universitas Sriwijaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.62932/jgs.v1i2.1273

Abstract

Identifikasi morfologi berdasarkan lineament dan analisis struktur geologi telah dilakukan di Desa Tanjung Beringin dan sekitarnya, Kabupaten Lahat, Provinsi Sumatera Selatan. Tahapan awal dalam identifikasi menggunakan pendekatan penginderaan jauh melalui analisis lineament menggunakan data DEMNAS. Penelitian ini difokuskan pada analisis lineament dengan data Digital Elevation Model (DEM) untuk mengidentifikasi struktur geologi dan morfologi di daerah penelitian. Metode yang digunakan dalam penelitian yaitu observatif, analitik dan interpretatif. Penelitian dilakukan data DEMNAS yang kemudian diektraksi menggunakan software PCI Geomatica dan setelah itu dikorelasi dengan data struktur geologi di lapangan. Analisis lineament yang digunakan yaitu panjang, orientasi dan densitas lineament. Penelitian ini bertujuan untuk menginterpretasi hubungan antara data lineament dengan hasil data lapangan. Lokasi penelitian dikontrol oleh struktur geologi yaitu fracture dan morfologi. Berdasarkan penelitian tersebut didapatkan data, daerah Tanjung Beringin tersusun atas fracture yang di analisa menghasilkan sesar mendatar kanan dan 3 satuan geomorfik/bentuklahan yaitu Channel Irregular Meander (CIM), Perbukitan Tinggi Berlereng Curam (PTBC), dan Perbukitan Denudasional (PD).
Remote Sensing Techniques for Identifying Flood Prone Areas Using the Vegetation Index, Water Index, and Simple Additive Weighting Methods for Mekarsari Areas, Cianjur Regency, West Java Harnani Harnani; Putri Savira
Journal of Earth and Marine Technology (JEMT) Vol 4, No 1 (2023)
Publisher : Lembaga Penelititan dan Pengabdian kepada Masyarakat - Institut Teknologi Adhi Tama Suraba

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jemt.2023.v4i1.4564

Abstract

Flood is a natural disaster with an intensity that often occurs in cities on a scale with excess water discharge in some areas. This research was conducted to determine the risk of flooding in Mekarsari Village and its surroundings, Cianjur Regency, West Java. (According to InaRisk, 2022) Risk and danger of flooding Moderate – High. This study uses data for the entire year 2022. With several parameters used in this study including land cover, rainfall, soil type, slope, NDVI, NDWI and SAVI. Simple Additive Weighting or weighting for each parameter with different results, according to the classification of each of these parameters. The results of this weighting will become a Flood Hazard Risk Map which was previously the result of overlay and intersection of land cover map, rainfall map, soil type map, slope map, Normalized Difference Vegetation Index map, Normalized Difference Water Index map and Soil Adjusted Vegetation Index map. On the Flood Disaster Risk Map there are five categories of vulnerability levels Not Hazardous, Less Hazardous, Moderate, Hazardous and Very Hazardous. The cause of the risk of flooding in the study area is that most of the land use is diverted to rice fields, plantations, dry agricultural land and settlements so that the lack of vacant land causes low absorption of rainwater and also steep slopes and high elevations which also cause rainwater to be stored in the lowlands. settlements) with moderate to high rainfall intensity every month. There is also a lack of education for the community to mitigate the risk of flood disasters so that waste management and waterways in settlements are inadequate and well managed.
Geotourism Assessment using the M-GAM method (Modified Geosite Assessment Model) Sawahlunto Region, West Sumatra Dieny Dezilia; Harnani Harnani
Journal of Earth and Marine Technology (JEMT) Vol 4, No 1 (2023)
Publisher : Lembaga Penelititan dan Pengabdian kepada Masyarakat - Institut Teknologi Adhi Tama Suraba

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jemt.2023.v4i1.4881

Abstract

The geological setting in the area is a strong attraction for natural tourism. The Sawahlunto Geopark area is one of the Geoparks located in West Sumatra Province which has a variety of geological sites. This area meets the criteria that make it a potential Geopark. The purpose of this analysis is to evaluate the potential of geotourism and use this assessment as a basis for developing geotourism in the Sawahlunto and surrounding geotourism areas. This analytical study was carried out using the M-GAM (Modified Geosite Assessment Model) method. In the study process, research methods were carried out using questionnaire data based on 27 indicators from the M-GAM method.M-GAM method has 27 indicators consisting of main and additional values that will be used as a questionnaire which will produce quantitative results. The 27 indicators contain several geotourism assessments, including scientific value, aesthetic value, protection value, functional value, and tourism value of a geosite. The maximum score that can be obtained by a geosite that has all the perfect criteria in 27 indicators will get a main score of 12 and an additional score of 15. 7 geosites will be assessed with results, namely Batu Runciang (8.17 and 7.62), Serpih Bakelok (6.35 and 7.72), Tabiang Tinggi (6.81 and 8.14) and Puncak Cemara (8.19 and 8.41), Stone Garden (6.37 and 7.96), Batu Gantuang Cave (3.91 and 6.07) and Kubang Waterfall (3.48 and 6.48). Referring to the results of the Sawahlunto geosite assessment, it was concluded that the Batu Runciang and Puncak Cemara Geosites had a high value in terms of main values compared to the other 5 geosites. Meanwhile, for additional value, Tabiang Tinggi and Puncak Cemara have sufficient value compared to the other 5 Geosites. This is because geosites with low value still lack various things such as facilities and promotions. Efforts that can be made are to build facilities at several geosites that still experience a lack of public facilities. Apart from that, promotion on social media is also very helpful in introducing geosites to the public.
Use of Spatial Data in Mapping Landslide Prone Areas in Luhurjaya and Surrounding Areas, Lebak Regency, Banten Province Abiyyu, Muhammad Dimas Al; Harnani, Harnani
Journal of Earth and Marine Technology (JEMT) Vol 4, No 2 (2024)
Publisher : Lembaga Penelititan dan Pengabdian kepada Masyarakat - Institut Teknologi Adhi Tama Suraba

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jemt.2024.v4i2.5262

Abstract

Landslides are a natural process that occurs in a natural landscape on earth which can cause various environmental damage and can cause loss of life. An increase in the risk of landslides can be caused by uncontrolled land conversion due to the increasing population so that land development is necessary. The research was conducted in Luhurjaya and surrounding areas, Cipanas District, Lebak Regency, Banten with an area of 9 x 9 km. The spatial integration method was used to map landslide-prone zones using a scoring and weighting method, using five parameters, namely slope, rainfall, lineament density, rock type, and NDVI. Those five parameters are then overlaid to form a landslide susceptibility map. As a result of analyzing the research area based on these five parameters, it was found that this area has five slope classes, one rainfall class, five lineament density classes, three rock type classes, and four NDVI classes. After all the datas are scored and weighed, it was found that this research area can be classified to three zones, namely low landslide susceptibility zone, medium landslide susceptibility zone, and high landslide susceptibility zone. From the results of this analysis, disaster mitigation should be needed that can affect the community in the Lebak Regency area, Banten Province, namely in the form of providing provisions in the form of knowledge to the community regarding disaster management which is useful for minimizing the risk of the consequences of landslides