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Analisis Kondisi Hidrologi terhadap Perkembangan Wilayah Perkotaan Studi Kasus DAS Kali Belik Yogyakarta Suprayogi, Slamet; Fatchurohman, Hendy; Widyastuti, M
Jurnal Geografi : Media Informasi Pengembangan dan Profesi Kegeografian Vol 16, No 2 (2019): July
Publisher : Universitas Negeri Semarang

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.15294/jg.v16i2.22364

Abstract

Perkembangan yang pesat di daerah Kota Yogyakarta memberikan berbagai konsekuensi dari sisi hidrologi. Perubahan lahan terbangun untuk memenuhi kebutuhan fasilitas fisik kota sangat cepat, seperti bangunan, jalan, dan tempat parkir. Kondisi ini akan merubah fungsi lahan sebagai satu kesatuan proses hidrologi, yakni lahan-lahan yang awalnya menyerap air  menjadi kedap air. Alih fungsi lahan yang diikuti oleh peningkatan aliran permukaan akan berpengaruh terhadap sumberdaya air baik dari segi kualitas maupun kuantitas. Hasil dari penelitian adalah terjadi perubahan penggunaan lahan di DAS Belik, yaitu berupa pengurangan lahan bervegetasi dan peningkatan lahan terbangun. Perubahan penggunaan lahan ini menyebabkan peningkatan koefisien aliran dan Curve Number (CN) di DAS Belik. Selain menyebabkan peningkatan koefisien aliran dan CN, peningkatan lahan terbagun juga menjadi sumber pencemar airtanah. Besarnya limbah domestik (detergen) dan sumber pencemar organik yang disebabkan konstruksi septictank yang terlalu dekat dengan sumur menyebabkan nilai phospat, nitrat, dan coliform jauh melebihi baku mutu air kelas 1. Kemudian arah aliran airtanah di DAS Belik bergerak dari hulu menuju ke arah hilir/selatan dengan potensi debit mencapai 104 liter/detik. Jika airtanah tercemar, maka konsentrasi pencemaran terbesar akan terjadi di bagian hilir DAS Belik.The consequence of rapid urbanization in the city of Yogyakarta lead to hydrological system change. Population and economic growth are the main reason for the increase in living place demand in the city of Yogyakarta. Landuse change is the impact of urban sprawl, which lead to the diminishing of groundwater resources and the increasing of overland flow. The extension of the built area that reaches the peri-urbans area and countryside will absolutely affect the quality and quantity of water resources.  The results show that landuse conversion occurred in several landuses in the sub-watershed of Belik. The main landuse change that detected from 2003-2012 is the diminishing of vegetated land and the increasing number of built area. Land conversion increased the run-off coefficient and Curve Number, that lead into the contamination of groundwater. The concentration of phosphate and coliform in almost all points exceeds the minimum standard of potable water. These results indicate that domestic wastewater and septic tank misconstructions play important role toward groundwater contamination. From the flownets construction, it shows that the groundwater flow from the northern part into southern part of  Belik sub-watershed with potential discharge up to 104 liter/second. There is also possibility for groundwater contamination to extent and reach the downstream area. the water resources.
Data Pesawat Udara Tanpa Awak Untuk Pendukung Analisis Dinamika Pesisir dan Erosi Pantai: Studi Kasus Pantai Pandansimo, Bantul, Daerah Istiwewa Yogyakarta Fatchurohman, Hendy; Indrawati, Like; Ningtiyas, Iswanti Rahayu; Nadhira, Nur Anisa; Meliyasari, Sasvita Gevi
Jurnal Spatial Wahana Komunikasi dan Informasi Geografi Vol. 23 No. 2 (2023): Spatial : Wahana Komunikasi dan Informasi Geografi
Publisher : Department Geography Education Faculty of Social Science - Universitas Negeri Jakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21009/spatial.232.04

Abstract

The coastal area is one of the most vulnerable areas to the threat of disaster due to the acceleration of climate change. One of the almost universal threats in coastal areas worldwide is coastal erosion. The coastal area of Bantul District, Special Region of Yogyakarta, is one of the areas that is quite severely affected by coastal erosion. This research aims to (1) determine the dynamics of the coastal area in the Pandansimo Beach area; (2) map the rate of abrasion at Pandansimo Beach, and (3) determine the leading causes of the coastal erosion that occurs. High-resolution Pleiades satellite data with a 50cm spatial resolution is used to determine the temporal changes in the coastline. In addition, satellite imagery from Google Earth is also used for the analysis from 2010-2021. The changes in the coastline are calculated using the DSAS software. Detailed morphological data was obtained from the acquisition of aerial photos using a multirotor unmanned aircraft. Based on the analysis, it was found that the process of coastal erosion dominated the dynamics of the coastal area. The average coastline regression value was recorded at 2.46 meters/year. Hydrodynamic and morphodynamic factors such as wind and wave forces, diminishing of fluvial sediment supply, and climate change are believed to cause coastal erosion.
Kerawanan Gelombang Pasang terhadap Penggunaan Lahan di Kawasan Wisata Pantai Sepanjang-Drini, Pesisir Selatan Kabupaten Gunungkidul Prabawa, Bayu Argadyanto; Wahyuhana, Ratika Tulus; Fatchurohman, Hendy
Geomedia Majalah Ilmiah dan Informasi Kegeografian Vol. 22 No. 1 (2024): Geo Media: Majalah Ilmiah dan Informasi Kegeografian
Publisher : Universitas Negeri Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21831/gm.v22i1.72493

Abstract

Gunungkidul Regional Spatial Plan states that Sepanjang and Drini Beach are designated areas for tourism zone, even Drini Beach is included in the development of a Fish Landing Base in Gunungkidul. The fact is that the Sepanjang-Drini coastal area is one of the susceptible area to storm tide that occur repeatedly every year. This research aims to study the land use susceptibility in the  Sepanjang-Pantai Drini coastal area based on the storm tide model. Tidal wave analysis conducted by modeling inundation caused by run-up height of tidal waves scenario, that overlayed with land use map. The susceptible area to tidal waves based on 2.99 meter wave height scenario in the Sepanjang Coast to Drini Beach is 4.82 hectares. The land use that mostly affected by tidal waves is an open area land use of sand beach. Stalls are the ones most susceptible building to tidal waves, where there are at least 130 units located in tidal waves susceptible area.
Modeling of Land Cover Changes in Banjarbaru City South Kalimantan Province Saputra, Aswin Nur; Saputra, Muhammad Wahyu; Fatchurohman, Hendy; Aryaguna, Prama Ardha
JURNAL GEOGRAFI Vol. 16 No. 1 (2024): JURNAL GEOGRAFI
Publisher : Universitas Negeri Medan

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24114/jg.v16i1.48121

Abstract

Urban areas often experience land cover changes. Banjarbaru is one of several cities in Indonesia that has experienced land changes. The relocation of the administrative center of Banjarmasin City to Banjarbaru City led to the development of settlements. One spatial analysis carried out to examine the phenomenon of land change is remote sensing techniques. The method that can be used is the Land Change Modeler from MOLUSCE in QGIS. This model uses the CAM (Cellular Automata Markov) method to identify land cover change and predict land cover distribution. CAM can understand and predict land change patterns by considering land use, vegetation, and cell spatial interactions. This modeling is based on land cover data for 2015 and 2020 and several supporting parameters such as DEM data and distance to roads. Based on the modeling results from 2015 and 2020, Banjarbaru City experienced a change in built-up land, with most of it occurring in the center of Banjarbaru City. Based on the Markov Chain method by looking at land changes in the previous year, the development of built-up land increased by about 8% of the Banjarbaru City area of 32917.41 hectares. Based on the prediction results, the development of built-up land is centered in the middle of Banjarbaru City, such as North and South Banjarbaru Districts, due to the development of residential development.Keywords: Land Cover, Land Change Modeller, Cellular Automata, Markov Chain
Karst Aquifer Characterization by Means of Its Karstification Degree and Time Series Analysis (Case: Ngerong Spring in Rengel Karst, East Java, Indonesia) Mujib, Muhammad Asyroful; Adji, Tjahyo Nugroho; Haryono, Eko; Naufal, Muhammad; Fatchurohman, Hendy
Indonesian Journal on Geoscience Vol. 11 No. 1 (2024)
Publisher : Geological Agency

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17014/ijog.11.1.45-60

Abstract

The purpose of this study is to define the characteristics of the karst aquifer, which is approximated by the parameters of (1) degree of karstification (Dk) and (2) time series analysis (cross-correlation and auto-correlation). This research focuses on the Ngerong Spring, the largest spring in Rengel Karst, East Java, Indonesia. Pendant rain gauge RG-3M and HOBO U20L-02 water-level data loggers were installed over one year with a recording interval of 15 minutes. Furthermore, after one year of time-series discharge data was obtained, the discharge recession coefficient was applied to make the recession formula. It was then used to estimate the karstification degree scale from 1 to 10. The aquifer memory system and the spring response to rainfall events were analyzed by auto-correlation and cross-correlation. The results of this study indicate that the karstification degree (Dk) of the Ngerong Spring system is 4.8-5.0, with one laminar and one turbulent flow subregime type. The aquifer system comprises a subregime with turbulent and laminar flow, where the substantial role in groundwater discharge plays the subregime with laminar flow. Meanwhile, time series analysis shows that the capacity of aquifer storage in the Ngerong Spring is large enough. It has a memory effect for 26.41 days, followed by a rapid response to rainfall events within 8 hours. Compared with several other karst sites in Java, the Ngerong Spring aquifer has the youngest development level with the best storage and the slowest release.