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KAJIAN TINGKAT BAHAYA EROSI PADA BERBAGAI TIPE TUTUPAN LAHAN SUB DAS PANJARATAN DI DAS TABUNIO KABUPATEN TANAH LAUT Wisda Hartati; Syarifuddin Kadir; Badaruddin Badaruddin
Jurnal Sylva Scienteae Vol 6, No 4 (2023): Jurnal Sylva Scienteae Vol 6 No 4 Edisi Agustus 2023
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v6i4.10021

Abstract

Changes in land use in an area are caused by direct land use. Land degradation due to land use changes that are not accompanied by visible damage prevention measures cause high levels of erosion and sedimentation and low levels of rainwater infiltration cause several problems.Tanah Laut Regency is an area where there is a lot of land conversion, so its not functioning properly. The goal of this study was to calculate the amount of erosion based on the type of land cover in the Panjaratan sub-watershed and to analyze the level of erosion hazard (TBE) in various land covers in the Panjaratan sub-watershed. Method that used is the method proposed by Wischmeier & Smith, namely the Universal Soil Loss Equation (USLE) and data collection by purposive sampling. The results was obtained show that the number of suspected erosion in the Panjaratan Sub-Watershed was 60.97 tonsa/ahaa/ayr with an average of 6.77 tonsa/ahaa/ayr and categorized as very light erosion with details The highest amount of erosion value was in Land Unit 3 in wood tuber farming with an of 14.47 tonsa/ahaa/ayr erosion with erosion hazard class I, while the lowest value was in Land Unit 4 in Jackfruit Plantations with 1.99 tonsa/ahaa/ayr erosion with erosion hazard class I. While the erosion hazard level in all land units shows TBE class 0-SR (very light) is found in UL 1 Corn plantation, UL 2 reeds, UL 4 Jackfruit Plantation, UL 5 Shrubs, UL 6 alang- alang, dryland agriculture at UL 3, Oil palm plantations at UL 7 and 8 While TBE class I-R (light) there is UL 9 on open landPerubahan tata guna lahan di suatu wilayah disebabkan karena adanya pemanfaatan lahan secara langsung. Degradasi lahan akibat dari perubahan tata guna lahan yang tidak disertai dengan tindakan pencegahan kerusakan secara kasat mata menimbulkan tingginya tingkat erosi dan sedimentasi serta rendahnya tingkat resapan air hujan menimbulkan beberapa permasalahan. Kabupaten Tanah Laut merupakan daerah yang banyak terjadi alih fungsi lahan sehingga tidak berfungsi baik. Tujuan penelitian ini adalah menghitung besarnya erosi berdasarkan tipe tutupan lahan di Sub DAS Panjaratan dan menganalisis tingkat bahaya erosi (TBE) di berbagai tutupan lahan di Sub DAS Panjaratan. Metode yang digunakan adalah metode yang dikenalkan Wischmeier & Smith berupa Universal Soil Loss Equation (USLE) dan pengambilan datanya dengan cara purposive sampling. Hasil penelitian menunjukkan Jumlah dugaan erosi di Sub DAS Panjaratan adalah 60,97 ton./.ha/.thn dengan rata rata 6,77 ton./.ha/.thn dan dikategori erosi sangat ringan dengan rincian. Jumlah nilai erosi tertinggi berada pada Unit Lahan 3 pada Pertanian umbi kayu dengan nilai 14,47 ton./.ha/.thn dengan kelas bahaya erosi I, Sedangkan nilai terendah ada pada Unit Lahan 4 pada Perkebunan Nangka dengan nilai 1,99 ton./.ha/.thn dengan kelas bahaya erosi I. Tingkat bahaya erosi pada semua unit menunjukkan TBE kelas 0-SR (sangat ringan) terdapat pada UL 1  Perkebunan jagung,  UL 2 alang-alang, UL 4 Perkebunan Nangka, UL 5 Semak Belukar, UL 6 alang- alang , pertanian lahan kering pada UL 3, Perkebunan sawit pada UL 7 dan 8 Sedangkan TBE kelas I-R (ringan) ada UL 9 pada lahan terbuka
PERUBAHAN SOSIAL MASYARAKAT DAYAK MERATUS PASCA BANJIR PADA DESA PATIKALAIN KABUPATEN HULU SUNGAI TENGAH Normaulida Normaulida; Hafizianor Hafizianor; Badaruddin Badaruddin
Jurnal Sylva Scienteae Vol 6, No 5 (2023): Jurnal Sylva Scienteae Vol 6 No 5 Edisi Oktober 2023
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v6i5.10666

Abstract

The purpose of this study is to 1) anaIyze the sociaI chages that occur in the socio-economic aspects of the forest viIIage community which incIude the economic condition of the community househoId and the contribution of forest resources to the community, 2) AnaIyze the sociaI change that occur in the socio-cuIturaI aspects of the forest viIIage comunity which incIude status sociaI and sociaI roIes, sociaI stratification and sociaI mobiIity. Thus study uses a quantitative anaIysis approach using a questionnaire that was anaIyzed on Wilcoxon Macth Pairs. This research was conducted in Patikalain ViIIage, Hantakan District, Hulu Sungai Tengah Regency, South Kalimantan. The resuIts of this study indicate that: 1) change that occur in the community due to fIooding, which causes sociaI changes in socio-economic aspects which incIude: a) circumstances the economy of forest viIIage communities; b) the roIe of forest resources for the community; 2) sociaI changes that occur in socio-cuIturaI aspects, nameIy changes in sociaI status and roIes, changes that occur in sociaI stratification, changes aIso occur in famiIy sociaI mobiIity, and changes aIso occur in peopIe's mindsets towards the enviromentTujuan dari peneIitian ini untuk 1) menganaIisis perubahan sosiaI yang terjadi pada aspek sosiaI ekonomi masyarakat desa hutan yang meIiputi keadaan perekonomian rumah tangga masyarakat dan kontribusi sumberdaya hutan bagi masyarakat, 2) MenganaIisis perubahan sosiaI yang terjadi pada aspek sosiaI budaya masyarakat desa hutan yang meIiputi status sosiaI dan peranan sosiaI, stratifikasi sosiaI dan mobiIitas sosiaI. PeneIitian ini menggunakan anaIisis kuantitatif pendekatan dengan menggunakan kuesioner yang dianaIisis pada Wilcoxon Match Pairs. PeneIitian ini diIakukan di Desa PatikaIain, Kecamatan Hantakan, Kabupaten HuIu Sungai Tengah, KaIimantan SeIatan. HasiI peneIitian ini menunjukan bahwa: 1) perubahan yang terjadi pada masyarakat akibat terjadinya banjir, yang menyebabkan terjadinya perubahan sosiaI pada aspek sosiaI ekonomi yang meIiputi: a) keadaan perekonomian masyarakat desa hutan; b) peran sumber daya hutan bagi masyarakat; 2) perubahan sosiaI yang terjadi pada aspek sosiaI budaya yaitu perubahan terjadi pada status dan peran sosiaI, perubahan juga terjadi pada stratifikasi sosiaI, perubahan juga terjadi pada mobiIitas sosiaI keIuarga, dan perubahan juga terjadi pada poIa pikir masyarakat terhadap Iingkungan.
ANALISIS INFILTRASI BERBAGAI UNIT LAHAN YANG BERBEDA PADA SUB DAS BANYU IRANG DAS MALUKA Friska Aprilia Banjarina; Badaruddin Badaruddin; Syarifuddin Kadir
JURNAL RIMBA LESTARI Vol 1 No 1 (2021): Vol. 1 No. 1 (2021)
Publisher : Jurusan Kehutanan

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/rimbalestari.v1i1.388

Abstract

The purpose of this study is to analyze the infiltration rate in land units with different types of land cover in the Banyu Irang Sub Watershed in the Maluka Watershed. Analyzing the volume and infiltration capacity of land units with different types of land cover in the Banyu Irang watershed in the Maluka Watershed. The method used in this research is the Horton method. Factors affecting infiltration are soil texture, soil bulk density, total soil porosity, soil organic matter, and soil moisture content. The results of the study show the value of the rate, volume dan capacity of infiltration, where the highest infiltration rate is found in the secondary forest land cover with a value of 145,5 mm/hr on land unit 19 with slope grade between 0-8% and the lowest infiltration rate is found in alang-alang (reeds) land cover with a value of 3,0 mm/hr on land units 32 with slope grade between 15-25%. The highest infiltration capacity and volume occurred in secondary forest land cover with a value of 83,490 mm/hr in land units 19. The lowest infiltration capacity and volume occurs in alang-alang (reeds) land cover with a value of 0,787 mm/hr on land units 1 and 0,846 mm/hr on land units 1.
ANALISIS SIFAT FISIK TANAH TERHADAP LAJU DAN VOLUME INFILTRASI DI DAERAH TANGKAPAN AIR (DTA) BARABAI KABUPATEN HULU SUNGAI TENGAH Reynaldy Yustisio; Badaruddin Badaruddin; Syarifuddin Kadir
Jurnal Sylva Scienteae Vol 7, No 2 (2024): Jurnal Sylva Scientea Vol 7 No 2 Edisi April 2024
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v7i2.12319

Abstract

Research at Barabai CA for 3 months. The aims of this study were to analyze the physical properties of soil in Barabai CA of Hulu Sungai Tengah District, analyze the relationship of infiltration capacity and volume, and measure the infiltration rate.  The primary data of this research is soil physical properties. Data from related agencies were used as secondary data. The results of the highest bulk density analysis in land unit 7 1.50 g/cm3, the lowest bulk density was found in land unit 8 with a value of 0.71 g/cm3. The results of the analysis of the highest particle density value in land unit 7 with a value of 2.45 g/cm3, the lowest particle density value was found in land unit 11 1.80 g/cm3. In land unit 8 with the highest value of 64.08%, land unit 7 with the lowest value of 38.86%. The relationship between infiltration capacity and infiltration volume with a very close correlation value of 0.9819, means that only 0.02 is influenced by other factorsPenelitian di DTA Barabai selama 3 bulan. Tujuan penelitian ini adalah untuk menganalisis sifat fisik tanah DTA Barabai Kabupaten HST, hubungan kapasitas dan volume, dan pengukuran laju infiltrasi. Data primer penelitian ini adalah sifat fisik tanah.  Data Instansi terkait digunakan sebagai data sekunder. Hasil analisis Bulk Density (BD)  tertinggi di unit lahan 7 dengan nilai 1.50 g/cm3, BD  dan terendah di unit lahan 8 dengan nilai 0.71 g/cm3. Hasil analisis nilai particle density (PD) tertinggi di unit lahan  7 dengan nilai sebesar 2,45 g/cm3, PD terendah terdapat pada unit lahan 11 dengan angka 1,80 g/cm3. Di unit lahan 8 dengan nilai sebesar 64,08% tertinggi, unit lahan 7 dengan nilai 38,86% terendah. Hubungan kapasitas infiltrasi dan volume infiltrasi dengan nilai kolerasi sangat erat yaitu 0,9819 artinya hanya 0,02 dipengaruhi oleh faktor lain
PEMETAAN BENCANA TANAH LONGSOR DI DTA BARABAI MENGGUNAKAN METODE EKSTRAKSI NDBI, SAVI, DAN CBI Naufal Noor Kamil; Badaruddin Badaruddin; Syam'ani Syam'ani
Jurnal Sylva Scienteae Vol 7, No 2 (2024): Jurnal Sylva Scientea Vol 7 No 2 Edisi April 2024
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v7i2.12316

Abstract

The destruction of forest areas results in large amounts of surface runoff, thereby disrupting soil stability and triggering landslides. The landslide disaster occurred in the Barabai Catchment Area (DTA) followed by flood. Mapping the location of landslides using images can be done as a mitigation effort in disasters. The extraction method is used to determine changes in an area, so it can be used to observe changes in soil appearance due to landslides. The purpose of this study was to test the accuracy of the extraction method at the landslide location using Sentinel-2 imagery and analyze its spatial distribution in the Barabai catchment area. The extraction methods used are NDBI, SAVI, and CBI. The accuracy test was carried out using the Confusion Matrix method by comparing the results of image extraction with field surveys. Sampling in the survey was carried out by accidental sampling by considering the access road to the landslide location. The results of testing the accuracy of the extraction method obtained the highest Overall Accuracy by the NDBI method of 73.53%, then the SAVI method 63.73%, and the CBI method 69.61%. The area of the landslide in the Barabai catchment area is estimated at 183.92 HectaresRusaknya kawasan hutan mengakibatkan aliran permukaan dalam jumlah besar, sehingga mengganggu kestabilan tanah dan memicu terjadinya bencana tanah longsor. Bencana tanah longsor terjadi pada Daerah Tangkapan Air (DTA) Barabai diikuti dengan banjir. Pemetaan lokasi tanah longsor menggunakan citra dapat dilakukan sebagai upaya mitigasi pada bencana. Metode ekstraksi digunakan untuk mengetahui perubahan suatu area, sehingga dapat digunakan dalam mengamati perubahan kenampakan tanah akibat tanah longsor. Tujuan Penelitian ini adalah menguji akurasi metode ekstraksi pada lokasi longsor menggunakan citra Sentinel-2 dan menganalisis distribusi spasialnya di daerah tangkapan air Barabai. Metode ekstraksi yang digunakan adalah NDBI, SAVI, dan CBI. Uji akurasi dilakukan menggunakan metode Confusion Matrix dengan membandingkan hasil ekstraksi citra dengan survey lapangan. Pengambilan sampel dalam survey dilakukan secara Accidental Sampling dengan mempertimbangkan akses jalan lokasi longsor. Hasil dari pengujian akurasi dari metode ekstraksi didapatkan Overall Accuracy tertinggi oleh metode NDBI sebesar 73,53%, kemudian metode SAVI 63,73%, dan metode CBI 69,61%. Luas longsoran tanah pada daerah tangkapan air barabai diperkirakan sebesar 183,92 Hektar.
Co-Authors Abdi Fithria Adi Rahmadi Ahmad Jauhari Ahmad Mujaffar Ahmad Yamani Ahmadi Ahmadi Akhmad Hidayat Akhmad Rizalli Saidy Andi Mizwar Arief R. M. Akbar Baharudin Nur Efendi Basir Basir Budi Susilo Dahni Dahni Dedy Supratono Dina Naemah Edy Kurniawan Eko Rini Indrayatie Eko Suhartono Eko Suhartono Emmy Sri Mahreda Emmy Sri Mahreda Fakhrur Razie Friska Aprilia Banjarina Gusti Muhammad Hatta Gusti Reni Amalinda Gusti Rusmayadi Hafizianor Hafizianor Hanif Faisol Ichsan Ridwan Idiannor Mahyudin Ilmi Akbar Irma Febrianty Jefri H Simamora Karta Sirang Khairun Nisa Kissinger Kissinger Kurdiansyah Lusi Anggraeni M. Faisal Ramadhani Mahrus Aryadi Meilawati Meilawati Miftahul Munir Moh Zely Fahruddin Monica Andriana Mufidah Asy’ari Muhammad Damiri Muhammad Helmi Muhammad Ruslan Muhammad Ruslan Mujari Rahman Mustika Wiratri Naufal Noor Kamil Nina Wahyuningsih Noraito Gultom Normaulida Normaulida Nur Syifa Yarnie Nurlina Nurlina Rahman Rahman Rahmiyati Rahmiyati Raiwani Wahdah Raziv Rahman Reynaldy Yustisio Ridwan Mulyawan Riski Dwi Saputro Riza Arian Noor Rizal Anshari Rizqi Puteri Mahyudin Robby Arni Sederi Sederi Setia Budi Peran Siami Muslikhah Siti Hamidah Supari Supari Susilawati Susilawati Syahidar Khalid Syam'ani Syam'ani Syarifuddin Kadir Vina Delya Wisda Hartati Yesi Eka Pratiwi Yudi Firmanul Arifin Yuniarti Yuniarti Zainal Abidin